147 results on '"Littler, K"'
Search Results
2. A High‐Fidelity Benthic Stable Isotope Record of Late Cretaceous–Early Eocene Climate Change and Carbon‐Cycling
- Author
-
Barnet, JSK, Littler, K, Westerhold, T, Kroon, D, Leng, MJ, Bailey, I, Röhl, U, and Zachos, JC
- Subjects
Climate Action ,Life Below Water - Published
- 2019
3. Oceanic Anoxic Event 2 triggered by Kerguelen volcanism
- Author
-
Walker-Trivett, C.A., Kender, S., Bogus, K.A., Littler, K., Edvardsen, T., Leng, M.J., Lacey, J., Riding, J.B., Millar, I.L., Wagner, D., Walker-Trivett, C.A., Kender, S., Bogus, K.A., Littler, K., Edvardsen, T., Leng, M.J., Lacey, J., Riding, J.B., Millar, I.L., and Wagner, D.
- Abstract
Large Igneous Provinces (LIPs) are associated with global warming and carbon cycle perturbations during Oceanic Anoxic Event 2 (OAE2, ~94 Ma) and the Mid-Cenomanian Event (MCE, ~96.5 Ma). However, there is still no consensus on the role volcanism played as a trigger, or its source – previously ascribed to the Caribbean LIP or High Arctic LIP. Here, we use Mentelle Basin sedimentary mercury (Hg) concentrations to determine the timing of volcanism, and neodymium (Nd) and strontium (Sr) isotopes for sedimentary provenance. High Hg concentrations compared to Northern Hemisphere records, and a shift to radiogenic Nd isotopes, indicates Kerguelen LIP volcanic activity and plateau uplift occurred in the lead up to and within OAE2. Whilst we find limited evidence that a volcanic event caused the MCE, pulsed Hg spikes before and during OAE2 imply volcanic emissions were key in driving climate and carbon cycle changes and triggering OAE2.
- Published
- 2024
4. Frequency, magnitude and character of hyperthermal events at the onset of the Early Eocene Climatic Optimum
- Author
-
Lauretano, V, Littler, K, Polling, M, Zachos, JC, and Lourens, LJ
- Subjects
Paleontology ,Physical Geography and Environmental Geoscience - Abstract
Recent studies have shown that the Early Eocene Climatic Optimum (EECO) was preceded by a series of short-lived global warming events, known as hyperthermals. Here we present high-resolution benthic stable carbon and oxygen isotope records from ODP Sites 1262 and 1263 (Walvis Ridge, SE Atlantic) between ∼ 54 and ∼ 52 million years ago, tightly constraining the character, timing, and magnitude of six prominent hyperthermal events. These events, which include Eocene Thermal Maximum (ETM) 2 and 3, are studied in relation to orbital forcing and long-term trends. Our findings reveal an almost linear relationship between δ13C and δ18O for all these hyperthermals, indicating that the eccentricity-paced covariance between deep-sea temperature changes and extreme perturbations in the exogenic carbon pool persisted during these events towards the onset of the EECO, in accordance with previous observations for the Paleocene Eocene Thermal Maximum (PETM) and ETM2. The covariance of δ13C and δ18O during H2 and I2, which are the second pulses of the "paired" hyperthermal events ETM2-H2 and I1-I2, deviates with respect to the other events. We hypothesize that this could relate to a relatively higher contribution of an isotopically heavier source of carbon, such as peat or permafrost, and/or to climate feedbacks/local changes in circulation. Finally, the δ18O records of the two sites show a systematic offset with on average 0.2 ‰ heavier values for the shallower Site 1263, which we link to a slightly heavier isotopic composition of the intermediate water mass reaching the northeastern flank of the Walvis Ridge compared to that of the deeper northwestern water mass at Site 1262.
- Published
- 2015
5. The geochemistry of modern calcareous barnacle shells and applications for palaeoenvironmental studies
- Author
-
Ullmann, C.V., Gale, A.S., Huggett, J., Wray, D., Frei, R., Korte, C., Broom-Fendley, S., Littler, K., and Hesselbo, S.P.
- Published
- 2018
- Full Text
- View/download PDF
6. Climate and carbon-cycling in the Early Cretaceous
- Author
-
Littler, K.
- Subjects
550 - Abstract
The Cretaceous (~145–65 Ma) is widely regarded as a greenhouse period with warm, equable climates and elevated atmospheric CO2 relative to the modern. However, the earliest Cretaceous (Berriasian–Barremian; 145–125 Ma) is commonly characterised as a relatively colder “coolhouse” interval, typified by lower global temperatures than the mid-Cretaceous. Unfortunately, the lack of absolute sea surface temperature (SST) estimates prior to the Barremian has hampered efforts to definitively reconstruct Early Cretacous climate. Here, the TEX86 palaeotemperature proxy, for which a detailed review is provided, has been used to generate a 13 myr record of SST estimates for the Early Cretaceous, based on sediments from assorted deep-sea drilling sites. A consistent offset in the TEX86 ratio between transported mudstones and pelagic carbonates in the low-latitude marine sediments (DSDP Sites 603 and 534) has been identified, which may be linked to post-burial diagenesis or a difference in organic matter type between lithologies. Mindful of these apparent lithological effects on TEX86, only the pelagic sediments were used to subsequently reconstruct Early Cretaceous SSTs. These TEX86 records demonstrate both elevated SSTs (>27 ºC) at low and mid-latitudes relative to the modern, and the apparent stability of these high temperatures over long timescales. This lack of SST variation in the low-latitudes during the Valanginian positive carbon-isotope event (CIE; ~135–138 Ma), casts doubt on the warming-weathering feedback model put forward to explain this major perturbation. Additionally, new paired bulk organic (δ13Corg) and bulk carbonate (δ13Ccarb) carbon-isotope records from North Atlantic DSDP sites, have been used to reconstruct relative changes in pCO2 across the CIE. These observed fluctuations in Δ13C imply changes in carbon-cycling and a possible drawdown in CO2, due to excess organic matter burial associated with the CIE.
- Published
- 2011
7. Climate Evolution Through the Onset and Intensification of Northern Hemisphere Glaciation
- Author
-
McClymont, EL, Ho, S‐L, Ford, HL, Bailey, I, Berke, MA, Bolton, CT, Schepper, S, Grant, GR, Groeneveld, J, Inglis, GN, Karas, C, Patterson, MO, Swann, GEA, Thirumalai, K, S.M.White, Alonso‐Garcia, M, Anand, P, Hoogakker, BAA, Littler, K, Petrick, BF, Risebrobakken, B, Abell, JT, Crocker, AJ, Graaf, F, Feakins, SJ, Hargreaves, JC, Jones, CL, Markowska, M, Ratnayake, AS, Stepanek, C, Tangunan, D, CEREGE, and Aix Marseille Univ, CNRS, IRD, INRA, Coll France
- Subjects
[SDE]Environmental Sciences - Abstract
International audience; The Pliocene Epoch (∼5.3-2.6 million years ago, Ma) was characterized by a warmer than present climate with smaller Northern Hemisphere ice sheets, and offers an example of a climate system in long-term equilibrium with current or predicted near-future atmospheric CO 2 concentrations (pCO 2). A long-term trend of ice-sheet expansion led to more pronounced glacial (cold) stages by the end of the Pliocene (∼2.6 Ma), known as the "intensification of Northern Hemisphere Glaciation" (iNHG). We assessed the spatial and temporal variability of ocean temperatures and ice-volume indicators through the late Pliocene and early Pleistocene (from 3.3 to 2.4 Ma) to determine the character of this climate transition. We identified asynchronous shifts in long-term means and the pacing and amplitude of shorter-term climate variability, between regions and between climate proxies. Early changes in Antarctic glaciation and Southern Hemisphere ocean properties occurred even during the mid-Piacenzian warm period (∼3.264-3.025 Ma) which has been used as an analog for future warming. Increased climate variability subsequently developed alongside signatures of larger Northern Hemisphere ice sheets (iNHG). Yet, some regions of the ocean felt no impact of iNHG, particularly in lower latitudes. Our analysis has demonstrated the complex, non-uniform and globally asynchronous nature of climate changes associated with the iNHG. Shifting ocean gateways and ocean circulation changes may have pre-conditioned the later evolution of ice sheets with falling atmospheric pCO 2. Further development of high-resolution, multi-proxy reconstructions of climate is required so that the full potential of the rich and detailed geological records can be realized. Plain Language Summary Warm climates of the geological past provide windows into future environmental responses to elevated atmospheric CO 2 concentrations, and past climate transitions identify important or sensitive regions and processes. We assessed the patterns of average ocean temperatures and indicators of ice sheet size over hundreds of thousands of years, and compared to shorter-term variability (tens of thousands of years) during a recent transition from late Pliocene warmth (when CO 2 was similar to present) to the onset of the large and repeated advances of northern hemisphere ice sheets referred to as the "ice ages." MCCLYMONT ET AL.
- Published
- 2023
- Full Text
- View/download PDF
8. Climate Evolution Through the Onset and Intensification of Northern Hemisphere Glaciation
- Author
-
McClymont, E. L., primary, Ho, S. L., additional, Ford, H. L., additional, Bailey, I., additional, Berke, M. A., additional, Bolton, C. T., additional, De Schepper, S., additional, Grant, G. R., additional, Groeneveld, J., additional, Inglis, G. N., additional, Karas, C., additional, Patterson, M. O., additional, Swann, G. E. A., additional, Thirumalai, K., additional, White, S. M., additional, Alonso‐Garcia, M., additional, Anand, P., additional, Hoogakker, B. A. A., additional, Littler, K., additional, Petrick, B. F., additional, Risebrobakken, B., additional, Abell, J. T., additional, Crocker, A. J., additional, de Graaf, F., additional, Feakins, S. J., additional, Hargreaves, J. C., additional, Jones, C. L., additional, Markowska, M., additional, Ratnayake, A. S., additional, Stepanek, C., additional, and Tangunan, D., additional
- Published
- 2023
- Full Text
- View/download PDF
9. Reconstructing PCO2 in the Deep Geological Past Using a General Phytoplankton Biomarker
- Author
-
Graham, O., primary, Witkowski, C., additional, Littler, K., additional, and Naafs, D., additional
- Published
- 2023
- Full Text
- View/download PDF
10. Site U1447
- Author
-
Clemens, S.C., primary, Kuhnt, W., additional, LeVay, L.J., additional, Anand, P., additional, Ando, T., additional, Bartol, M., additional, Bolton, C.T., additional, Ding, X., additional, Gariboldi, K., additional, Giosan, L., additional, Hathorne, E.C., additional, Huang, Y., additional, Jaiswal, P., additional, Kim, S., additional, Kirkpatrick, J.B., additional, Littler, K., additional, Marino, G., additional, Martinez, P., additional, Naik, D., additional, Peketi, A., additional, Phillips, S.C., additional, Robinson, M.M., additional, Romero, O.E., additional, Sagar, N., additional, Taladay, K.B., additional, Taylor, S.N., additional, Thirumalai, K., additional, Uramoto, G., additional, Usui, Y., additional, Wang, J., additional, Yamamoto, M., additional, and Zhou, L., additional
- Published
- 2016
- Full Text
- View/download PDF
11. Expedition 353 summary
- Author
-
Clemens, S.C., primary, Kuhnt, W., additional, LeVay, L.J., additional, Anand, P., additional, Ando, T., additional, Bartol, M., additional, Bolton, C.T., additional, Ding, X., additional, Gariboldi, K., additional, Giosan, L., additional, Hathorne, E.C., additional, Huang, Y., additional, Jaiswal, P., additional, Kim, S., additional, Kirkpatrick, J.B., additional, Littler, K., additional, Marino, G., additional, Martinez, P., additional, Naik, D., additional, Peketi, A., additional, Phillips, S.C., additional, Robinson, M.M., additional, Romero, O.E., additional, Sagar, N., additional, Taladay, K.B., additional, Taylor, S.N., additional, Thirumalai, K., additional, Uramoto, G., additional, Usui, Y., additional, Wang, J., additional, Yamamoto, M., additional, and Zhou, L., additional
- Published
- 2016
- Full Text
- View/download PDF
12. Expedition 353 methods
- Author
-
Clemens, S.C., primary, Kuhnt, W., additional, LeVay, L.J., additional, Anand, P., additional, Ando, T., additional, Bartol, M., additional, Bolton, C.T., additional, Ding, X., additional, Gariboldi, K., additional, Giosan, L., additional, Hathorne, E.C., additional, Huang, Y., additional, Jaiswal, P., additional, Kim, S., additional, Kirkpatrick, J.B., additional, Littler, K., additional, Marino, G., additional, Martinez, P., additional, Naik, D., additional, Peketi, A., additional, Phillips, S.C., additional, Robinson, M.M., additional, Romero, O.E., additional, Sagar, N., additional, Taladay, K.B., additional, Taylor, S.N., additional, Thirumalai, K., additional, Uramoto, G., additional, Usui, Y., additional, Wang, J., additional, Yamamoto, M., additional, and Zhou, L., additional
- Published
- 2016
- Full Text
- View/download PDF
13. Evidence of a South Asian Proto‐Monsoon During the Oligocene‐Miocene Transition
- Author
-
Beasley, C., primary, Kender, S., additional, Giosan, L., additional, Bolton, C. T., additional, Anand, P., additional, Leng, M. J., additional, Nilsson‐Kerr, K., additional, Ullmann, C. V., additional, Hesselbo, S. P., additional, and Littler, K., additional
- Published
- 2021
- Full Text
- View/download PDF
14. Key criteria for the ethical acceptability of COVID-19 human challenge studies: Report of a WHO Working Group
- Author
-
Jamrozik, E, Littler, K, Bull, S, Emerson, C, Kang, G, Kapulu, M, Rey, E, Saenz, C, Shah, S, Smith, PG, Upshur, R, Weijer, C, Selgelid, MJ, and COVID-19, WHO Working Group for Guidance on Human Challenge Studies in
- Subjects
Biomedical Research ,COVID-19 Vaccines ,Coronavirus disease 2019 (COVID-19) ,Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2) ,030231 tropical medicine ,Ethical standards ,World Health Organization ,Antiviral Agents ,03 medical and health sciences ,0302 clinical medicine ,Informed consent ,Humans ,030212 general & internal medicine ,Research ethics ,Informed Consent ,General Veterinary ,General Immunology and Microbiology ,SARS-CoV-2 ,Patient Selection ,Vaccination ,Public Health, Environmental and Occupational Health ,COVID-19 ,Bioethics ,Healthy Volunteers ,COVID-19 Drug Treatment ,Clinical trial ,Infectious Diseases ,Human Experimentation ,Key (cryptography) ,Molecular Medicine ,Engineering ethics ,WHO Report ,Psychology ,Ethics Committees, Research - Abstract
This report of the WHO Working Group for Guidance on Human Challenge Studies in COVID-19 outlines ethical standards for COVID-19 challenge studies. It includes eight Key Criteria related to scientific justification, risk-benefit assessment, consultation and engagement, co-ordination of research, site selection, participant selection, expert review, and informed consent. The document aims to provide comprehensive guidance to scientists, research ethics committees, funders, policymakers, and regulators in deliberations regarding SARS-CoV-2 challenge studies by outlining criteria that would need to be satisfied in order for such studies to be ethically acceptable.
- Published
- 2021
15. Lessons from a high-CO2 world: an ocean view from ∼ 3 million years ago
- Author
-
McClymont, EL, Ford, HL, Ho, SL, Tindall, JC, Haywood, AM, Alonso-Garcia, M, Bailey, I, Berke, MA, Littler, K, Patterson, MO, Petrick, B, Peterse, F, Ravelo, AC, Risebrobakken, B, De Schepper, S, Swann, GEA, Thirumalai, K, Tierney, JE, van der Weijst, C, White, S, Abe-Ouchi, A, Baatsen, MLJ, Brady, EC, Chan, W-L, Chandan, D, Feng, R, Guo, C, von der Heydt, AS, Hunter, S, Li, X, Lohmann, G, Nisancioglu, KH, Otto-Bliesner, BL, Peltier, WR, Stepanek, C, Zhang, Z, Marine and Atmospheric Research, Organic geochemistry, Marine palynology and palaeoceanography, Sub Dynamics Meteorology, Sub Physical Oceanography, and Marine Palynology
- Subjects
Global and Planetary Change ,Stratigraphy ,Palaeontology - Abstract
A range of future climate scenarios are projected for high atmospheric CO2 concentrations, given uncertainties over future human actions as well as potential environmental and climatic feedbacks. The geological record offers an opportunity to understand climate system response to a range of forcings and feedbacks which operate over multiple temporal and spatial scales. Here, we examine a single interglacial during the late Pliocene (KM5c, ca. 3.205±0.01 Ma) when atmospheric CO2 exceeded pre-industrial concentrations, but were similar to today and to the lowest emission scenarios for this century. As orbital forcing and continental configurations were almost identical to today, we are able to focus on equilibrium climate system response to modern and near-future CO2. Using proxy data from 32 sites, we demonstrate that global mean sea-surface temperatures were warmer than pre-industrial values, by ∼2.3 ∘C for the combined proxy data (foraminifera Mg∕Ca and alkenones), or by ∼3.2–3.4 ∘C (alkenones only). Compared to the pre-industrial period, reduced meridional gradients and enhanced warming in the North Atlantic are consistently reconstructed. There is broad agreement between data and models at the global scale, with regional differences reflecting ocean circulation and/or proxy signals. An uneven distribution of proxy data in time and space does, however, add uncertainty to our anomaly calculations. The reconstructed global mean sea-surface temperature anomaly for KM5c is warmer than all but three of the PlioMIP2 model outputs, and the reconstructed North Atlantic data tend to align with the warmest KM5c model values. Our results demonstrate that even under low-CO2 emission scenarios, surface ocean warming may be expected to exceed model projections and will be accentuated in the higher latitudes.
- Published
- 2020
16. Evidence of a South Asian Proto‐Monsoon During the Oligocene‐Miocene Transition
- Author
-
Beasley, C., Kender, S., Giosan, L., Bolton, C. T., Anand, P., Leng, M.J., Nilsson‐Kerr, K., Ullmann, C. V., Hesselbo, S. P., Littler, K., Beasley, C., Kender, S., Giosan, L., Bolton, C. T., Anand, P., Leng, M.J., Nilsson‐Kerr, K., Ullmann, C. V., Hesselbo, S. P., and Littler, K.
- Abstract
The geological history of the South Asian monsoon (SAM) before the Pleistocene is not well-constrained, primarily due to a lack of available continuous sediment archives. Previous studies have noted an intensification of SAM precipitation and atmospheric circulation during the middle Miocene (∼14 Ma), but no records are available to test how the monsoon changed prior to this. In order to improve our understanding of monsoonal evolution, geochemical and sedimentological data were generated for the Oligocene-early Miocene (30–20 Ma) from Indian National Gas Hydrate Expedition 01 Site NGHP-01-01A in the eastern Arabian Sea, at 2,674 m water depth. We find the initial glaciation phase (23.7–23.0 Ma) of the Oligocene-Miocene transition (OMT) to be associated with an increase in water column ventilation and water mass mixing, suggesting an increase in winter monsoon type atmospheric circulation, possibly driven by a relative southward shift of the intertropical convergence zone. During the latter part of the OMT, or “deglaciation” phase (23.0–22.7 Ma), a long-term decrease in Mn (suggestive of deoxygenation), increase in Ti/Ca and dissolution of the biogenic carbonate fraction suggest an intensification of a proto-summer SAM system, characterized by the formation of an oxygen minimum zone in the eastern Arabian Sea and a relative increase of terrigenous material delivered by runoff to the site. With no evidence at this site for an active SAM prior to the OMT we suggest that changes in orbital parameters, as well as possibly changing Tethyan/Himalayan tectonics, caused this step change in the proto-monsoon system at this intermediate-depth site.
- Published
- 2021
17. The DeepMIP contribution to PMIP4: methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data, incorporating version 0.1 of the DeepMIP database
- Author
-
Hollis, C.J., Dunkley Jones, T., Anagnostou, E., Bijl, P.K., Cramwinckel, M.J., Cui, Y., Dickens, G.R., Edgar, K.M., Eley, Y., Evans, D., Foster, G.L., Frieling, J., Inglis, G.N., Kennedy, E.M., Kozdon, R., Lauretano, V., Lear, C.H., Littler, K., Lourens, L., Meckler, A.N., Naafs, B.D.A., Pälike, H., Pancost, R.D., Pearson, P.N., Röhl, U., Royer, D.L., Salzmann, U., Schubert, B.A., Seebeck, H., Sluijs, A., Speijer, R.P., Stassen, P., Tierney, J.E., Tripati, A.K., Wade, B.S., Westerhold, T., Witkowski, C.R., Zachos, J.C., Zhang, Y.G., Huber, M., Lunt, D.J., Hollis, C.J., Dunkley Jones, T., Anagnostou, E., Bijl, P.K., Cramwinckel, M.J., Cui, Y., Dickens, G.R., Edgar, K.M., Eley, Y., Evans, D., Foster, G.L., Frieling, J., Inglis, G.N., Kennedy, E.M., Kozdon, R., Lauretano, V., Lear, C.H., Littler, K., Lourens, L., Meckler, A.N., Naafs, B.D.A., Pälike, H., Pancost, R.D., Pearson, P.N., Röhl, U., Royer, D.L., Salzmann, U., Schubert, B.A., Seebeck, H., Sluijs, A., Speijer, R.P., Stassen, P., Tierney, J.E., Tripati, A.K., Wade, B.S., Westerhold, T., Witkowski, C.R., Zachos, J.C., Zhang, Y.G., Huber, M., and Lunt, D.J.
- Abstract
Back to topThe early Eocene (56 to 48 million years ago) is inferred to have been the most recent time that Earth's atmospheric CO2 concentrations exceeded 1000 ppm. Global mean temperatures were also substantially warmer than those of the present day. As such, the study of early Eocene climate provides insight into how a super-warm Earth system behaves and offers an opportunity to evaluate climate models under conditions of high greenhouse gas forcing. The Deep Time Model Intercomparison Project (DeepMIP) is a systematic model–model and model–data intercomparison of three early Paleogene time slices: latest Paleocene, Paleocene–Eocene thermal maximum (PETM) and early Eocene climatic optimum (EECO). A previous article outlined the model experimental design for climate model simulations. In this article, we outline the methodologies to be used for the compilation and analysis of climate proxy data, primarily proxies for temperature and CO2. This paper establishes the protocols for a concerted and coordinated effort to compile the climate proxy records across a wide geographic range. The resulting climate “atlas” will be used to constrain and evaluate climate models for the three selected time intervals and provide insights into the mechanisms that control these warm climate states. We provide version 0.1 of this database, in anticipation that this will be expanded in subsequent publications.
- Published
- 2019
18. A High‐Fidelity Benthic Stable Isotope Record of Late Cretaceous–Early Eocene Climate Change and Carbon‐Cycling
- Author
-
Barnet, J.S.K., Littler, K., Westerhold, T., Kroon, D., Leng, M.J., Bailey, I., Röhl, U., Zachos, J.C., Barnet, J.S.K., Littler, K., Westerhold, T., Kroon, D., Leng, M.J., Bailey, I., Röhl, U., and Zachos, J.C.
- Abstract
The Late Cretaceous–Early Paleogene is the most recent period in Earth history that experienced sustained global greenhouse warmth on multimillion year timescales. Yet, knowledge of ambient climate conditions and the complex interplay between various forcing mechanisms are still poorly constrained. Here we present a 14.75 million‐year‐long, high‐resolution, orbitally tuned record of paired climate change and carbon‐cycling for this enigmatic period (~67–52 Ma), which we compare to an up‐to‐date compilation of atmospheric pCO2 records. Our climate and carbon‐cycling records, which are the highest resolution stratigraphically complete records to be constructed from a single marine site in the Atlantic Ocean, feature all major transient warming events (termed “hyperthermals”) known from this time period. We identify eccentricity as the dominant pacemaker of climate and the carbon cycle throughout the Late Maastrichtian to Early Eocene, through the modulation of precession. On average, changes in the carbon cycle lagged changes in climate by ~23,000 years at the long eccentricity (405,000‐year) band, and by ~3,000–4,500 years at the short eccentricity (100,000‐year) band, suggesting that light carbon was released as a positive feedback to warming induced by orbital forcing. Our new record places all known hyperthermals of the Late Maastrichtian–Early Eocene into temporal context with regards to evolving ambient climate of the time. We constrain potential carbon cycle influences of Large Igneous Province volcanism associated with the Deccan Traps and North Atlantic Igneous Province, as well as the sensitivity of climate and the carbon‐cycle to the 2.4 million‐year‐long eccentricity cycle.
- Published
- 2019
19. A framework for Controlled Human Infection Model (CHIM) studies in Malawi: Report of a Wellcome Trust workshop on CHIM in Low Income Countries held in Blantyre, Malawi
- Author
-
Gordon, SB, Rylance, J, Luck, A, Jambo, K, Ferreira, DM, Manda-Taylor, L, Bejon, P, Ngwira, B, Littler, K, Seager, Z, Gibani, M, Gmeiner, M, Roestenberg, M, Mlombe, Y, and Wellcome Trust CHIM workshop participants
- Subjects
Economic growth ,medicine.medical_specialty ,wc_680 ,workshop report ,030231 tropical medicine ,Alternative medicine ,Medicine (miscellaneous) ,Library science ,Developing country ,wa_395 ,Methods for Diagnostic & Therapeutic Studies ,General Biochemistry, Genetics and Molecular Biology ,03 medical and health sciences ,0302 clinical medicine ,Controlled human infection model ,vaccine ,Medicine ,030212 general & internal medicine ,Wellcome Trust CHIM workshop participants ,Capacity development ,wa_30 ,CHIM ,business.industry ,Corporate governance ,Health Systems & Services Research ,Articles ,w_20.5 ,3. Good health ,wa_540 ,Host country ,Low and middle income countries ,wz_112 ,Open Letter ,business - Abstract
Controlled human infection model (CHIM) studies have pivotal importance in vaccine development, being useful for proof of concept, pathogenesis, down-selection and immunogenicity studies. To date, however, they have seldom been carried out in low and middle income countries (LMIC), which is where the greatest burden of vaccine preventable illness is found. This workshop discussed the benefits and barriers to CHIM studies in Malawi. Benefits include improved vaccine effectiveness and host country capacity development in clinical, laboratory and governance domains. Barriers include acceptability, safety and regulatory issues. The report suggests a framework by which ethical, laboratory, scientific and governance issues may be addressed by investigators considering or planning CHIM in LMIC.
- Published
- 2017
20. The DeepMIP contribution to PMIP4: experimental design for model simulations of the EECO, PETM, and pre-PETM
- Author
-
Lunt, D. J., Huber, M., Baatsen, M. L. J., Caballero, R., DeConto, R., Donnadieu, Y., Evans, D., Feng, R., Foster, G., Gasson, E., von der Heydt, A. S., Hollis, C. J., Kirtland Turner, S., Korty, R. L., Kozdon, R., Krishnan, S., Ladant, J. -B., Langebroek, P., Lear, C. H., LeGrande, A. N., Littler, K., Markwick, P., Otto-Bliesner, B., Pearson, P., Poulsen, C., Salzmann, U., Shields, C., Snell, K., Starz, M., Super, J., Tabour, C., Tierney, J., Tourte, G. J. L., Upchurch, G. R., Wade, B., Wing, S. L., Winguth, A. M. E., Wright, N., Zachos, J. C., Zeebe, R., Sub Physical Oceanography, and Marine and Atmospheric Research
- Abstract
Past warm periods provide an opportunity to evaluate climate models under extreme forcing scenarios, in particular high (> 800 ppmv) atmospheric CO2 concentrations. Although a post-hoc intercomparison of Eocene (~50 million years ago, Ma) climate model simulations and geological data has been carried out previously, models of past high-CO2 periods have never been evaluated in a consistent framework. Here, we present an experimental design for climate model simulations of three warm periods within the latest Paleocene and the early Eocene. Together these form the first phase of DeepMIP – the deeptime model intercomparison project, itself a group within the wider Paleoclimate Modelling Intercomparison Project (PMIP). The experimental design consists of three core paleo simulations and a set of optional sensitivity studies. The experimental design specifies and provides guidance on boundary conditions associated with palaeogeography, greenhouse gases, orbital configuration, solar constant, land surface parameters, and aerosols. Initial conditions, simulation length, and output variables are also specified. Finally, we explain how the geological datasets, which will be used to evaluate the simulations, will be developed.
- Published
- 2017
21. The geochemistry of modern calcareous barnacle shells and applications for palaeoenvironmental studies
- Author
-
Ullmann, C. V., Gale, A. S., Huggett, J., Wray, D., Frei, Robert, Korte, C., Broom-Fendley, S., Littler, K., Hesselbo, S. P., Frei, Regina, Ullmann, C. V., Gale, A. S., Huggett, J., Wray, D., Frei, Robert, Korte, C., Broom-Fendley, S., Littler, K., Hesselbo, S. P., and Frei, Regina
- Abstract
Thoracican barnacles of the Superorder Thoracicalcarea Gale, 2016 are sessile calcifiers which are ubiquitous in the intertidal zone and present from very shallow to the deepest marine environments; they also live as epiplankton on animals and detritus. The geochemical composition of their shell calcite has been shown to yield information about environmental conditions, but comprehensive analyses of barnacle shell geochemistry are so far lacking. Here, a dataset is reported for Mg/Ca, Sr/Ca, Mn/Ca, Fe/Ca, as well as carbon and oxygen isotope ratios for 42 species from the Balaniformes, Verruciformes, Scalpelliformes and Lepadiformes. Barnacles predominantly form low-Mg-calcite with very high Sr/Ca ratios averaging 4.2 mmol/mol. The Mn/Ca and Fe/Ca ratios in shell plates are variable and can exceed >4 mmol/mol in barnacles that are attached to manmade structures or live close to (anthropogenic) sources of Mn and Fe. No strong phylogenetic control on the average element/Ca ratios is observed in barnacles. The Balaniformes show a ca. 40 enrichment of Mg in their scuta and terga as compared to other shell plates-a pattern which is not seen in other barnacles. The combination of low to medium Mg/Ca ratios and high Sr/Ca ratios is rare for marine biogenic calcite. Barnacles may thus become important for robustly reconstructing past seawater composition, if this signature is also present in fossil barnacle calcite and can be used alongside other fossil taxa with different Sr incorporation behaviour. Carbon and oxygen isotope data support the view that the oxygen isotope thermometer for barnacles is robust and that most barnacle species form their calcite near isotopic equilibrium with ambient water. The Lepadiformes, however, show a tendency for strong co-variation of delta (super 13) C with delta (super 18) O values and depletion in (super 13) C and (super 18) O which is attributed to isotopic disequilibrium during shell secretion. Strong systematic fluctuations in Mg/Ca
- Published
- 2018
22. Evolving perspectives on broad consent for genomics research and biobanking in Africa. Report of the Second H3Africa Ethics Consultation Meeting, 11 May 2015
- Author
-
de Vries, J, Littler, K, Matimba, A, McCurdy, S, Ouwe Missi Oukem-Boyer, O, Seeley, J, and Tindana, P
- Abstract
A report on the Second H3Africa Ethics Consultation Meeting, which was held in Livingstone, Zambia on 11 May 2015. The meeting demonstrated considerable evolution by African Research Ethics Committees on thinking about broad consent as a consent option for genomics research and biobanking. The meeting concluded with a call for broader engagement with policy makers across the continent in order to help these recognise the need for guidance and regulation where these do not exist and to explore harmonisation where appropriate and possible.
- Published
- 2016
23. Frequency, magnitude and character of hyperthermal events at the onset of the Early Eocene Climatic Optimum
- Author
-
Lauretano, V., Littler, K., Polling, M., Zachos, J.C., Lourens, L.J., Stratigraphy and paleontology, NWO-VICI: Evolution of astronomically paced climate changes from Greenhouse to Icehouse world, Stratigraphy and paleontology, and NWO-VICI: Evolution of astronomically paced climate changes from Greenhouse to Icehouse world
- Subjects
Water mass ,Orbital forcing ,010504 meteorology & atmospheric sciences ,δ18O ,lcsh:Environmental protection ,Stratigraphy ,Holocene climatic optimum ,Permafrost ,010502 geochemistry & geophysics ,01 natural sciences ,Isotopes of oxygen ,Physical Geography and Environmental Geoscience ,Paleontology ,lcsh:Environmental pollution ,lcsh:TD169-171.8 ,lcsh:Environmental sciences ,0105 earth and related environmental sciences ,lcsh:GE1-350 ,Global and Planetary Change ,geography ,geography.geographical_feature_category ,δ13C ,Ridge ,13. Climate action ,lcsh:TD172-193.5 ,Geology - Abstract
Recent studies have shown that the Early Eocene Climatic Optimum (EECO) was preceded by a series of short-lived global warming events, known as hyperthermals. Here we present high-resolution benthic stable carbon and oxygen isotope records from ODP Sites 1262 and 1263 (Walvis Ridge, SE Atlantic) between ~ 54 and ~ 52 million years ago, tightly constraining the character, timing, and magnitude of six prominent hyperthermal events. These events, which include Eocene Thermal Maximum (ETM) 2 and 3, are studied in relation to orbital forcing and long-term trends. Our findings reveal an almost linear relationship between δ13C and δ18O for all these hyperthermals, indicating that the eccentricity-paced covariance between deep-sea temperature changes and extreme perturbations in the exogenic carbon pool persisted during these events towards the onset of the EECO, in accordance with previous observations for the Paleocene Eocene Thermal Maximum (PETM) and ETM2. The covariance of δ13C and δ18O during H2 and I2, which are the second pulses of the "paired" hyperthermal events ETM2-H2 and I1-I2, deviates with respect to the other events. We hypothesize that this could relate to a relatively higher contribution of an isotopically heavier source of carbon, such as peat or permafrost, and/or to climate feedbacks/local changes in circulation. Finally, the δ18O records of the two sites show a systematic offset with on average 0.2 ‰ heavier values for the shallower Site 1263, which we link to a slightly heavier isotopic composition of the intermediate water mass reaching the northeastern flank of the Walvis Ridge compared to that of the deeper northwestern water mass at Site 1262.
- Published
- 2015
- Full Text
- View/download PDF
24. International Ocean Discovery Program Expedition 353 preliminary report: Indian Monsoon Rainfall, 29 November 2014 – 29 January 2015
- Author
-
Clemens, Steven C., Kuhnt, Wolfgang, LeVay, Leah J., Anand, P., Ando, T., Bartol, M., Bolton, C. T., Ding, X., Gariboldi, K., Giosan, L., Hathorne, Edmund C., Huang, Y., Jaiswal, P., Kim, Sunghan, Kirkpatrick, J. B., Littler, K., Marino, G., Martinez, P., Naik, D., Peketi, A., Phillips, S. C., Robinson, M. M., Romero, O. E., Sagar, N., Taladay, K. B., Taylor, S. N., Thirumalai, K., Uramoto, G., Usui, Y., Wang, J., Yamamoto, M., and Zhou, L.
- Abstract
International Ocean Discovery Program (IODP) Expedition 353 (29 November 2014–29 January 2015) drilled six sites in the Bay of Bengal, recovering 4280 m of sediments during 32.9 days of on-site drilling. Recovery averaged 97%, including coring with the advanced piston corer, half-length advanced piston corer, and extended core barrel systems. The primary objective of Expedition 353 is to reconstruct changes in Indian monsoon circulation since the Miocene at tectonic to centennial timescales. Analysis of the sediment sections recovered will improve our understanding of how monsoonal climates respond to changes in forcing external to the Earth’s climate system (i.e., insolation) and changes in forcing internal to the Earth’s climate system, including changes in continental ice volume, greenhouse gases, sea level, and the ocean-atmosphere exchange of energy and moisture. All of these mechanisms play critical roles in current and future climate change in monsoonal regions. The primary signal targeted is the exceptionally low salinity surface waters that result, in roughly equal measure, from both direct summer monsoon precipitation to the Bay of Bengal and runoff from the numerous large river basins that drain into the Bay of Bengal. Changes in rainfall and surface ocean salinity are captured and preserved in a number of chemical, physical, isotopic, and biological components of sediments deposited in the Bay of Bengal. Expedition 353 sites are strategically located in key regions where these signals are the strongest and best preserved. Salinity changes at IODP Sites U1445 and U1446 (northeast Indian margin) result from direct precipitation as well as runoff from the Ganges-Brahmaputra river complex and the many river basins of peninsular India. Salinity changes at IODP Sites U1447 and U1448 (Andaman Sea) result from direct precipitation and runoff from the Irrawaddy and Salween river basins. IODP Site U1443 (Ninetyeast Ridge) is an open-ocean site with a modern surface water salinity very near the global mean but is documented to have recorded changes in monsoonal circulation over orbital to tectonic timescales. This site serves as an anchor for establishing the extent to which the north to south (19°N to 5°N) salinity gradient changes over time.
- Published
- 2015
25. The DeepMIP contribution to PMIP4: experimental design for model simulations of the EECO, PETM, and pre-PETM
- Author
-
Sub Physical Oceanography, Marine and Atmospheric Research, Lunt, D. J., Huber, M., Baatsen, M. L. J., Caballero, R., DeConto, R., Donnadieu, Y., Evans, D., Feng, R., Foster, G., Gasson, E., von der Heydt, A. S., Hollis, C. J., Kirtland Turner, S., Korty, R. L., Kozdon, R., Krishnan, S., Ladant, J. -B., Langebroek, P., Lear, C. H., LeGrande, A. N., Littler, K., Markwick, P., Otto-Bliesner, B., Pearson, P., Poulsen, C., Salzmann, U., Shields, C., Snell, K., Starz, M., Super, J., Tabour, C., Tierney, J., Tourte, G. J. L., Upchurch, G. R., Wade, B., Wing, S. L., Winguth, A. M. E., Wright, N., Zachos, J. C., Zeebe, R., Sub Physical Oceanography, Marine and Atmospheric Research, Lunt, D. J., Huber, M., Baatsen, M. L. J., Caballero, R., DeConto, R., Donnadieu, Y., Evans, D., Feng, R., Foster, G., Gasson, E., von der Heydt, A. S., Hollis, C. J., Kirtland Turner, S., Korty, R. L., Kozdon, R., Krishnan, S., Ladant, J. -B., Langebroek, P., Lear, C. H., LeGrande, A. N., Littler, K., Markwick, P., Otto-Bliesner, B., Pearson, P., Poulsen, C., Salzmann, U., Shields, C., Snell, K., Starz, M., Super, J., Tabour, C., Tierney, J., Tourte, G. J. L., Upchurch, G. R., Wade, B., Wing, S. L., Winguth, A. M. E., Wright, N., Zachos, J. C., and Zeebe, R.
- Published
- 2017
26. The DeepMIP contribution to PMIP4: experimental design for model simulations of the EECO, PETM, and pre-PETM (version 1.0)
- Author
-
Lunt, D. J., Huber, M., Anagnostou, E., Baatsen, M. L. J., Caballero, R., DeConto, R., Dijkstra, H. A., Donnadieu, Y., Evans, D., Feng, R., Foster, G. L., Gasson, E., von der Heydt, A. S., Hollis, C. J., Inglis, G. N., Jones, S. M., Kiehl, J., Turner, S. K., Korty, R. L., Kozdon, R., Krishnan, S., Ladant, J.-B., Langebroek, P. M., Lear, C. H., LeGrande, A. N., Littler, K., Markwick, P., Otto-Bliesner, B., Pearson, P., Poulsen, C. J., Salzmann, U., Shields, C., Snell, K., Stärz, M., Super, J., Tabor, C., Tierney, J. E., Tourte, G. J. L., Tripati, A., Upchurch, G. R., Wade, B. S., Wing, S. L., Winguth, A. M. E., Wright, N. M., Zachos, J. C., Zeebe, Richard E., Lunt, D. J., Huber, M., Anagnostou, E., Baatsen, M. L. J., Caballero, R., DeConto, R., Dijkstra, H. A., Donnadieu, Y., Evans, D., Feng, R., Foster, G. L., Gasson, E., von der Heydt, A. S., Hollis, C. J., Inglis, G. N., Jones, S. M., Kiehl, J., Turner, S. K., Korty, R. L., Kozdon, R., Krishnan, S., Ladant, J.-B., Langebroek, P. M., Lear, C. H., LeGrande, A. N., Littler, K., Markwick, P., Otto-Bliesner, B., Pearson, P., Poulsen, C. J., Salzmann, U., Shields, C., Snell, K., Stärz, M., Super, J., Tabor, C., Tierney, J. E., Tourte, G. J. L., Tripati, A., Upchurch, G. R., Wade, B. S., Wing, S. L., Winguth, A. M. E., Wright, N. M., Zachos, J. C., and Zeebe, Richard E.
- Abstract
Past warm periods provide an opportunity to evaluate climate models under extreme forcing scenarios, in particular high ( > 800 ppmv) atmospheric CO2 concentrations. Although a post hoc intercomparison of Eocene ( ∼ 50 Ma) climate model simulations and geological data has been carried out previously, models of past high-CO2 periods have never been evaluated in a consistent framework. Here, we present an experimental design for climate model simulations of three warm periods within the early Eocene and the latest Paleocene (the EECO, PETM, and pre-PETM). Together with the CMIP6 pre-industrial control and abrupt 4 × CO2 simulations, and additional sensitivity studies, these form the first phase of DeepMIP – the Deep-time Model Intercomparison Project, itself a group within the wider Paleoclimate Modelling Intercomparison Project (PMIP). The experimental design specifies and provides guidance on boundary conditions associated with palaeogeography, greenhouse gases, astronomical configuration, solar constant, land surface processes, and aerosols. Initial conditions, simulation length, and output variables are also specified. Finally, we explain how the geological data sets, which will be used to evaluate the simulations, will be developed.
- Published
- 2017
27. Base of the Toarcian Stage of the Lower Jurassic defined by the Global Boundary Stratotype Section and Point (GSSP) at the Peniche section (Portugal)
- Author
-
Rocha, Rogerio Bordalo da, Mattioli, E., Duarte, L. V., Pittet, Bernard, Elmi, S., Mouterde, R., Cabral, M. C., Comas-Rengifo, M. J., Gómez Fernández, J. J., Goy Goy, A., Hesselbo, S., Jenkyns, H. C., Littler, K., Mailliot, S., Oliveira, Luiz Carlos Veiga de, Osete, María Luisa, Perilli, N., Pinto, Susana, Ruget, Christiane, Suan, Guillaume, Rocha, Rogerio Bordalo da, Mattioli, E., Duarte, L. V., Pittet, Bernard, Elmi, S., Mouterde, R., Cabral, M. C., Comas-Rengifo, M. J., Gómez Fernández, J. J., Goy Goy, A., Hesselbo, S., Jenkyns, H. C., Littler, K., Mailliot, S., Oliveira, Luiz Carlos Veiga de, Osete, María Luisa, Perilli, N., Pinto, Susana, Ruget, Christiane, and Suan, Guillaume
- Abstract
The Global Stratotype Section and Point (GSSP) for the base of Toarcian Stage, Lower Jurassic, is placed at the base of micritic limestone bed 15e at Ponta do Trovão (Peniche, Lusitanian Basin, Portugal; coordinates: 39°22'15''N, 9°23'07''W), 80km north of Lisbon, and coincides with the mass occurrence of the ammonite Dactylioceras (Eodactylites). The Pliensbachian/ Toarcian boundary (PLB/TOA) is contained in a continuous section forming over 450m of carbonate-rich sediments. Tectonics, syn-sedimentary disturbance, metamorphism or significant diagenesis do not significantly affect this area. At the PLB/TOA, no vertical facies changes, stratigraphical gaps or hiatuses have been recorded. The base of the Toarcian Stage is marked in the bed 15e by the first occurrence of D. (E.) simplex, co-occurring with D. (E.) pseudocommune and D. (E.) polymorphum. The ammonite association of D. (Eodactylites) ssp. and other species e.g. Protogrammoceras (Paltarpites) cf. paltum, Lioceratoides aff. ballinense and Tiltoniceras aff. capillatum is particularly significant for the boundary definition and correlation with sections in different basins. Ammonites of the PLB/ TOA are taxa characteristic of both the Mediterranean and Northwest European provinces that allow reliable, global correlations. The PLB/TOA is also characterized by other biostratigraphical markers (brachiopods, calcareous nannofossils, ostracods and benthic foraminifers) and by high-resolution stable carbon and oxygen isotopes, and 87Sr/86Sr ratios that show distinctive changes just above the PLB/TOA, thus providing additional, powerful tools for global correlations. The PBL-TOA lies at the end of a second (and third) order cycle of sea-level change, and the top of bed 15e is interpreted as a sequence boundary. Cyclostratigraphy analysis is available for the Lower Toarcian of Ponta do Trovão. Detailed correlations with the Almonacid de la Cuba section (Iberian Range, Spain) provide complementary data of the ammonite
- Published
- 2016
28. Round Table Discussion: Data Sharing and Ethics of the Big Data
- Author
-
Littler, K., primary
- Published
- 2016
- Full Text
- View/download PDF
29. Evidence for global cooling in the Late Cretaceous
- Author
-
Linnert, Ch., Robinson, S.A., Lees, J.A., Bown, P.R., Pérez-Rodríguez, I., Petrizzo, M.R., Falzoni, F., Littler, K., Arz, J.A., and Russell, E.E.
- Abstract
The Late Cretaceous ‘greenhouse’ world witnessed a transition from one of the warmest climates of the past 140 million years to cooler conditions, yet still without significant continental ice. Low-latitude sea surface temperature (SST) records are a vital piece of evidence required to unravel the cause of Late Cretaceous cooling, but high-quality data remain illusive. Here, using an organic geochemical palaeothermometer (TEX86), we present a record of SSTs for the Campanian–Maastrichtian interval (~83–66¿Ma) from hemipelagic sediments deposited on the western North Atlantic shelf. Our record reveals that the North Atlantic at 35¿°N was relatively warm in the earliest Campanian, with maximum SSTs of ~35¿°C, but experienced significant cooling (~7¿°C) after this to
- Published
- 2014
30. Frequency, magnitude and character of hyperthermal events at the onset of the Early Eocene Climatic Optimum
- Author
-
Stratigraphy and paleontology, NWO-VICI: Evolution of astronomically paced climate changes from Greenhouse to Icehouse world, Lauretano, V., Littler, K., Polling, M., Zachos, J.C., Lourens, L.J., Stratigraphy and paleontology, NWO-VICI: Evolution of astronomically paced climate changes from Greenhouse to Icehouse world, Lauretano, V., Littler, K., Polling, M., Zachos, J.C., and Lourens, L.J.
- Published
- 2015
31. The Paleocene–Eocene Thermal Maximum at DSDP Site 277, Campbell Plateau, southern Pacific Ocean
- Author
-
Hollis, C. J., primary, Hines, B. R., additional, Littler, K., additional, Villasante-Marcos, V., additional, Kulhanek, D. K., additional, Strong, C. P., additional, Zachos, J. C., additional, Eggins, S. M., additional, Northcote, L., additional, and Phillips, A., additional
- Published
- 2015
- Full Text
- View/download PDF
32. Frequency, magnitude and character of hyperthermal events at the onset of the Early Eocene Climatic Optimum
- Author
-
Lauretano, V., primary, Littler, K., additional, Polling, M., additional, Zachos, J. C., additional, and Lourens, L. J., additional
- Published
- 2015
- Full Text
- View/download PDF
33. Supplementary material to "Onset of the Paleocene–Eocene Thermal Maximum in the southern Pacific Ocean (DSDP Site 277, Campbell Plateau)"
- Author
-
Hollis, C. J., primary, Hines, B. R., additional, Littler, K., additional, Villasante-Marcos, V., additional, Kulhanek, D. K., additional, Strong, C. P., additional, Zachos, J. C., additional, Eggins, S. M., additional, Northcote, L., additional, and Phillips, A., additional
- Published
- 2015
- Full Text
- View/download PDF
34. Onset of the Paleocene–Eocene Thermal Maximum in the southern Pacific Ocean (DSDP Site 277, Campbell Plateau)
- Author
-
Hollis, C. J., primary, Hines, B. R., additional, Littler, K., additional, Villasante-Marcos, V., additional, Kulhanek, D. K., additional, Strong, C. P., additional, Zachos, J. C., additional, Eggins, S. M., additional, Northcote, L., additional, and Phillips, A., additional
- Published
- 2015
- Full Text
- View/download PDF
35. Developing the science and methods of community engagement for genomic research and biobanking in Africa.
- Author
-
Tindana, P., Campbell, M., Marshall, P., Littler, K., Vincent, R., Seeley, J., de Vries, J., and Kamuya, D.
- Subjects
GENE libraries ,RECOMBINANT DNA ,HUMAN gene libraries ,GENOMES ,GENOMICS - Abstract
Historically, community engagement (CE) in research has been implemented in the fields of public health, education and agricultural development. In recent years, international discussions on the ethical and practical goals of CE have been extended to human genomic research and biobanking, particularly in the African context. While there is some consensus on the goals and value of CE generally, questions remain about the effectiveness of CE practices and how to evaluate this. Under the auspices of the Human Heredity and Health in Africa Initiative (H3Africa), the H3Africa CE working group organized a workshop in Stellenbosch, South Africa in March 2016 to explore the extent to which communities should be involved in genomic research and biobanking and to examine various methods of evaluating the effectiveness of CE. In this paper, we present the key themes that emerged fromthe workshop and make a case for the development of a rigorous application, evaluation and learning around approaches for CE that promote a more systematic process of engaging relevant communities. We highlight the key ways in which CE should be embedded into genomic research and biobanking projects. [ABSTRACT FROM AUTHOR]
- Published
- 2017
- Full Text
- View/download PDF
36. An emerging palaeoceanographic ‘missing link’: multidisciplinary study of rarely recovered parts of deep-sea Santonian–Campanian transition from Shatsky Rise
- Author
-
Ando, A., primary, Woodard, S. C., additional, Evans, H. F., additional, Littler, K., additional, Herrmann, S., additional, Macleod, K. G., additional, Kim, S., additional, Khim, B.-K., additional, Robinson, S. A., additional, and Huber, B. T., additional
- Published
- 2013
- Full Text
- View/download PDF
37. Onset of the Paleocene-Eocene Thermal Maximum in the southern Pacific Ocean (DSDP Site 277, Campbell Plateau).
- Author
-
Hollis, C. J., Hines, B. R., Littler, K., Villasante-Marcos, V., Kulhanek, D. K., Strong, C. P., Zachos, J. C., Eggins, S. M., Northcote, L., and Phillips, A.
- Abstract
Re-examination of a sediment core collected by the Deep Sea Drilling Project (DSDP Site 277) on the western margin of the Campbell Plateau, Southwest Pacific Ocean (paleolatitude of ~ 65° S), has identified an intact Paleocene-Eocene (P-E) boundary overlain by a 34 cm-thick record of the initial phase of the Paleocene-Eocene Thermal Maximum (PETM) within nannofossil chalk. The upper part of the PETM is truncated, either due to drilling disturbance or a sedimentary hiatus. An intact record of the onset of the PETM is indicated by a gradual decrease in δ
13 C values over 20 cm, followed by a 14 cm interval in which δ13 C is 2%0 lighter than uppermost Paleocene values. After accounting for effects of diagenetic alteration, we use δ18 O and Mg/Ca values from foraminiferal tests to determine that intermediate and surface waters warmed by ~ 6° at the onset of the PETM prior to the full development of the negative δ13 C excursion. After this initial warming, sea temperatures were relatively stable through the PETM, but declined abruptly across the unconformity that truncates the event at this site. Mg/Ca analysis of foraminiferal tests indicate peak intermediate and surface water temperatures of ~ 19 and ~ 32°C, respectively. These temperatures may be influenced by enhanced poleward ocean heat transport during the PETM and surface water values may also be biased towards warm season temperatures. [ABSTRACT FROM AUTHOR]- Published
- 2015
- Full Text
- View/download PDF
38. The Global Forum for Bioethics in Research: Past, present and future.
- Author
-
Littler, K., Millum, J., and Wassenaar, D. R.
- Subjects
BIOETHICS ,RESEARCH ethics ,FORUMS ,DEVELOPED countries ,DEVELOPING countries - Abstract
The Global Forum on Bioethics in Research (GFBR) served as a global platform for debate on ethical issues in international health research between 1999 and 2008, bringing together research ethics experts, researchers, policy makers and community members from developing and developed countries. In total, nine GFBR meetings were held on six continents. Work is currently underway to revive the GFBR. This paper describes the purpose and history of the GFBR and presents key elements for its reinstatement, future functioning and sustainability. Potential participants and sponsors are encouraged to contribute actively to the future of this unique international research ethics event. [ABSTRACT FROM AUTHOR]
- Published
- 2014
- Full Text
- View/download PDF
39. Nontraumatic soft tissue afflictions of the hand
- Author
-
wood, David, primary, Burton, R. I., additional, and Littler, K. W, additional
- Published
- 1976
- Full Text
- View/download PDF
40. Bound excitons in the narrow-gap semiconductor InSb
- Author
-
Seiler, D G, primary, Littler, K H, additional, and Littler, C L, additional
- Published
- 1986
- Full Text
- View/download PDF
41. Magnitude and pacing of Early Jurassic palaeoclimate change : chemostratigraphy and cyclostratigraphy of the British Lower Jurassic (Sinemurian-Pliensbachian)
- Author
-
Hudson, Alexander Joseph Leslie, Hesselbo, S., Littler, K., and Riding, J.
- Subjects
Geology ,Geoscience ,Palaeoclimate ,Paleoclimate ,Climate ,Sedimentology ,Cyclostratigraphy ,Stratigraphy ,Chemostratigraphy ,Jurassic ,Sinemurian ,XRF ,Burton Row ,Mochras ,Mercury Analysis ,Astrochronology ,Pliensbachian ,Somerset - Abstract
Palaeoclimate research in the Early Jurassic (201.4-174.1 million years ago) has historically focussed on geologically short, large-magnitude climatic events such as the Triassic-Jurassic (T-J) boundary mass extinction and the Toarcian Oceanic Anoxic Event (T-OAE). However, the climate system in the remaining ~18 myr of the Early Jurassic is significantly under studied; particularly given the identification of several smaller magnitude and crucially, less well understood carbon-cycle perturbations. In this thesis, I examine the Sinemurian-Early Pliensbachian from three sites: two archived British Geological Survey (BGS) boreholes (Mochras Borehole Cardigan Bay, Wales and Burton Row Borehole, Somerset, England) as-well-as the Robin Hood's Bay coastal exposure, Yorkshire, England. I present new, high-resolution multiple-proxy chemostratigraphy (hand-held X-ray fluorescence, stable isotope (δ13Cbulk-org & wood), Rock Eval pyrolysis and Mercury concentration data) through the interval, in order to elucidate the climate and carbon cycle evolution. I demonstrate the reproducibility of two negative carbon cycle excursions of ~4 ‰ δ13Corg associated with enhanced organic burial, marine flooding surfaces and shallow marine dysoxia; the first across the obtusum-oxynotum zone and the second at the Sinemurian-Pliensbachian boundary (raricostatum-jamesoni Zones). Mercury analysis of samples from the Burton Row borehole suggest LIP volcanism did not force climatic change in the Sinemurian and Early Pliensbachian with largely background values of Hg/TOC and no correlation of Mercury enrichment with intervals of isotopically light carbon (or dates of late phase CAMP). Spectral analysis of the high-resolution chemostratigraphy reveals evidence of Milankovitch cyclicity embedded within all studied records and proxies. This finding allows the generation of a robust orbitally tuned age model for the Sinemurian providing an estimate of 7.18 myr for the stage duration. The astronomically tuned age model suggests approximately 0.6-0.8 myr for the obtusum-oxynotum zone CIE and 1.8 myr for the SPBE. The events coincide precisely with the 2.4 myr long eccentricity maxima alluding to an orbital eccentricity control on the carbon cycle and climate. A novel methodology for quantifying the amount of time held within cryptic hiatuses is presented based upon integrating sequence stratigraphy and astrochronology. This method allows the quantification of at least 200-400 kyr of missing time held within several levels in the Robin Hoods bay Sinemurian record. To this end, the results of this thesis provide a compelling insight into an interval of time seldom studied. The analysis of the competing effects of large igneous province volcanism and orbital forcing gives strong evidence for the latter as the primary driver of palaeoclimate change in the Sinemurian and raises intriguing questions about the context of the larger- magnitude Early Jurassic OAEs. Geochemical data from multiple sites provides the means to generate a robust astrochronology for the Sinemurian that has implications for the apportioned time in the Early Jurassic.
- Published
- 2021
42. Investigating Paleogene strata from the tropical low latitudes : new insights from integrated chemostratigraphy, sedimentology, and biostratigraphy
- Author
-
Beasley, C., Littler, K., Kender, S., Hesselbo, S., Cotton, L., and Al Suwaidi, A.
- Subjects
Paleogene ,Palaeoceanography ,Palaeoclimatology ,Geochemistry ,Biostratigraphy ,Sedimentology ,Tropical low latitudes - Abstract
The Paleogene (66-23 Ma) was characterised by warming and cooling trends, on the scales of tens-of-thousands to millions of years, ultimately driven by tectonic processes (e.g., Zachos et al., 2001; Westerhold et al., 2020). Shorter period variability occurs due to changes in the Earth's orbital configuration, known as Milankovitch cyclicity, driving changes in the climate and carbon cycle. This high frequency variability is well-known from increasingly detailed sedimentological and geochemical records primarily from deep sea sedimentary archives; however, there are relatively fewer records from shallow and intermediate water depths or low latitude areas. In addition to these quasi-periodic Milankovitch cycles a number of significant global climate perturbations are recorded in the Paleogene rock record including the well known Paleocene-Eocene thermal maximum (PETM; ~56 Ma), where global sea surface temperatures are thought to have increased by ~3-4°C (e.g., McInerney & Wing, 2011). Low latitude areas, such as the Middle East and Arabian Sea, are thus far relatively understudied in terms of their combined palaeoenvironmental and biostratigraphic records through the Paleogene. As such, further high-resolution records from low latitude, shallow water and intermediate depth sites are important to discern orbital-scale variability and constrain how these regions responded to geologically rapid climate changes. This project applies a number of varied geochemical, sedimentological, and palaeontological techniques to material from both onshore shelf sea settings (Jordan and the United Arab Emirates) and open ocean (Arabian Sea) sediment cores. The overarching aim of the project is to analyse the changes in palaeoenvironment, palaeoclimate, and palaeoecology in low latitude, tropical environments of the Middle East and Arabian Sea through the Paleogene. The PETM is shown to have a limited impact on the oceanography and biota of this area, with the long-term warming from the late Paleocene to early Eocene instead causing shifts in biodiversity and influences of specific water masses. Similarly, the Oligocene-Miocene transition is shown to have an important role in the long-term evolution of the Arabian Sea region and proto-South Asian monsoon system.
- Published
- 2021
43. Fire & global change during key intervals of the Late Triassic & Early Jurassic with a focus on the Central Polish Basin
- Author
-
Pointer, R., Hesselbo, S., Belcher, C., and Littler, K.
- Subjects
622 ,geology ,palaeoclimate ,wildfire ,carbon-isotopes ,isotope geochemistry ,organic geochemistry ,Poland ,Polish Basin ,Triassic ,Jurassic - Abstract
Core from modern-day Poland recovering fluvial and paralic strata provides an excellent record of climatic and environmental changes in the Central Polish Basin during two key intervals of the Early Jurassic. Thick successions of Rhaetian-Hettangian and Pliensbachian-Toarcian age are examined using a number of techniques in order to understand the wildfire activity history, carbon-cycle interactions, and organic matter composition of sediments at two sites in the Central Polish Basin. Physical and geochemical proxies for wildfire activity show evidence of increased wildfire activity both prior to and after the Toarcian Oceanic Anoxic Event (OAE) at the Kazewy-1 site, with suppression of wildfire activity during the negative carbon-isotope excursion of the OAE. Correlation with published wildfire activity proxy records from additional sites in the Tethyan realm shows that this pattern was not limited to the Central Polish Basin, but is part of a wider, regional change. Additionally, new wildfire activity proxy records show increased wildfire activity across the Triassic-Jurassic Boundary at the Kaszewy-1 and Niekłań PIG-1 sites in the Central Polish Basin, correlating with other contemporaneous proxy records from Denmark and Greenland. New carbon-isotope records generated from terrestrial organic matter from the Niekłań PIG-1 core show trends towards heavier δ¹³C values immediately after the Triassic-Jurassic Boundary, providing evidence of a perturbation to the carbon-cycle at this time. Exploratory investigation of sediments from the Kaszewy-1 core provides a new record of BIT indices of Early Jurassic sediments, surpassing the oldest-known use of this terrestrial organic matter input proxy. Additionally, a newly-developed technique is used to investigate carbon-isotope variability in fossil terrestrial organic matter across the Toarcian Oceanic Anoxic Event carbon-isotope excursions. A new record of individual phytoclast δ¹³C values demonstrates that, despite δ¹³C variability between phytoclasts from a single horizon, larger overall trends in δ¹³C values can be identified from single phytoclast δ¹³C measurements. Core from modern-day Poland recovering fluvial and paralic strata provides an excellent record of climatic and environmental changes in the Central Polish Basin during two key intervals of the Early Jurassic. Thick successions of Rhaetian-Hettangian and Pliensbachian-Toarcian age are examined using a number of techniques in order to understand the wildfire activity history, carbon-cycle interactions, and organic matter composition of sediments at two sites in the Central Polish Basin. Physical and geochemical proxies for wildfire activity show evidence of increased wildfire activity both prior to and after the Toarcian Oceanic Anoxic Event (OAE) at the Kazewy-1 site, with suppression of wildfire activity during the negative carbon-isotope excursion of the OAE. Correlation with published wildfire activity proxy records from additional sites in the Tethyan realm shows that this pattern was not limited to the Central Polish Basin, but is part of a wider, regional change. Additionally, new wildfire activity proxy records show increased wildfire activity across the Triassic-Jurassic Boundary at the Kaszewy-1 and Niekłań PIG-1 sites in the Central Polish Basin, correlating with other contemporaneous proxy records from Denmark and Greenland. New carbon-isotope records generated from terrestrial organic matter from the Niekłań PIG-1 core show trends towards heavier δ¹³C values immediately after the Triassic-Jurassic Boundary, providing evidence of a perturbation to the carbon-cycle at this time. Exploratory investigation of sediments from the Kaszewy-1 core provides a new record of BIT indices of Early Jurassic sediments, surpassing the oldest-known use of this terrestrial organic matter input proxy. Additionally, a newly-developed technique is used to investigate carbon-isotope variability in fossil terrestrial organic matter across the Toarcian Oceanic Anoxic Event carbon-isotope excursions. A new record of individual phytoclast δ¹³C values demonstrates that, despite δ¹³C variability between phytoclasts from a single horizon, larger overall trends in δ¹³C values can be identified from single phytoclast δ¹³C measurements.
- Published
- 2019
44. Investigating climate change and carbon cycling during the Latest Cretaceous to Paleogene (~67-52 million years ago) : new geochemical records from the South Atlantic and Indian Oceans
- Author
-
Barnet, J., Littler, K., Kroon, D., and Bailey, I.
- Subjects
551.46 ,Paleoceanography ,Palaeoceanography ,Paleoclimate ,Palaeoclimate ,Orbital forcing ,Milankovitch cyclicity ,Stable carbon isotopes ,Stable oxygen isotopes ,Trace metals ,Foraminifera ,Cretaceous ,Paleogene ,Maastrichtian ,K/Pg boundary ,Paleocene ,Eocene ,South Atlantic ,Indian Ocean ,Walvis Ridge ,Ninetyeast Ridge ,Ocean Drilling Program ,International Ocean Discovery Program - Abstract
The Late Cretaceous–early Paleogene is the most recent period of Earth history with a dynamic carbon cycle that experienced sustained global greenhouse warmth and can offer a valuable insight into our anthropogenically-warmer future world. Yet, knowledge of ambient climate conditions and evolution of the carbon cycle at this time, along with their relation to forcing mechanisms, are still poorly constrained. In this thesis, I examine marine sediments recovered from the South Atlantic Walvis Ridge (ODP Site 1262) and Indian Ocean Ninetyeast Ridge (IODP Site U1443 and ODP Site 758), to shed new light on the evolution of the climate and carbon cycle from the Late Maastrichtian through to the Early Eocene (~67.10–52.35 Ma). The overarching aims of this thesis are: 1) to identify the long-term trends and principle forcing mechanisms driving the climate and carbon cycle during this time period, through construction of 14.75 million-year-long, orbital-resolution (~1.5–4 kyr), stratigraphically complete, benthic stable carbon (δ13Cbenthic) and oxygen (δ18Obenthic) isotope records; 2) to investigate in more detail the climatic and carbon-cycle perturbations of the Early–Middle Paleocene (e.g., the Dan-C2 event, Latest Danian Event and the Danian/Selandian Transition Event) and place these in their proper (orbital) temporal context; 3) to investigate the Late Maastrichtian warming event and its relationship to the eruption of the Deccan Traps Large Igneous Province, as well as its role (if any) in the subsequent Cretaceous/Paleogene (K/Pg) mass extinction; 4) to provide the first orbital-resolution estimates of temperature and carbonate chemistry variability from the low latitude Indian Ocean spanning the Late Paleocene–Early Eocene, through analysis of trace element and stable isotope data from multiple foraminiferal species. Taken together, the results presented in this thesis provide a critical new insight into the dynamic evolution of the climate and carbon cycle during the greenhouse world of the early Paleogene, and shed light on the potential forcing mechanisms driving the climate and carbon cycle during this time.
- Published
- 2018
45. Health gain among psychiatric patients
- Author
-
Littler, K.
- Published
- 1994
- Full Text
- View/download PDF
46. Equitable access to pandemic products demands stronger public governance.
- Author
-
Strobeyko A, Atuire CA, Faden R, Ho CWL, Ido V, Kamal-Yanni M, Kavanagh M, Littler K, Paremoer L, Phelan AL, Storeng KT, Upshur R, and Moon S
- Abstract
Competing Interests: The conception of this Comment was a collective effort based on group discussion. Ideas were exchanged in nine meetings of the WHO Ethics & Governance Sub-Working Group on Pandemic-Related Products between June 22, 2023, and June 10, 2024. AS and SM co-wrote the first and subsequent drafts of the manuscript. CAA, RF, CWLH, VI, MK-Y, MK, KL, LP, ALP, KTS, and RU contributed comments and suggestions on each subsequent draft and discussed them during group meetings and over email. All authors contributed to the input, review, analysis, and editing. AS and SM managed the process of reviews and edits. All authors are members of the WHO Ethics & Governance Sub-Working Group on Pandemic-Related Products set up to advise WHO on its role in governance of health products. The working group reported their independent findings to the WHO Chief Scientist. AS reports consultancy at WHO with payments from a Wellcome Trust grant (222525/Z/21/Z) and a grant from the Swiss National Science Foundation (221399). KL declares two Wellcome Trust grants (222525/Z/21/Z and 306679/Z/23/Z). KTS declares a grant from the Norwegian Research Council (301929). MK-Y reports consultancies for UNAIDS. RU declares co-chairing the WHO Ethics & Governance Working Group. SM reports grants paid to her institution from Pax Sapiens, Bill & Melinda Gates Foundation, Resolve to Save Lives, Permanent Mission of the Republic of Korea (to the UN Office and other international organisations in Geneva), and the Federal Office of Foreign Affairs, Switzerland. No authors were employed or funded by the US National Institutes of Health during this work. The listed funding sources did not exert any influence over the preparation of the manuscript or the decision to submit for publication. All authors have had access to the data, research, and analysis used in the preparation of this Comment and jointly accept responsibility for its publication.
- Published
- 2024
- Full Text
- View/download PDF
47. Research ethics and artificial intelligence for global health: perspectives from the global forum on bioethics in research.
- Author
-
Shaw J, Ali J, Atuire CA, Cheah PY, Español AG, Gichoya JW, Hunt A, Jjingo D, Littler K, Paolotti D, and Vayena E
- Subjects
- Humans, Global Health, South Africa, Ethics, Research, Artificial Intelligence, Bioethics
- Abstract
Background: The ethical governance of Artificial Intelligence (AI) in health care and public health continues to be an urgent issue for attention in policy, research, and practice. In this paper we report on central themes related to challenges and strategies for promoting ethics in research involving AI in global health, arising from the Global Forum on Bioethics in Research (GFBR), held in Cape Town, South Africa in November 2022., Methods: The GFBR is an annual meeting organized by the World Health Organization and supported by the Wellcome Trust, the US National Institutes of Health, the UK Medical Research Council (MRC) and the South African MRC. The forum aims to bring together ethicists, researchers, policymakers, research ethics committee members and other actors to engage with challenges and opportunities specifically related to research ethics. In 2022 the focus of the GFBR was "Ethics of AI in Global Health Research". The forum consisted of 6 case study presentations, 16 governance presentations, and a series of small group and large group discussions. A total of 87 participants attended the forum from 31 countries around the world, representing disciplines of bioethics, AI, health policy, health professional practice, research funding, and bioinformatics. In this paper, we highlight central insights arising from GFBR 2022., Results: We describe the significance of four thematic insights arising from the forum: (1) Appropriateness of building AI, (2) Transferability of AI systems, (3) Accountability for AI decision-making and outcomes, and (4) Individual consent. We then describe eight recommendations for governance leaders to enhance the ethical governance of AI in global health research, addressing issues such as AI impact assessments, environmental values, and fair partnerships., Conclusions: The 2022 Global Forum on Bioethics in Research illustrated several innovations in ethical governance of AI for global health research, as well as several areas in need of urgent attention internationally. This summary is intended to inform international and domestic efforts to strengthen research ethics and support the evolution of governance leadership to meet the demands of AI in global health research., (© 2024. The Author(s).)
- Published
- 2024
- Full Text
- View/download PDF
48. Digital tools for youth health promotion: principles, policies and practices in sub-Saharan Africa.
- Author
-
Ferretti A, Adjei KK, Ali J, Atuire C, Ayuk BT, Banougnin BH, Cengiz N, Gichoya J, Jjingo D, Juma DO, Kotze W, Krubiner C, Littler K, McCradden MD, Moodley K, Naidoo M, Nair G, Obeng-Kyereh K, Oliver K, Ralefala D, Toska E, Wekesah FM, Wright J, and Vayena E
- Subjects
- Humans, Adolescent, South Africa, Health Promotion, Health Policy, Digital Health
- Abstract
Although digital health promotion (DHP) technologies for young people are increasingly available in low- and middle-income countries (LMICs), there has been insufficient research investigating whether existing ethical and policy frameworks are adequate to address the challenges and promote the technological opportunities in these settings. In an effort to fill this gap and as part of a larger research project, in November 2022, we conducted a workshop in Cape Town, South Africa, entitled 'Unlocking the Potential of Digital Health Promotion for Young People in Low- and Middle-Income Countries'. The workshop brought together 25 experts from the areas of digital health ethics, youth health and engagement, health policy and promotion and technology development, predominantly from sub-Saharan Africa (SSA), to explore their views on the ethics and governance and potential policy pathways of DHP for young people in LMICs. Using the World Café method, participants contributed their views on (i) the advantages and barriers associated with DHP for youth in LMICs, (ii) the availability and relevance of ethical and regulatory frameworks for DHP and (iii) the translation of ethical principles into policies and implementation practices required by these policies, within the context of SSA. Our thematic analysis of the ensuing discussion revealed a willingness to foster such technologies if they prove safe, do not exacerbate inequalities, put youth at the center and are subject to appropriate oversight. In addition, our work has led to the potential translation of fundamental ethical principles into the form of a policy roadmap for ethically aligned DHP for youth in SSA., (© The Author(s) 2024. Published by Oxford University Press.)
- Published
- 2024
- Full Text
- View/download PDF
49. Taking stock: Is gene drive research delivering on its principles?
- Author
-
Roberts AJ, Hackett K, Coche I, James SL, Littler K, Santos M, and Emerson CI
- Subjects
- Humans, Biomedical Research ethics, Gene Drive Technology methods
- Abstract
Gene drive technology has been recognized for its potential to provide durable and cost-effective solutions for previously intractable problems in public health, conservation, and agriculture. In recognition of the rapid advances in this field, in 2016 the U.S. National Academies of Sciences, Engineering, and Medicine issued a report making several recommendations aimed at researchers, funders, and policymakers for the safe and responsible research and development of gene drive technology. Subsequently, in 2017 sixteen global organizations self-identifying as sponsors and supporters of gene drive research became public signatories committed to the 'Principles for Gene Drive Research' which were inspired by the report's recommendations. Herein we reflect on the progress of gene drive research in relation to the ethical principles laid out and committed to by the signatories to the Principles. Our analysis indicates high levels of alignment with the Principles in the field of gene drive research. The manuscript also discusses the Gene Drive Research Forum, which had its genesis in the publication of the Principles. Discussions between participants at the latest meeting of the Forum point to the work that lies ahead for gene drive research in line with the Principles. Going forward the gene drive research community can productively focus on: i) safety and efficacy criteria for open release, ii) risk assessment frameworks and methods, iii) more downstream technical, regulatory and policy considerations for field evaluations and implementation, iv) continued transparency and developing mechanisms of accountability, and v) strengthening capacity in locales of potential release and expected drive spread., Competing Interests: No competing interests were disclosed., (Copyright: © 2024 Roberts AJ et al.)
- Published
- 2024
- Full Text
- View/download PDF
50. Ethical approval for controlled human infectious model clinical trial protocols - A workshop report.
- Author
-
Jamrozik E, Littler K, Meln I, Van Molle W, Morel S, Olesen OF, Rubbrecht M, Balasingam S, and Neels P
- Subjects
- Humans, Healthy Volunteers, Research Design, Drug Development
- Abstract
Controlled Human Infectious Model studies (CHIM) involve deliberately exposing volunteers to pathogens. To discuss ethical issues related to CHIM, the European Vaccine Initiative and the International Alliance for Biological Standardization organised the workshop "Ethical Approval for CHIM Clinical Trial Protocols", which took place on May 30-31, 2023, in Brussels, Belgium. The event allowed CHIM researchers, regulators, ethics committee (EC) members, and ethicists to examine the ethical criteria for CHIM and the role(s) of CHIM in pharmaceutical development. The discussions led to several recommendations, including continued assurance that routine ethical requirements are met, assurance that participants are well-informed, and that preparation of study documents must be both ethically and scientifically sound from an early stage. Study applications must clearly state the rationale for the challenge compared to alternative study designs. ECs need to have clear guidance and procedures for evaluating social value and assessing third-party risks. Among other things, public trust in research requires minimisation of harm to healthy volunteers and third-party risk. Other important considerations include appropriate stakeholder engagement, public education, and access to health care for participants after the study., Competing Interests: Declaration of competing interest All authors declare no competing interests., (Copyright © 2024. Published by Elsevier Ltd.)
- Published
- 2024
- Full Text
- View/download PDF
Catalog
Discovery Service for Jio Institute Digital Library
For full access to our library's resources, please sign in.