Search

Your search keyword '"Zhuang, Guangchao"' showing total 30 results
Start Over Author "Zhuang, Guangchao"
30 results on '"Zhuang, Guangchao"'

3. Mineralization kinetics of biosiliceous sediments in hot subseafloors

Author

Aiello, Ivano W., Höfig, Tobias W., Riboulleau, Armelle, Teske, Andreas P., Lizarralde, Daniel, Ash, Jeanine L., Bojanova, Diana P., Buatier, Martine D., Edgcomb, Virginia P., Galerne, Christophe Y., Gontharet, Swanne, Heuer, Verena B., Jiang, Shijun, Kars, Myriam A.C., Kim, Ji-Hoon, Koornneef, Louise M.T., Marsaglia, Kathleen M., Meyer, Nicolette R., Morono, Yuki, Negrete-Aranda, Raquel, Neumann, Florian, Pastor, Lucie C., Peña-Salinas, Manet E., Pérez-Cruz, Ligia L., Ran, Lihua, Sarao, John A., Schubert, Florian, Khogenkumar Singh, S., Stock, Joann M., Toffin, Laurent, Xie, Wei, Yamanaka, Toshiro, and Zhuang, Guangchao

Published
2024
Full Text
View/download PDF

5. Nitrogen isotope homogenization of dissolved ammonium with depth and 15N enrichment of ammonium during incorporation into expandable layer silicates in organic-rich marine sediment from Guaymas Basin, Gulf of California

Author

Aiello, Ivano W., Ash, Jeanine L., Bojanova, Diana P., Buatier, Martine D., Edgcomb, Virginia P., Galerne, Christophe Y., Gontharet, Swanne, Heuer, Verena B., Jiang, Shijun, Kars, Myriam A.C., Koornneef, Louise M.T., Marsaglia, Kathleen M., Meyer, Nicolette R., Morono, Yuki, Negrete-Aranda, Raquel, Neumann, Florian, Peña-Salinas, Manet E., Pérez-Cruz, Ligia L., Ran, Lihua, Riboulleau, Armelle, Sarao, John A., Schubert, Florian, Singh, S. Khogenkumar, Stock, Joann M., Toffin, Laurent, Xie, Wei, Zhuang, Guangchao, Yamanaka, Toshiro, Sakamoto, Arisa, Kiyokawa, Kanon, Jo, Jaeguk, Onishi, Yuji, Kuwahara, Yoshihiro, Kim, Ji-Hoon, Pastor, Lucie C., Teske, Andreas, Lizarralde, Daniel, and Höfig, Tobias W.

Published
2024
Full Text
View/download PDF

7. What Causes Excess Deepening of the Sediment Mixed Layer in the Deep Ocean?

Author

Zhu, Zenghui, primary, Yu, Huaming, additional, Bianchi, Thomas S., additional, Lian, Ergang, additional, Burnett, William C., additional, Paytan, Adina, additional, Guo, Xiaoyi, additional, Zhao, Shibin, additional, Zhuang, Guangchao, additional, Men, Wu, additional, Li, Sanzhong, additional, Yu, Zhigang, additional, and Xu, Bochao, additional

Published
2024
Full Text
View/download PDF

15. Heat flow and thermal regime in the Guaymas Basin, Gulf of California: Estimates of conductive and advective heat transport

Author

Neumann, Florian, Negrete-Aranda, Raquel, Harris, Robert, Contreras, Juan, Galerne, Christophe, Peña-Salinas, Manet, Spelz, Ronald, Teske, Andreas, Lizarralde, Daniel, Höfig, Tobias, Aiello, Ivano, Ash, Janine, Bojanova, Diana, Buatier, Martine, Edgcomb, Virginia, Gontharet, Swanne, Heuer, Verena, Jiang, Shijun, Kars, Myriam A.C., Kim, Ji‐hoon, Koornneef, Louise M.T., Marsaglia, Kathleen, Meyer, Nicolette, Morono, Yuki, Pastor, Lucie, Pérez Cruz, Ligia, Ran, Lihua, Riboulleau, Armelle, Sarao, John, Schubert, Florian, Singh, S. Khogenkumar, Stock, Joann, Toffin, Laurent M.A.A., Xie, Wei, Yamanaka, Toshiro, Zhuang, Guangchao, Centro de Investigacion Cientifica y de Education Superior de Ensenada [Mexico] (CICESE), College of Earth, Ocean and Atmospheric Sciences [Corvallis] (CEOAS), Oregon State University (OSU), Universität Bremen, Universidad Autónoma de Baja California (UABC), University of North Carolina [Chapel Hill] (UNC), University of North Carolina System (UNC), Woods Hole Oceanographic Institution (WHOI), International Ocean Discovery Program, Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Cycles biogéochimiques marins : processus et perturbations (CYBIOM), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Center for Marine Environmental Sciences [Bremen] (MARUM), Geological Sciences, Florida State University [Tallahassee] (FSU), Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Laboratoire Environnement Profond (LEP), Etudes des Ecosystèmes Profonds (EEP), and Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)

Subjects
Guyamas Basin, [SDE]Environmental Sciences, IODP Expedition 385, Geology, Heat Flow, Heat Transfer
Abstract

Heat flow is estimated at eight sites drilled during the International Ocean Discovery Program Expedition 385 into the Guaymas Basin, Gulf of California. The expedition sought to understand the thermal regime of the basin and heat transfer between off-axis sills intruding the organic-rich sediments of the Guaymas Basin, and the basin floor. The distinct sedimentation rates, active tectonics, and magmatism makes the basin interesting for scientific discoveries. Results show sedimentation corrected heat flow values range 119-221 mW/m2 in the basin and 257-1003 mW/m2 at the site of a young sill intrusion, denominated Ringvent. Thermal analysis shows that heat in the Guaymas Basin is being dissipated by conduction for plate ages >0.2 Ma, whereas younger plate ages are in a state of transient cooling by both conduction and advection. Drilling sites show that Ringvent is an active sill being cooled down slowly by circulating fluids with discharge velocities 10–200 mm/yr. Possible recharge sites are located ~1 km away from the sill's border. Modeling of the heat output at Ringvent indicates a sill thickness of ~240 m. A simple order-of-magnitude model predicts that relatively small amounts of magma are needed to account for the elevated heat flow in non-volcanic, sediment-filled rifts like the central and northern Gulf of California in which heating of the upper crust is achieved via advection by sill emplacement and hydrothermal circulation. Multiple timescales of cooling control the crustal, chemical and biological evolution of the Guaymas Basin. Here we recognize at least four timescales: the time interval between intrusions (~103 yr), the thermal relaxation time of sills (~104 yr), the characteristic cooling time of the sediments (~105 yr), and the cooling of the entire crust at geologic timescales.

Published
2023

16. Exploration of Deep Ocean Ferromanganese Nodule Fields Using Radon as a Tracer

Author

Guo, Xiaoyi, primary, Xu, Bochao, additional, Yu, Huaming, additional, Burnett, William C., additional, Li, Sanzhong, additional, Lian, Ergang, additional, Zhu, Zenghui, additional, Zhao, Shibin, additional, Chen, Guangquan, additional, Duan, Xiaoyong, additional, Dimova, Natasha, additional, Wang, Yanni, additional, Zhuang, Guangchao, additional, and Yu, Zhigang, additional

Published
2022
Full Text
View/download PDF

19. Magma-sediment mingling processes, control and longevity of related hydrothermal systems – Implications for the Earth’s Carbon-, Plate-, Life-Cycles (IODP Exp 385, Guaymas Basin, Gulf of California)

Author

Galerne, Christophe, Bach, Wolfgang, Berndt, Christian, Schwark, Lorenz, Höfig, Tobias, Buatier, Martine, Cheviet, Alban, Kahl, Wolf-Achim, Hasenclever, Jörg, Lizarralde, Daniel, Stockhausen, Martin, Wiggers, Christin, Karstens, Jens, Monien, Patrick, Teske, Andreas, Aiello, Ivano W., Ash, Jeanine L., Bojanova, Diana P., Edgcomb, Virginia P., Gontharet, Swanne, Heuer, Verena B., Jiang, Shijun, Kars, Myriam A.C., Singh, S. Khogenkumar, Kim, Ji-Hoon, Koornneef, Louise M.T., Marsaglia, Kathleen M., Meyer, Nicolette R., Morono, Yuki, Negrete-Aranda, Raquel, Neumann, Florian, Pastor, Lucie C., Pena-Salinas, Manet E., Cruz, Ligia L. Perez, Ran, Lihua, Riboulleau, Armelle, Sarao, John A., Schubert, Florian, Stock, Joann M., Toffin, Laurent M.A.A., Xie, Wei, Yamanaka, Toshiro, Zhuang, Guangchao, Ortega, Rodrigo Perez, Geoscience Department and MARUM, University of Bremen, Helmholtz Centre for Ocean Research [Kiel] (GEOMAR), Institute of Geosciences [Kiel], Christian-Albrechts-Universität zu Kiel (CAU), Curtin University [Perth], Planning and Transport Research Centre (PATREC), International Ocean Discovery Program, Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC), University of Bremen, University of Hamburg, Woods Hole Oceanographic Institution (WHOI), University of North Carolina [Chapel Hill] (UNC), University of North Carolina System (UNC), Cycles biogéochimiques marins : processus et perturbations (CYBIOM), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Geological Sciences, Florida State University [Tallahassee] (FSU), Kyung Hee University (KHU), Kochi Institute for Core Sample Research, and Japan Agency for Marine-Earth Science and Technology (JAMSTEC)

Subjects
[SDE]Environmental Sciences
Abstract

Magma-sediment mingling occurring in shallow porous sediments is mainly investigated through field observations of old exhumed rift basins. During the IODP Expedition 385 we have drilled through the shallow sills emplaced in the active rift of the Guaymas Basin, Gulf of California. The results of this expedition enable a pioneer study of the impact of recent magma-sediment mingling processes leading to peperite formation. Furthermore, it provides a present-day geological context to investigate and quantify the impact of this mingling process on the element cycles in subsurface sediments, and temporal evolution of the microbial habitat associated with epithermal hydrothermal fluid circulation. Our approach of exploring magma-sediment mingling processes includes laboratory experiments, numerical modelling, and identification of specific field analogues in addition to petrological and geochemical constraints.Using these modern techniques, we review here the discoveries made during the IODP Expedition 385 and present preliminary results from our post-cruise research from the perspective of the peperite formation. We report here petrographic and geochemical evidence of magma sediment hybridization indicative of an intense mingling process inferred to occur during the emplacement phase. The rheology of the soft, unconsolidated sediment controls and explains the various intrusion shapes and dimensions. Numerical simulation results indicate that heat dissipation in this context is much less efficient, which in turn considerably decreases the amount of thermogenic gas mobilized through thermal cracking in the contact aureole of sills. Additionally, we observe that hydrothermal pipe systems established during the cooling phase of sill emplacement can remain active at moderate- to low-temperature state after the heat of the sill has vanished. Using 2D seismic information and IODP drilling results, we were able to reconstruct the 3D structure of the sill at depth. It is funnel-shaped and roots in a depth where geothermal fluids can ascend from. The temperature found at these depths is consistent with the background geothermal gradient, suggesting that the large heat flow anomaly found at Hole U1548C is the mere expression of the active hydrothermal circulation fuelled by deeply sourced geothermal fluids.These potentially long-lasting hydrothermal systems provide preferable temperature and energetic conditions for microbial activity to thrive, with mildly degraded petroleum components from below and water recharge from above. Moreover, evidence indicates that the sill at Site U1547 is non-unique at the scale of the Guaymas Basin. How many of these catabolic reactors form at the early rifting phase? Can this process perhaps trigger peaks in subsurface biomass production associated with new continental margin formation? Our research heralds the dawn of a new paradigm. We suggest that in the context of a nascent ocean, sill emplacement in the first 500 m of sediments may power life instead of suppressing it.

Published
2022

20. Biological Sulfate Reduction in Deep Subseafloor Sediment of Guaymas Basin

Author

Nagakura, Toshiki, Schubert, Florian, Wagner, Dirk, Kallmeyer, Jens, Teske, Andreas, Lizarralde, Daniel, W., Tobias, Aiello, Ivano W., Ash, Jeanine L., Bojanova, Diana P., Buatier, Martine D., Edgcomb, Virginia P., Galerne, Christophe Y., Gontharet, Swanne, Heuer, Verena B., Jiang, Shijun, Kars, Myriam A.C., Singh, S. Khogenkumar, Kim, Ji-Hoon, Koornneef, Louise M.T., Marsaglia, Kathleen M., Meyer, Nicolette R., Morono, Yuki, Negrete-Aranda, Raquel, Neumann, Florian, Pastor, Lucie C., Pena-Salinas, Manet E., Cruz, Ligia L. Perez, Ran, Lihua, Riboulleau, Armelle, Sarao, John A., Stock, Joann M., Toffin, Laurent M.A.A., Xie, Wei, Zhuang, Guangchao, Ortega, Rodrigo Perez, Institute of Molecular Medicine and Cell Research (ZBMZ), University of Freiburg [Freiburg], GeoForschungsZentrum - Helmholtz-Zentrum Potsdam (GFZ), Institute of Earth and Environmental Science [Potsdam], University of Potsdam = Universität Potsdam, University of North Carolina [Chapel Hill] (UNC), University of North Carolina System (UNC), Woods Hole Oceanographic Institution (WHOI), Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG), Institut national des sciences de l'Univers (INSU - CNRS)-Université du Littoral Côte d'Opale (ULCO)-Université de Lille-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Nord]), Geological Sciences, Florida State University [Tallahassee] (FSU), and Kyung Hee University (KHU)

Subjects
Microbiology (medical), sulfate reduction subsurface life deep biosphere thermophiles Guaymas Basin, sulfate reduction, [SDE]Environmental Sciences, deep biosphere, Guaymas Basin, subsurface life, Microbiology, thermophiles
Abstract

Sulfate reduction is the quantitatively most important process to degrade organic matter in anoxic marine sediment and has been studied intensively in a variety of settings. Guaymas Basin, a young marginal ocean basin, offers the unique opportunity to study sulfate reduction in an environment characterized by organic-rich sediment, high sedimentation rates, and high geothermal gradients (100–958°C km−1). We measured sulfate reduction rates (SRR) in samples taken during the International Ocean Discovery Program (IODP) Expedition 385 using incubation experiments with radiolabeled 35SO42− carried out at in situ pressure and temperature. The highest SRR (387 nmol cm−3 d−1) was recorded in near-surface sediments from Site U1548C, which had the steepest geothermal gradient (958°C km−1). At this site, SRR were generally over an order of magnitude higher than at similar depths at other sites (e.g., 387–157 nmol cm−3 d−1 at 1.9 mbsf from Site U1548C vs. 46–1.0 nmol cm−3 d−1 at 2.1 mbsf from Site U1552B). Site U1546D is characterized by a sill intrusion, but it had already reached thermal equilibrium and SRR were in the same range as nearby Site U1545C, which is minimally affected by sills. The wide temperature range observed at each drill site suggests major shifts in microbial community composition with very different temperature optima but awaits confirmation by molecular biological analyses. At the transition between the mesophilic and thermophilic range around 40°C–60°C, sulfate-reducing activity appears to be decreased, particularly in more oligotrophic settings, but shows a slight recovery at higher temperatures.

Published
2022

21. Microbial cell distribution in the Guaymas Basin subseafloor biosphere, a young marginal rift basin with rich organics and steep temperature gradient

Author

Morono, Yuki, Teske, Andreas, Galerne, Christophe, Bojanova, Diana, Edgcomb, Virginia, Meyer, Nicolette, Schubert, Florian, Toffin, Laurent, Lizarralde, Daniel, Höfig, Tobias W., Aiello, Ivano W., Ash, Janine L., Buatier, Martine, Gontharet, Swanne, Heuer, Verena B., Jiang, Shijun, Kars, Myriam A.C., Kim, Ji-Hoon, Koornneef, Louise M.T., Marsaglia, Kathleen M., Negrete-Aranda, Raquel, Neumann, Florian, Pastor, Lucie C., Peña-Salinas, Manet, Cruz, Ligia L. Pérez, Ran, Lihua, Riboulleau, Armelle, Sarao, John A., Singh, S. Khogenkumar, Stock, Joann M., Xie, Wei, Yamanaka, Toshiro, Zhuang, Guangchao, Woods Hole Oceanographic Institution (WHOI), Institute of Molecular Medicine and Cell Research (ZBMZ), University of Freiburg [Freiburg], Laboratoire de microbiologie des environnements extrêmophiles (LM2E), Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS), Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG), Institut national des sciences de l'Univers (INSU - CNRS)-Université du Littoral Côte d'Opale (ULCO)-Université de Lille-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Nord]), Geological Sciences, Florida State University [Tallahassee] (FSU), Kyung Hee University (KHU), and Key Laboratory of Marine Ecosystem Dynamics

Subjects
[SDE]Environmental Sciences
Abstract

Guaymas Basin is a young marginal rift basin in the Gulf of California characterized by active seafloor spreading and rapid sediment deposition, including organic-rich sediments derived from highly productive overlying waters and terrigenous sediments from nearby continental margins. The combination of active seafloor spreading and rapid sedimentation within a narrow basin results in a dynamic environment where linked physical, chemical, and biological processes regulate the cycling of sedimentary carbon and other elements. This continuum of interrelating processes from magma to microbe motivated International Ocean Discovery Program Expedition 385 and is reflected in its title, “Guaymas Basin Tectonics and Biosphere.”During IODP Expedition 385, organic-rich sediments with sill intrusions on the flanking regions and in the northern axial graben of Guaymas Basin (in eight sites) were drilled and core samples were recovered. Those cored samples were examined for their microbial cell abundance in a highly sensitive manner by density-gradient cell separation at the super clean room of Kochi Core Center, Japan, followed by direct counting on fluorescence microscopy. Cell abundance in surficial seafloor sediment (~109 cells/cm3) was roughly 1000 times higher than the bottom seawater (~106 cells/cm3) and gradually decreased with increasing depth and temperature. In contrast to the cell abundance profile observed at Nankai Trough (IODP Exp. 370), the gradual decrease of cell abundance was observed up to around 75ºC, and we detected microbial cells even at hot horizons above 100ºC.We will present the overview of the microbial cell distribution in the Guaymas Basin and discuss its relation to the current and past environmental conditions, e.g., temperature and sill-intrusion, etc.

Published
2022

22. Investigating microbial constraints on hydrocarbon processing in Guaymas Basin subseafloor sediments with sill intrusions

Author

Teske, Andreas, Mara, Paraskevi, Vázquez, Mirna, Baker, Brett, Morono, Yuki, Edgcomb, Virginia, Lizarralde, Daniel, Höfig, Tobias W., Aiello, Ivano W., Ash, Jeanine L., Bojanova, Diana P., Buatier, Martine, Galerne, Christophe Y., Gontharet, Swanne, Heuer, Verena B., Jiang, Shijun, Kars, Myriam A.C., Kim, Ji-Hoon, Koornneef, Louise M.T., Marsaglia, Kathleen M., Meyer, Nicolette R., Negrete-Aranda, Raquel, Neumann, Florian, Pastor, Lucie C., Peña-Salinas, Manet, Cruz, Ligia L. Pérez, Ran, Lihua, Riboulleau, Armelle, Sarao, John A., Schubert, Florian, Singh, S. Khogenkumar, Stock, Joann M., Toffin, Laurent M.A.A., Xie, Wei, Yamanaka, Toshiro, Zhuang, Guangchao, Department of Chemistry [Heraklion], University of Crete [Heraklion] (UOC), University of Texas at Austin [Austin], Woods Hole Oceanographic Institution (WHOI), Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG), Institut national des sciences de l'Univers (INSU - CNRS)-Université du Littoral Côte d'Opale (ULCO)-Université de Lille-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Nord]), Geological Sciences, Florida State University [Tallahassee] (FSU), Kyung Hee University (KHU), Key Laboratory of Marine Ecosystem Dynamics, Institute of Molecular Medicine and Cell Research (ZBMZ), and University of Freiburg [Freiburg]

Subjects
[SDE]Environmental Sciences
Abstract

Guaymas Basin is a young marginal rift basin in the Gulf of California characterized by active seafloor spreading and rapid deposition of organic-rich sediments derived from highly productive overlying waters and terrigenous sediments from nearby continental margins. Catalyzed by the steep geothermal gradient, sedimentary organic material of photosynthetic origin turns into a diverse spectrum of hydrocarbons that accumulate especially in deep, hot sediments, and might supply substrates for hydrocarbon-degrading microorganisms. The “from magma to microbe” perspective on these processes motivated International Ocean Discovery Program Expedition 385“Guaymas Basin Tectonics and Biosphere.”Hydrocarbon concentrations were determined in sediment samples selected from eight drilling sites on the flanking regions and in the northern axial graben of Guaymas Basin. Total petroleum hydrocarbon (C9-C44) concentrations increased from ca. 50-250 mg/kg towards >2000 mg/kg at in-situ temperatures above 80°C. A similar increase from ca. 10 mg/kg towards >100 mg/kg was observed for total saturated hydrocarbons. These gradients are shaped by abiotic hydrocarbon generation above 80°C at depth, and possibly by microbial hydrocarbon degradation at cooler temperatures in the upper sediment column. In a two-pronged approach, we are currently investigating the activity of bacterial/fungal consortia, isolated from Guaymas Basin surficial sediments, in the oxidation of selected alkanes and polyaromatics that occur at Guaymas Basin. In parallel, we explore the diversity, depth range and in-situ temperature range of bacteria, archaea and fungi in the Guaymas Basin subsurface sediments using PCR and metagenomic sequencing, to constrain microbial hydrocarbon cycling in the deep subsurface. Updates on these ongoing investigations will be presented.

Published
2022

24. Guaymas Basin Tectonics and Biosphere

Author

Teske, A., Lizarralde, D., Höfig, T.W., Aiello, Ivano W., Ash, Jeanine L., Bojanova, Diana P., Buatier, Martine D., Edgcomb, Virginia P., Galerne, Christophe Y., Gontharet, Swanne, Heuer, Verena B., Jiang, Shijun, Kars, Myriam A.C., Singh, S. Khogenkumar, Kim, Ji-Hoon, Koornneef, Louise M.T., Marsaglia, Kathleen M., Meyer, Nicolette R., Morono, Yuki, Negrete-Aranda, Raquel, Neumann, Florian, Pastor, Lucie C., Pena-Salinas, Manet E., Perez-Cruz, Ligia L., Ran, Lihua, Riboulleau, Armelle, Sarao, John A., Schubert, Florian, Stock, Joann M., Toffin, Laurent M.A.A., Xie, Wei, Yamanaka, Toshiro, Zhuang, Guangchao, Ortega, Rodrigo Perez, European Infective Endocarditis Registry (Euro-Endo), Woods Hole Oceanographic Institution (WHOI), International Ocean Discovery Program, Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Cycles biogéochimiques marins : processus et perturbations (CYBIOM), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Geological Sciences, Florida State University [Tallahassee] (FSU), Kyung Hee University (KHU), Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Key Laboratory of Marine Ecosystem Dynamics, Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG), Institut national des sciences de l'Univers (INSU - CNRS)-Université du Littoral Côte d'Opale (ULCO)-Université de Lille-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Nord]), Institute of Molecular Medicine and Cell Research (ZBMZ), University of Freiburg [Freiburg], Seismological Laboratory, California Institute of Technology (CALTECH), and Tokyo University of Marine Science and Technology (TUMSAT)

Subjects
Tectonics, Guaymas Basin, [SDE]Environmental Sciences, Geochemistry, Biosphere, Geology
Abstract

A complete set of the logging data collected during the expedition is available at http://mlp.ldeo.columbia.edu/logdb/scientific_ocean_drilling. If you have problems downloading the data, wish to receive additional logging data, or have questions regarding the data, please contact Database Administrator, Bore

Published
2021

25. Magma plumbing system and associated hydrothermal vents in the Guaymas Basin - geometry and implications

Author

Galerne, Christophe, Lizarralde, Daniel, Berndt, Christian, Neumann, Florian, Höfig, Tobias, Stock, Joann, Peña-Salinas, Manet, Negrete-Aranda, Raquel, Teske, Andreas, Aiello, Ivano W., Ash, Jeanine L., Bojanova, Diana P., Buatier, Martine D., Edgcomb, Virginia P., Gontharet, Swanne, Heuer, Verena B., Jiang, Shijun, Kars, Myriam A.C., Singh, S. Khogenkumar, Kim, Ji-Hoon, Koornneef, Louise M.T., Marsaglia, Kathleen M., Meyer, Nicolette R., Morono, Yuki, Pastor, Lucie C., Cruz, Ligia L. Perez, Ran, Lihua, Riboulleau, Armelle, Sarao, John, Schubert, Florian, Toffin, Laurent M.A.A., Xie, Wei, Yamanaka, Toshiro, Zhuang, Guangchao, Ortega, Rodrigo Perez, Woods Hole Oceanographic Institution (WHOI), Helmholtz Centre for Ocean Research [Kiel] (GEOMAR), International Ocean Discovery Program, Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), Cycles biogéochimiques marins : processus et perturbations (CYBIOM), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Geological Sciences, Florida State University [Tallahassee] (FSU), Kyung Hee University (KHU), Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Key Laboratory of Marine Ecosystem Dynamics, Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG), and Institut national des sciences de l'Univers (INSU - CNRS)-Université du Littoral Côte d'Opale (ULCO)-Université de Lille-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Nord])

Subjects
Guaymas Basin, Magma, [SDE]Environmental Sciences, Geochemistry, 14. Life underwater, Geology, Hydrothermal vent
Abstract

We document the geometry of a massive sill at the root of an approximately 20-m high and 800 m-wide ring of hydrothermal formations, termed Ringvent, located 28.5 km off-axis on the northwestern flanking regions of the actively rifting Guaymas Basin (Gulf of California). Using petrophysical data collected during the IODP Expedition 385 and processed 2D seismic profiles, we present evidence on the mechanics of sill emplacement and how the related hydrothermal vent conduits were constructed. The currently active moderate-temperature hydrothermal vent field indicates that, despite being cold and crystallized, the magma plumbing system, is tapping into a deeper geothermal source of the basin. The vent system roots at the vertical end of the magma plumbing system with the top of the sill located at a depth range of 80 to 150 m below the seafloor. Our research aims at constraining how far deep the geothermal fluids are coming from, and identifying how close the hydrothermal system is from a steady-state condition, to draw implications for how frequently such a system may arise in nascent ocean basins.

Published
2021

27. Microbial Communities Under Distinct Thermal and Geochemical Regimes in Axial and Off-Axis Sediments of Guaymas Basin

Author

Teske, Andreas, primary, Wegener, Gunter, additional, Chanton, Jeffrey P., additional, White, Dylan, additional, MacGregor, Barbara, additional, Hoer, Daniel, additional, de Beer, Dirk, additional, Zhuang, Guangchao, additional, Saxton, Matthew A., additional, Joye, Samantha B., additional, Lizarralde, Daniel, additional, Soule, S. Adam, additional, and Ruff, S. Emil, additional

Published
2021
Full Text
View/download PDF

28. Magnetic mineral diagenesis and associated biogeochemical processes in cold seepage and gas hydrate sites of the Guaymas Basin

Author

Kars, Myriam, primary, Pastor, Lucie, additional, Burin, Céline, additional, Morono, Yuki, additional, Koornneef, Louise, additional, Höfig, Tobias, additional, Teske, Andreas, additional, Lizarralde, Daniel, additional, Aiello, Ivano, additional, Ash, Jeanine, additional, Bojanova, Diana, additional, Buatier, Martine, additional, Edgcomb, Virginia, additional, Galerne, Christophe, additional, Gontharet, Swanne, additional, Heuer, Verena, additional, Jiang, Shijun, additional, Kim, Ji-Hoon, additional, Marsaglia, Kathie, additional, Meyer, Nicolette, additional, Neumann, Florian, additional, Negrete, Raquel, additional, Peña-Salinas, Manet, additional, Perez Cruz, Ligia, additional, Ran, Lihua, additional, Riboulleau, Armelle, additional, Sarao, John, additional, Schubert, Florian, additional, Singh, S. Khogenkumar, additional, Stock, Joann, additional, Toffin, Laurent, additional, Xie, Wei, additional, Xu, Shumei, additional, Yamanaka, Toshiro, additional, and Zhuang, Guangchao, additional

Published
2021
Full Text
View/download PDF

30. Methylotropher Methanogenese und potentielle methylierte Substrate in marinen Sedimenten

Author

Zhuang, Guangchao, Hinrichs, Kai-Uwe, and Teske, Andreas

Subjects
550 Earth sciences and geology, methylotrophic methanogenesis, ddc:550, marine sediment, Methane, methylated substrates
Abstract

Methane is the simplest hydrocarbon and a potent greenhouse gas that plays important roles in atmospheric chemistry, the global carbon cycle, and the formation of gas hydrates in marine sediment. Microbial production of methane is the terminal step during the degradation of organic matter. It is generally thought that methane is predominantly produced from hydrogenotrophic and acetoclastic methanogenesis, while methylotrophic methanogenesis and its relative importance for methane production in marine sediments remain largely unconstrained. The main objective of this study is to constrain potential methylated substrates and methylotrophic methanogenic activities, and further evaluate the importance of methylotrophic methanogenesis in marine sediment. As the lack of knowledge on in situ concentrations of methylated compounds impedes our understanding on their quantitative contribution to methane production, the first step was to determine the concentrations and carbon isotopic composition of methylated compounds using newly-developed methods. Quantitative or isotopic analysis of methanol, trimethylamine (TMA) and dimethylsulfide (DMS) in marine sediment and pore waters were achieved using gas chromatographic approaches in combination with a range of pretreatment techniques. Using these protocols, the concentrations and distributions of methylated compounds were determined in a variety of marine sediments from Aarhus Bay in Denmark, Orca Basin in the Gulf of Mexico and Gulf of Lions in the northwestern Mediterranean Sea. To further constrain the importance of methylotrophic methanogenesis, two case studies combining the newly-developed methods as well as various biogeochemical analyses were performed in hypersaline sediment and estuarine sediment. In hypersaline sediment of Orca Basin, multiple lines of evidences from abundances of methanogenic substrates, carbon isotope systematics between methane and substrates, thermodynamic calculations, stable isotope tracer and radiotracer experiments as well as gene and lipid biomarkers collectively confirmed that methylotrophic methanogenesis was the dominant methanogenic pathway in Orca Basin sediments. Furthermore, the distribution of methanogenic substrates, activity and diversity were characterized to quantitatively estimate the relative importance of different methanogenic pathways in estuarine sediment of the northwestern Mediterranean Sea. The results showed that both methylotrophic and hydrogenotrophic methanogenesis contributed to the formation of methane in the sulfate reduction zone, with methylotrophic methanogenesis accounting for 13%-74% of the total methane production. In the sulfate-depleted sediments, hydrogenotrophic methanogenesis dominated methanogenic pathway (67%-97%), whereas acetoclastic methanogenesis contributed up to 31% of methane production in organic-rich sediment. In contrast, the contribution of methylotrophic methanogenesis to the total methanogenic activity was negligible in the methanogenic zone (< 1%). Collectively, new constraints from methylated compounds and the metabolic activities improve our quantitative understanding on methylotrophic methanogenesis in different marine sediment settings. The findings in this thesis provide more comprehensive insights into the relative importance of methylotrophic methanogenesis in marine sediment.

Published
2014

Catalog

Books, media, physical & digital resources
See catalog results