8 results on '"Cromartie, Amy"'
Search Results
2. Temperature, Precipitation, Vegetation, and Human Controls on brGDGTs in soils from a semi-arid altitudinal transect from the Republic of Armenia
- Author
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Cromartie, Amy, Ménot, Guillemette, Robles, Mary, Dugerdil, Lucas, Ansanay-Alex, Salomé, Peyron, Odile, Joannin, Sébastien, Cornell University [New York], Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Institut de recherche pour le développement [IRD] : UR226-Centre National de la Recherche Scientifique (CNRS)-Université de Montpellier (UM), Università degli Studi del Molise = University of Molise (UNIMOL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement [IRD] : UR226-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), and Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC)
- Subjects
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment - Published
- 2022
3. Holocene Fires and Mountain Communities in the Grasslands of Armenia
- Author
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Cromartie, Amy, Barhoumi, Cheima, Ménot, Guillemette, Messager, Erwan, Peyron, Odile, David, Etienne, Sabatier, Pierre, Joannin, Sébastien, Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement [IRD] : UR226-Centre National de la Recherche Scientifique (CNRS), Cornell University [New York], Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), and Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])
- Subjects
[SDE.MCG]Environmental Sciences/Global Changes ,[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment - Abstract
International audience
- Published
- 2022
4. Climate changes during the Late Glacial in southern Europe: new insights based on pollen and brGDGTs of Lake Matese in Italy.
- Author
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Robles, Mary, Peyron, Odile, Ménot, Guillemette, Brugiapaglia, Elisabetta, Wulf, Sabine, Appelt, Oona, Blache, Marion, Vannière, Boris, Dugerdil, Lucas, Paura, Bruno, Ansanay-Alex, Salomé, Cromartie, Amy, Charlet, Laurent, Guédron, Stephane, de Beaulieu, Jacques-Louis, and Joannin, Sébastien
- Subjects
YOUNGER Dryas ,POLLEN ,ANTARCTIC ice ,JET streams ,SEA ice - Abstract
The Late Glacial (14 700–11 700 cal BP) is a key climate period marked by rapid but contrasted changes in the Northern Hemisphere. Indeed, regional climate differences have been evidenced during the Late Glacial in Europe and the northern Mediterranean. However, past climate patterns are still debated since temperature and precipitation changes are poorly investigated towards the lower European latitudes. Lake Matese in southern Italy is a key site in the central Mediterranean to investigate climate patterns during the Late Glacial. This study aims to reconstruct climate changes and their impacts at Matese using a multi-proxy approach including magnetic susceptibility, geochemistry (XRF core scanning), pollen data and molecular biomarkers like branched glycerol dialkyl glycerol tetraethers (brGDGTs). Paleotemperatures and paleo-precipitation patterns are quantitatively inferred from pollen assemblages (multi-method approach: modern analogue technique, weighted averaging partial least-squares regression, random forest and boosted regression trees) and brGDGT calibrations. The results are compared to a latitudinal selection of regional climate reconstructions in Italy to better understand climate processes in Europe and in the circum-Mediterranean region. A warm Bølling–Allerød and a marked cold Younger Dryas are revealed in all climate reconstructions inferred from various proxies (chironomids, ostracods, speleothems, pollen, brGDGTs), showing no latitudinal differences in terms of temperatures across Italy. During the Bølling–Allerød, no significant changes in terms of precipitation are recorded; however, a contrasted pattern is visible during the Younger Dryas. Slightly wetter conditions are recorded south of 42 ∘ N, whereas dry conditions are recorded north of 42 ∘ N. During the Younger Dryas, cold conditions can be attributed to the southward position of North Atlantic sea ice and of the polar frontal jet stream, whereas the increase in precipitation in southern Italy seems to be linked to relocation of Atlantic storm tracks into the Mediterranean, induced by the Fennoscandian ice sheet and the North European Plain. By contrast, warm conditions during the Bølling–Allerød can be linked to the northward position of North Atlantic sea ice and of the polar frontal jet stream. [ABSTRACT FROM AUTHOR]
- Published
- 2023
- Full Text
- View/download PDF
5. Climate changes during the Lateglacial in South Europe: new insights based on pollen and brGDGTs of Lake Matese in Italy.
- Author
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Robles, Mary, Peyron, Odile, Ménot, Guillemette, Brugiapaglia, Elisabetta, Wulf, Sabine, Appelt, Oona, Blache, Marion, Vannière, Boris, Dugerdil, Lucas, Paura, Bruno, Ansanay-Alex, Salomé, Cromartie, Amy, Charlet, Laurent, Guédron, Stephane, de Beaulieu, Jacques-Louis, and Joannin, Sébastien
- Abstract
The Lateglacial (14,700–11,700 cal BP) is a key climate period marked by rapid but contrasted changes in the Northern Hemisphere. Indeed, regional climate differences have been evidenced during the Lateglacial in Europe and the Northern Mediterranean areas. However, past climate patterns are still debated since temperature and precipitation changes are poorly investigated towards the lower European latitudes. Lake Matese in Southern Italy is a key site in the Central Mediterranean to investigate climate patterns during the Lateglacial. This study uses a multi-proxy approach including magnetic susceptibility, geochemistry (XRF core scanning), pollen data and molecular biomarkers like branched Glycerol Dialkyl Glycerol Tetraethers (brGDGTs) to reconstruct climate changes and their impacts at Matese. Palaeotemperatures and -precipitation patterns are quantitatively inferred from pollen assemblages (multi-method approach: Modern Analogue Technique, Weighted Averaging Partial Least Squares regression, Random Forest, and Boosted Regression Trees) and brGDGTs calibrations. The results are compared to a latitudinal selection of regional climate reconstructions in Italy to better understand climate processes in Europe and in the circum-Mediterranean region. A warm Bølling–Allerød and a marked cold Younger Dryas are revealed in all climate reconstructions inferred from various proxies (chironomids, ostracods, speleothems, pollen, brGDGTs), showing no latitudinal differences in terms of temperatures across Italy. During the Bølling–Allerød, no significant changes in terms of precipitation are recorded, however, a contrasted pattern is visible during the Younger Dryas. Slightly wet conditions are recorded south of latitude 42° N whereas dry conditions are recorded north of latitude 42° N. During the Younger Dryas, cold conditions can be attributed to the southward position of North Atlantic sea-ice and of the Polar Frontal JetStream whereas the increase of precipitation is Southern Italy seems to be linked to relocation of Atlantic storm tracks into the Mediterranean, induced by the Fennoscandian ice sheet and the North European Plain. On the contrary, during the Bølling–Allerød warm conditions can be linked to the northward position of North Atlantic sea-ice and of the Polar Frontal JetStream. [ABSTRACT FROM AUTHOR]
- Published
- 2022
- Full Text
- View/download PDF
6. A Holocene glycerol dialkyl glycerol tetraether (GDGT) MAAT reconstruction from the country of Armenia
- Author
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Cromartie, Amy, Peyron, Odile, Joannin, Sébastien, Mary, Robles, Dugerdil, Lucas, Blanchet, Claire, Messager, Erwan, Etienne, David, MENOT, Guillemette, Cornell University [New York], Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement [IRD] : UR226-Centre National de la Recherche Scientifique (CNRS), University of Molise [Campobasso] (UNIMOL), University of Molise, Laboratoire de Physique de l'ENS Lyon (Phys-ENS), École normale supérieure - Lyon (ENS Lyon)-Centre National de la Recherche Scientifique (CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon, Environnements, Dynamiques et Territoires de la Montagne (EDYTEM), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS), Centre Alpin de Recherche sur les Réseaux Trophiques et Ecosystèmes Limniques (CARRTEL), Institut National de la Recherche Agronomique (INRA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE), Università degli Studi del Molise = University of Molise (UNIMOL), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Centre National de la Recherche Scientifique (CNRS), Environnements, Dynamiques et Territoires de Montagne (EDYTEM), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), and Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS)
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[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment ,ComputingMilieux_MISCELLANEOUS - Abstract
International audience
- Published
- 2019
7. Iranian Long Spouted Vessels of the Third and Second Millennium BCE: Contextualizing an Enigmatic Vessel
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Cromartie, Amy
- Subjects
Long-beaked ,Central Asia ,Archaeology ,Third Millennium BCE ,Second Millennium BCE ,Iran ,Social and Behavioral Sciences ,Spouted - Abstract
Long spouted vessels have a long tradition on the Iranian Plateau that spans the millennia. Well known from the Iron Age in northern Iran their context outside of this regional time frame, to date, has been understudied. This paper is part of a multi-stage research project, which aims to understand their evolution and possible ritual function both inside and outside of Iran. In this paper I present the initial data collection and findings of this research. Using previously published excavation reports, I trace these vessel’s location, material composition, and grave context. From these data I find that the long-spouted morphology has been present on the Iranian plateau since the 4th millennium BCE, and were present in Iran, Mesopotamia, and Central Asia during the 3rd and 2nd millennium BCE. I also examine their possible ritual function by looking at their representation in figural art. These data will be used in further research where I will investigate if these vessels represent a continuation of shared ritual between these regional centers.
- Published
- 2014
8. The Project ArAGATS Kasakh Valley Archaeological Survey, Armenia: Report of the 2014-2017 Seasons.
- Author
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LINDSAY, IAN, GREENE, ALAN F., MARSHALL, MAUREEN E., BADALYAN, RUBEN, CROMARTIE, AMY, AZATYAN, KAREN, AGHIKYAN, LEVON, KHATCHADOURIAN, LORI, MKRTCHYAN, ARSHALUYS, and SMITH, ADAM T.
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ARCHAEOLOGICAL surveying , *POLITICAL systems , *CHRONOLOGY , *CEMETERIES , *FORTIFICATION - Abstract
During four field seasons spanning 2014 through 2017, Project ArAGATS (Archaeology and Geography of Ancient Transcaucasian Societies) expanded our long-term research on the origins and development of complex political systems in the South Caucasus with a comprehensive study of the upper Kasakh River valley in north-central Armenia. The Kasakh Valley Archaeological Survey employed both systematic transect survey of 43 km2 and extensive satellite- and drone-based reconnaissance to accommodate the complex topography of the Lesser Caucasus and the impacts of Soviet-era land amelioration. Though our survey was animated by questions related to the chronology and distribution of Bronze and Iron Age fortifications and cemeteries, we also recorded Paleolithic sites stretching back to the earliest human settlement of the Caucasus, Early Bronze Age surface finds, and historic landscape modifications. Concurrent to the survey, members of the ArAGATS team carried out test excavations at select settlement sites and associated burials, and a series of wetland core extractions, with the goals of affirming site occupation sequences and setting them within their environmental context. This report provides an overview of the results of these multidisciplinary activities. [ABSTRACT FROM AUTHOR]
- Published
- 2022
- Full Text
- View/download PDF
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