Confocal Raman microscopy and its contribution to sclerochronology

Rising global temperatures, ocean acidification and rising sea levels: just three of many changes mankind will have to deal with in the future. A precise understanding of past warm phases is essential for successfully anticipating forthcoming change and mitigating its consequences. Understanding the...

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Main Authors: Beierlein, Lars, Nehrke, Gernot, Brey, Thomas
Format: Conference Object
Language:unknown
Published: 2012
Subjects:
Online Access:https://epic.awi.de/id/eprint/33208/
https://hdl.handle.net/10013/epic.41706
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spelling ftawi:oai:epic.awi.de:33208 2024-09-15T17:54:29+00:00 Confocal Raman microscopy and its contribution to sclerochronology Beierlein, Lars Nehrke, Gernot Brey, Thomas 2012-09-26 https://epic.awi.de/id/eprint/33208/ https://hdl.handle.net/10013/epic.41706 unknown Beierlein, L. , Nehrke, G. orcid:0000-0002-2851-3049 and Brey, T. orcid:0000-0002-6345-2851 (2012) Confocal Raman microscopy and its contribution to sclerochronology , Jubiläumstagung der Paläontologischen Gesellschaft, Berlin, Germany, 24 September 2012 - 29 September 2012 . hdl:10013/epic.41706 EPIC3Jubiläumstagung der Paläontologischen Gesellschaft, Berlin, Germany, 2012-09-24-2012-09-29 Conference notRev 2012 ftawi 2024-06-24T04:07:26Z Rising global temperatures, ocean acidification and rising sea levels: just three of many changes mankind will have to deal with in the future. A precise understanding of past warm phases is essential for successfully anticipating forthcoming change and mitigating its consequences. Understanding the connections of the complex global climate system during warm phases, when climate conditions were similar to what we can expect for the future, is a major task for palaeo-climate reconstructions. Since instrumental data are restricted to the last two centuries, past climates can only be revealed by proxy data. Fossil biogenic carbonates (e.g., molluscs, foraminifera) are key-sources of information for palaeo-climatic and palaeo-environmental reconstructions, as anatomical and/or geochemical properties of the carbonate can serve as proxies for certain environmental parameters. Confocal Raman microscopy (CRM) can play a central role in analysis and quality control of biogenic carbonate studies. CRM can identify mineral (and organic) phase(s) in marine biogenic carbonates at high spatial resolution (300 nm), i.e. it allows to identify taphonomic changes in the carbonate structure. Furthermore, this method is ideal to detect possible contaminations, e.g., resulting from shell preparation in the laboratory (e.g., by epoxy resin or super glue). CRM is also a valuable tool to identify and visualize growth increments within accretionally precipitated carbonate skeletons of marine organisms. Commonly used dyeing techniques (like e.g., Mutvei´s solution) are often inefficient when applied to fossil biogenic carbonates with low organic content. CRF can reveal shell formation processes at a very high spatial resolution, even in several million years old shell material Here, we demonstrate the potential of CRM supported analysis, using shells of the marine bivalve Arctica islandica. Its wide northern-boreal distribution, its relative abundance in the fossil record (present in the North Atlantic since at least 20 million years), ... Conference Object Arctica islandica North Atlantic Ocean acidification Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Rising global temperatures, ocean acidification and rising sea levels: just three of many changes mankind will have to deal with in the future. A precise understanding of past warm phases is essential for successfully anticipating forthcoming change and mitigating its consequences. Understanding the connections of the complex global climate system during warm phases, when climate conditions were similar to what we can expect for the future, is a major task for palaeo-climate reconstructions. Since instrumental data are restricted to the last two centuries, past climates can only be revealed by proxy data. Fossil biogenic carbonates (e.g., molluscs, foraminifera) are key-sources of information for palaeo-climatic and palaeo-environmental reconstructions, as anatomical and/or geochemical properties of the carbonate can serve as proxies for certain environmental parameters. Confocal Raman microscopy (CRM) can play a central role in analysis and quality control of biogenic carbonate studies. CRM can identify mineral (and organic) phase(s) in marine biogenic carbonates at high spatial resolution (300 nm), i.e. it allows to identify taphonomic changes in the carbonate structure. Furthermore, this method is ideal to detect possible contaminations, e.g., resulting from shell preparation in the laboratory (e.g., by epoxy resin or super glue). CRM is also a valuable tool to identify and visualize growth increments within accretionally precipitated carbonate skeletons of marine organisms. Commonly used dyeing techniques (like e.g., Mutvei´s solution) are often inefficient when applied to fossil biogenic carbonates with low organic content. CRF can reveal shell formation processes at a very high spatial resolution, even in several million years old shell material Here, we demonstrate the potential of CRM supported analysis, using shells of the marine bivalve Arctica islandica. Its wide northern-boreal distribution, its relative abundance in the fossil record (present in the North Atlantic since at least 20 million years), ...
format Conference Object
author Beierlein, Lars
Nehrke, Gernot
Brey, Thomas
spellingShingle Beierlein, Lars
Nehrke, Gernot
Brey, Thomas
Confocal Raman microscopy and its contribution to sclerochronology
author_facet Beierlein, Lars
Nehrke, Gernot
Brey, Thomas
author_sort Beierlein, Lars
title Confocal Raman microscopy and its contribution to sclerochronology
title_short Confocal Raman microscopy and its contribution to sclerochronology
title_full Confocal Raman microscopy and its contribution to sclerochronology
title_fullStr Confocal Raman microscopy and its contribution to sclerochronology
title_full_unstemmed Confocal Raman microscopy and its contribution to sclerochronology
title_sort confocal raman microscopy and its contribution to sclerochronology
publishDate 2012
url https://epic.awi.de/id/eprint/33208/
https://hdl.handle.net/10013/epic.41706
genre Arctica islandica
North Atlantic
Ocean acidification
genre_facet Arctica islandica
North Atlantic
Ocean acidification
op_source EPIC3Jubiläumstagung der Paläontologischen Gesellschaft, Berlin, Germany, 2012-09-24-2012-09-29
op_relation Beierlein, L. , Nehrke, G. orcid:0000-0002-2851-3049 and Brey, T. orcid:0000-0002-6345-2851 (2012) Confocal Raman microscopy and its contribution to sclerochronology , Jubiläumstagung der Paläontologischen Gesellschaft, Berlin, Germany, 24 September 2012 - 29 September 2012 . hdl:10013/epic.41706
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