Mapping of recent brachiopod microstructure: A tool for environmental studies

Shells of brachiopods are excellent archives for environmental reconstructions in the recent and distant past as their microstructure and geochemistry respond to climate and environmental forcings. We studied the morphology and size of the basic structural unit, the secondary layer fibre, of the she...

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Published in:Journal of Structural Biology
Main Authors: Ye, Facheng, Crippa, Gaia, Angiolini, Lucia, Brand, Uwe, Capitani, GianCarlo, Cusack, Maggie, Garbelli, Claudio, Griesshaber, Erika, Harper, Elizabeth, Schmahl, Wolfgang
Format: Report
Language:English
Published: ACADEMIC PRESS INC ELSEVIER SCIENCE 2018
Subjects:
Online Access:http://ir.nigpas.ac.cn/handle/332004/17866
https://doi.org/10.1016/j.jsb.2017.11.011
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spelling ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/17866 2023-05-15T14:04:23+02:00 Mapping of recent brachiopod microstructure: A tool for environmental studies Ye, Facheng Crippa, Gaia Angiolini, Lucia Brand, Uwe Capitani, GianCarlo Cusack, Maggie Garbelli, Claudio Griesshaber, Erika Harper, Elizabeth Schmahl, Wolfgang 2018-03-01 http://ir.nigpas.ac.cn/handle/332004/17866 https://doi.org/10.1016/j.jsb.2017.11.011 英语 eng ACADEMIC PRESS INC ELSEVIER SCIENCE JOURNAL OF STRUCTURAL BIOLOGY http://ir.nigpas.ac.cn/handle/332004/17866 doi:10.1016/j.jsb.2017.11.011 Biominerals Micromorphometry Ontogenetic variation Geochemical and environmental proxies TEREBRATALIA-TRANSVERSA HIERARCHICAL ARCHITECTURE OCEAN ACIDIFICATION ISOTOPE COMPOSITION FOSSIL BRACHIOPODS SHELL BIOMATERIALS CLIMATE-CHANGE GLOBAL CHANGE CALCITE OXYGEN Biochemistry & Molecular Biology Biophysics Cell Biology 期刊论文 2018 ftchinacscnigpas https://doi.org/10.1016/j.jsb.2017.11.011 2019-08-14T12:43:51Z Shells of brachiopods are excellent archives for environmental reconstructions in the recent and distant past as their microstructure and geochemistry respond to climate and environmental forcings. We studied the morphology and size of the basic structural unit, the secondary layer fibre, of the shells of several extant brachiopod taxa to derive a model correlating microstructural patterns to environmental conditions. Twenty-one adult specimens of six recent brachiopod species adapted to different environmental conditions, from Antarctica, to New Zealand, to the Mediterranean Sea, were chosen for microstructural analysis using SEM, TEM and EBSD. We conclude that: 1) there is no significant difference in the shape and size of the fibres between ventral and dorsal valves, 2) there is an ontogenetic trend in the shape and size of the fibres, as they become larger, wider, and flatter with increasing age. This indicates that the fibrous layer produced in the later stages of growth, which is recommended by the literature to be the best material for geochemical analyses, has a different morphostructure and probably a lower organic content than that produced earlier in life. In two species of the same genus living in seawater with different temperature and carbonate saturation state, a relationship emerged between the microstructure and environmental conditions. Fibres of the polar Liothyrella uva tend to be smaller, rounder and less convex than those of the temperate Liothyrella neozelanica, suggesting a relationship between microstructural size, shell organic matter content, ambient seawater temperature and calcite saturation state. Report Antarc* Antarctica Ocean acidification Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) New Zealand Journal of Structural Biology 201 3 221 236
institution Open Polar
collection Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences)
op_collection_id ftchinacscnigpas
language English
topic Biominerals
Micromorphometry
Ontogenetic variation
Geochemical and environmental proxies
TEREBRATALIA-TRANSVERSA
HIERARCHICAL ARCHITECTURE
OCEAN ACIDIFICATION
ISOTOPE COMPOSITION
FOSSIL BRACHIOPODS
SHELL BIOMATERIALS
CLIMATE-CHANGE
GLOBAL CHANGE
CALCITE
OXYGEN
Biochemistry & Molecular Biology
Biophysics
Cell Biology
spellingShingle Biominerals
Micromorphometry
Ontogenetic variation
Geochemical and environmental proxies
TEREBRATALIA-TRANSVERSA
HIERARCHICAL ARCHITECTURE
OCEAN ACIDIFICATION
ISOTOPE COMPOSITION
FOSSIL BRACHIOPODS
SHELL BIOMATERIALS
CLIMATE-CHANGE
GLOBAL CHANGE
CALCITE
OXYGEN
Biochemistry & Molecular Biology
Biophysics
Cell Biology
Ye, Facheng
Crippa, Gaia
Angiolini, Lucia
Brand, Uwe
Capitani, GianCarlo
Cusack, Maggie
Garbelli, Claudio
Griesshaber, Erika
Harper, Elizabeth
Schmahl, Wolfgang
Mapping of recent brachiopod microstructure: A tool for environmental studies
topic_facet Biominerals
Micromorphometry
Ontogenetic variation
Geochemical and environmental proxies
TEREBRATALIA-TRANSVERSA
HIERARCHICAL ARCHITECTURE
OCEAN ACIDIFICATION
ISOTOPE COMPOSITION
FOSSIL BRACHIOPODS
SHELL BIOMATERIALS
CLIMATE-CHANGE
GLOBAL CHANGE
CALCITE
OXYGEN
Biochemistry & Molecular Biology
Biophysics
Cell Biology
description Shells of brachiopods are excellent archives for environmental reconstructions in the recent and distant past as their microstructure and geochemistry respond to climate and environmental forcings. We studied the morphology and size of the basic structural unit, the secondary layer fibre, of the shells of several extant brachiopod taxa to derive a model correlating microstructural patterns to environmental conditions. Twenty-one adult specimens of six recent brachiopod species adapted to different environmental conditions, from Antarctica, to New Zealand, to the Mediterranean Sea, were chosen for microstructural analysis using SEM, TEM and EBSD. We conclude that: 1) there is no significant difference in the shape and size of the fibres between ventral and dorsal valves, 2) there is an ontogenetic trend in the shape and size of the fibres, as they become larger, wider, and flatter with increasing age. This indicates that the fibrous layer produced in the later stages of growth, which is recommended by the literature to be the best material for geochemical analyses, has a different morphostructure and probably a lower organic content than that produced earlier in life. In two species of the same genus living in seawater with different temperature and carbonate saturation state, a relationship emerged between the microstructure and environmental conditions. Fibres of the polar Liothyrella uva tend to be smaller, rounder and less convex than those of the temperate Liothyrella neozelanica, suggesting a relationship between microstructural size, shell organic matter content, ambient seawater temperature and calcite saturation state.
format Report
author Ye, Facheng
Crippa, Gaia
Angiolini, Lucia
Brand, Uwe
Capitani, GianCarlo
Cusack, Maggie
Garbelli, Claudio
Griesshaber, Erika
Harper, Elizabeth
Schmahl, Wolfgang
author_facet Ye, Facheng
Crippa, Gaia
Angiolini, Lucia
Brand, Uwe
Capitani, GianCarlo
Cusack, Maggie
Garbelli, Claudio
Griesshaber, Erika
Harper, Elizabeth
Schmahl, Wolfgang
author_sort Ye, Facheng
title Mapping of recent brachiopod microstructure: A tool for environmental studies
title_short Mapping of recent brachiopod microstructure: A tool for environmental studies
title_full Mapping of recent brachiopod microstructure: A tool for environmental studies
title_fullStr Mapping of recent brachiopod microstructure: A tool for environmental studies
title_full_unstemmed Mapping of recent brachiopod microstructure: A tool for environmental studies
title_sort mapping of recent brachiopod microstructure: a tool for environmental studies
publisher ACADEMIC PRESS INC ELSEVIER SCIENCE
publishDate 2018
url http://ir.nigpas.ac.cn/handle/332004/17866
https://doi.org/10.1016/j.jsb.2017.11.011
geographic New Zealand
geographic_facet New Zealand
genre Antarc*
Antarctica
Ocean acidification
genre_facet Antarc*
Antarctica
Ocean acidification
op_relation JOURNAL OF STRUCTURAL BIOLOGY
http://ir.nigpas.ac.cn/handle/332004/17866
doi:10.1016/j.jsb.2017.11.011
op_doi https://doi.org/10.1016/j.jsb.2017.11.011
container_title Journal of Structural Biology
container_volume 201
container_issue 3
container_start_page 221
op_container_end_page 236
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