Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis
The carbon stable isotope (δ13C) composition of the calcitic tests of planktonic foraminifera has an important role as a geochemical tracer of ocean carbon system changes associated with the Cretaceous/Paleogene (K/Pg) mass extinction event and its aftermath. Questions remain, however, about the ext...
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ftunivcardiff:oai:https://orca.cardiff.ac.uk:10123 2023-05-15T18:00:39+02:00 Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis Birch, Heather S. Coxall, Helen Kathrine Pearson, Paul Nicholas 2012-06 https://orca.cardiff.ac.uk/id/eprint/10123/ https://doi.org/10.1666/11027.1 unknown The Paleontological Society Birch, Heather S. https://orca.cardiff.ac.uk/view/cardiffauthors/A114661W.html, Coxall, Helen Kathrine https://orca.cardiff.ac.uk/view/cardiffauthors/A007483I.html and Pearson, Paul Nicholas https://orca.cardiff.ac.uk/view/cardiffauthors/A0179150.html orcid:0000-0003-4628-9818 orcid:0000-0003-4628-9818 2012. Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis. Paleobiology 38 (3) , pp. 374-390. 10.1666/11027.1 https://doi.org/10.1666/11027.1 doi:10.1666/11027.1 GC Oceanography QE Geology Article PeerReviewed 2012 ftunivcardiff https://doi.org/10.1666/11027.1 2022-10-20T22:34:13Z The carbon stable isotope (δ13C) composition of the calcitic tests of planktonic foraminifera has an important role as a geochemical tracer of ocean carbon system changes associated with the Cretaceous/Paleogene (K/Pg) mass extinction event and its aftermath. Questions remain, however, about the extent of δ13C isotopic disequilibrium effects and the impact of depth habitat evolution on test calcite δ13C among rapidly evolving Paleocene species, and the influence this has on reconstructed surface-to-deep ocean dissolved inorganic carbon (DIC) gradients. A synthesis of new and existing multispecies data, on the relationship between δ13C and δ18O and test size, sheds light on these issues. Results suggest that early Paleocene species quickly radiated into a range of depths habitats in a thermally stratified water column. Negative δ18O gradients with increasing test size in some species of Praemurica suggest either ontogenetic or ecotypic dependence on calcification temperature that may reflect depth/light controlled variability in symbiont photosynthetic activity. The pattern of positive δ13C test-size correlations allows us to (1) identify metabolic disequilibrium δ13C effects in small foraminifera tests, as occur in the immediate aftermath of the K/Pg event, (2) constrain the timing of evolution of foraminiferal photosymbiosis to 63.5 Ma, ∼0.9 Myr earlier than previously suggested, and (3) identify the apparent loss of symbiosis in a late-ranging morphotype of Praemurica. These findings have implications for interpreting δ13C DIC gradients at a resolution appropriate for incoming highly resolved K/Pg core records. Article in Journal/Newspaper Planktonic foraminifera Cardiff University: ORCA (Online Research @ Cardiff) Paleobiology 38 3 374 390 |
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Cardiff University: ORCA (Online Research @ Cardiff) |
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ftunivcardiff |
language |
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topic |
GC Oceanography QE Geology |
spellingShingle |
GC Oceanography QE Geology Birch, Heather S. Coxall, Helen Kathrine Pearson, Paul Nicholas Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis |
topic_facet |
GC Oceanography QE Geology |
description |
The carbon stable isotope (δ13C) composition of the calcitic tests of planktonic foraminifera has an important role as a geochemical tracer of ocean carbon system changes associated with the Cretaceous/Paleogene (K/Pg) mass extinction event and its aftermath. Questions remain, however, about the extent of δ13C isotopic disequilibrium effects and the impact of depth habitat evolution on test calcite δ13C among rapidly evolving Paleocene species, and the influence this has on reconstructed surface-to-deep ocean dissolved inorganic carbon (DIC) gradients. A synthesis of new and existing multispecies data, on the relationship between δ13C and δ18O and test size, sheds light on these issues. Results suggest that early Paleocene species quickly radiated into a range of depths habitats in a thermally stratified water column. Negative δ18O gradients with increasing test size in some species of Praemurica suggest either ontogenetic or ecotypic dependence on calcification temperature that may reflect depth/light controlled variability in symbiont photosynthetic activity. The pattern of positive δ13C test-size correlations allows us to (1) identify metabolic disequilibrium δ13C effects in small foraminifera tests, as occur in the immediate aftermath of the K/Pg event, (2) constrain the timing of evolution of foraminiferal photosymbiosis to 63.5 Ma, ∼0.9 Myr earlier than previously suggested, and (3) identify the apparent loss of symbiosis in a late-ranging morphotype of Praemurica. These findings have implications for interpreting δ13C DIC gradients at a resolution appropriate for incoming highly resolved K/Pg core records. |
format |
Article in Journal/Newspaper |
author |
Birch, Heather S. Coxall, Helen Kathrine Pearson, Paul Nicholas |
author_facet |
Birch, Heather S. Coxall, Helen Kathrine Pearson, Paul Nicholas |
author_sort |
Birch, Heather S. |
title |
Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis |
title_short |
Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis |
title_full |
Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis |
title_fullStr |
Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis |
title_full_unstemmed |
Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis |
title_sort |
evolutionary ecology of early paleocene planktonic foraminifera: size, depth habitat and symbiosis |
publisher |
The Paleontological Society |
publishDate |
2012 |
url |
https://orca.cardiff.ac.uk/id/eprint/10123/ https://doi.org/10.1666/11027.1 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
Birch, Heather S. https://orca.cardiff.ac.uk/view/cardiffauthors/A114661W.html, Coxall, Helen Kathrine https://orca.cardiff.ac.uk/view/cardiffauthors/A007483I.html and Pearson, Paul Nicholas https://orca.cardiff.ac.uk/view/cardiffauthors/A0179150.html orcid:0000-0003-4628-9818 orcid:0000-0003-4628-9818 2012. Evolutionary ecology of Early Paleocene planktonic foraminifera: Size, depth habitat and symbiosis. Paleobiology 38 (3) , pp. 374-390. 10.1666/11027.1 https://doi.org/10.1666/11027.1 doi:10.1666/11027.1 |
op_doi |
https://doi.org/10.1666/11027.1 |
container_title |
Paleobiology |
container_volume |
38 |
container_issue |
3 |
container_start_page |
374 |
op_container_end_page |
390 |
_version_ |
1766169835760254976 |