Evolutionary ecology of Early Paleocene planktonic foraminifera:Size, depth habitat and symbiosis
The carbon stable isotope ( 13 C) 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 ex...
Published in: | Paleobiology |
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Online Access: | https://hdl.handle.net/1983/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 https://research-information.bris.ac.uk/en/publications/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 https://doi.org/10.1666/11027.1 http://www.scopus.com/inward/record.url?scp=84868138646&partnerID=8YFLogxK |
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ftubristolcris:oai:research-information.bris.ac.uk:publications/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 2024-05-19T07:47:30+00:00 Evolutionary ecology of Early Paleocene planktonic foraminifera:Size, depth habitat and symbiosis Birch, Heather S. Coxall, Helen K. Pearson, Paul N. 2012-06-01 https://hdl.handle.net/1983/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 https://research-information.bris.ac.uk/en/publications/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 https://doi.org/10.1666/11027.1 http://www.scopus.com/inward/record.url?scp=84868138646&partnerID=8YFLogxK eng eng https://research-information.bris.ac.uk/en/publications/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 info:eu-repo/semantics/restrictedAccess Birch , H S , Coxall , H K & Pearson , P N 2012 , ' Evolutionary ecology of Early Paleocene planktonic foraminifera : Size, depth habitat and symbiosis ' , Paleobiology , vol. 38 , no. 3 , pp. 374-390 . https://doi.org/10.1666/11027.1 article 2012 ftubristolcris https://doi.org/10.1666/11027.1 2024-04-30T23:47:03Z The carbon stable isotope ( 13 C) 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 13 C isotopic disequilibrium effects and the impact of depth habitat evolution on test calcite 13 C 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 13 C and 18 O 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 18 O 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 13 C test-size correlations allows us to (1) identify metabolic disequilibrium 13 C 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 13 C DIC gradients at a resolution appropriate for incoming highly resolved K/Pg core records. Article in Journal/Newspaper Planktonic foraminifera University of Bristol: Bristol Research Paleobiology 38 3 374 390 |
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Open Polar |
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University of Bristol: Bristol Research |
op_collection_id |
ftubristolcris |
language |
English |
description |
The carbon stable isotope ( 13 C) 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 13 C isotopic disequilibrium effects and the impact of depth habitat evolution on test calcite 13 C 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 13 C and 18 O 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 18 O 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 13 C test-size correlations allows us to (1) identify metabolic disequilibrium 13 C 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 13 C 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 K. Pearson, Paul N. |
spellingShingle |
Birch, Heather S. Coxall, Helen K. Pearson, Paul N. Evolutionary ecology of Early Paleocene planktonic foraminifera:Size, depth habitat and symbiosis |
author_facet |
Birch, Heather S. Coxall, Helen K. Pearson, Paul N. |
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 |
publishDate |
2012 |
url |
https://hdl.handle.net/1983/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 https://research-information.bris.ac.uk/en/publications/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 https://doi.org/10.1666/11027.1 http://www.scopus.com/inward/record.url?scp=84868138646&partnerID=8YFLogxK |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Birch , H S , Coxall , H K & Pearson , P N 2012 , ' Evolutionary ecology of Early Paleocene planktonic foraminifera : Size, depth habitat and symbiosis ' , Paleobiology , vol. 38 , no. 3 , pp. 374-390 . https://doi.org/10.1666/11027.1 |
op_relation |
https://research-information.bris.ac.uk/en/publications/50cd1209-e4c5-413e-8932-aceb1c0c3eb5 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
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 |
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1799487927927963648 |