Raw Data for article Ecosystem Function after the K/Pg Extinction: Decoupling of Marine Carbon Pump and Diversity ...

The ocean biological pump is the mechanism by which carbon and nutrients are transported to depth. As such, the biological pump is critical in the partitioning of carbon dioxide between the ocean and atmosphere, and the rate at which that carbon can be sequestered through burial in marine sediments....

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Main Authors: Birch, Heather, Schmidt, Daniela N, Coxall, Helen, Kroon, Dick, Ridgwell, Andy
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2021
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.935502
https://doi.pangaea.de/10.1594/PANGAEA.935502
id ftdatacite:10.1594/pangaea.935502
record_format openpolar
spelling ftdatacite:10.1594/pangaea.935502 2024-09-15T18:31:01+00:00 Raw Data for article Ecosystem Function after the K/Pg Extinction: Decoupling of Marine Carbon Pump and Diversity ... Birch, Heather Schmidt, Daniela N Coxall, Helen Kroon, Dick Ridgwell, Andy 2021 application/zip https://dx.doi.org/10.1594/pangaea.935502 https://doi.pangaea.de/10.1594/PANGAEA.935502 en eng PANGAEA https://dx.doi.org/10.1098/rspb.2021.0863 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Biological pump ecology ecosystem function K/Pg Planktonic foraminifera article Collection Bundled Publication of Datasets 2021 ftdatacite https://doi.org/10.1594/pangaea.93550210.1098/rspb.2021.0863 2024-08-01T10:54:23Z The ocean biological pump is the mechanism by which carbon and nutrients are transported to depth. As such, the biological pump is critical in the partitioning of carbon dioxide between the ocean and atmosphere, and the rate at which that carbon can be sequestered through burial in marine sediments. How the structure and function of planktic ecosystems in the ocean govern the strength and efficiency of the biological pump and its resilience to disruption are poorly understood. The aftermath of the impact at the Cretaceous/ Palaeogene (K/Pg) boundary provides an ideal opportunity to address these questions as both the biological pump and marine plankton size and diversity were fundamentally disrupted. The excellent fossil record of planktic foraminifera as indicators of pelagic-biotic recovery combined with carbon isotope records tracing biological pump behaviour, show that the recovery of ecological traits (diversity, size and photosymbiosis) occurred much later (approx. 4.3 m.y) than biological pump ... Article in Journal/Newspaper Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Biological pump
ecology
ecosystem function
K/Pg
Planktonic foraminifera
spellingShingle Biological pump
ecology
ecosystem function
K/Pg
Planktonic foraminifera
Birch, Heather
Schmidt, Daniela N
Coxall, Helen
Kroon, Dick
Ridgwell, Andy
Raw Data for article Ecosystem Function after the K/Pg Extinction: Decoupling of Marine Carbon Pump and Diversity ...
topic_facet Biological pump
ecology
ecosystem function
K/Pg
Planktonic foraminifera
description The ocean biological pump is the mechanism by which carbon and nutrients are transported to depth. As such, the biological pump is critical in the partitioning of carbon dioxide between the ocean and atmosphere, and the rate at which that carbon can be sequestered through burial in marine sediments. How the structure and function of planktic ecosystems in the ocean govern the strength and efficiency of the biological pump and its resilience to disruption are poorly understood. The aftermath of the impact at the Cretaceous/ Palaeogene (K/Pg) boundary provides an ideal opportunity to address these questions as both the biological pump and marine plankton size and diversity were fundamentally disrupted. The excellent fossil record of planktic foraminifera as indicators of pelagic-biotic recovery combined with carbon isotope records tracing biological pump behaviour, show that the recovery of ecological traits (diversity, size and photosymbiosis) occurred much later (approx. 4.3 m.y) than biological pump ...
format Article in Journal/Newspaper
author Birch, Heather
Schmidt, Daniela N
Coxall, Helen
Kroon, Dick
Ridgwell, Andy
author_facet Birch, Heather
Schmidt, Daniela N
Coxall, Helen
Kroon, Dick
Ridgwell, Andy
author_sort Birch, Heather
title Raw Data for article Ecosystem Function after the K/Pg Extinction: Decoupling of Marine Carbon Pump and Diversity ...
title_short Raw Data for article Ecosystem Function after the K/Pg Extinction: Decoupling of Marine Carbon Pump and Diversity ...
title_full Raw Data for article Ecosystem Function after the K/Pg Extinction: Decoupling of Marine Carbon Pump and Diversity ...
title_fullStr Raw Data for article Ecosystem Function after the K/Pg Extinction: Decoupling of Marine Carbon Pump and Diversity ...
title_full_unstemmed Raw Data for article Ecosystem Function after the K/Pg Extinction: Decoupling of Marine Carbon Pump and Diversity ...
title_sort raw data for article ecosystem function after the k/pg extinction: decoupling of marine carbon pump and diversity ...
publisher PANGAEA
publishDate 2021
url https://dx.doi.org/10.1594/pangaea.935502
https://doi.pangaea.de/10.1594/PANGAEA.935502
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://dx.doi.org/10.1098/rspb.2021.0863
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.93550210.1098/rspb.2021.0863
_version_ 1810472605948313600