Morphometry of calcareous nannofossils from the Oceanic Anoxic Event 1a ...

Ocean acidification induced by atmospheric CO2 may be a major threat to marine ecosystems, particularly to calcareous nannoplankton. We show that, during the Aptian (~120 million years ago) Oceanic Anoxic Event 1a, which resulted from a massive addition of volcanic CO2, the morphological features of...

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Main Authors: Erba, Elisabetta, Bottini, Cinzia, Weissert, Helmut J, Keller, Christina E
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.771682
https://doi.pangaea.de/10.1594/PANGAEA.771682
id ftdatacite:10.1594/pangaea.771682
record_format openpolar
spelling ftdatacite:10.1594/pangaea.771682 2024-09-15T18:28:08+00:00 Morphometry of calcareous nannofossils from the Oceanic Anoxic Event 1a ... Erba, Elisabetta Bottini, Cinzia Weissert, Helmut J Keller, Christina E 2010 application/zip https://dx.doi.org/10.1594/pangaea.771682 https://doi.pangaea.de/10.1594/PANGAEA.771682 en eng PANGAEA https://dx.doi.org/10.1126/science.1188886 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg62 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 2010 ftdatacite https://doi.org/10.1594/pangaea.77168210.1126/science.1188886 2024-08-01T10:50:55Z Ocean acidification induced by atmospheric CO2 may be a major threat to marine ecosystems, particularly to calcareous nannoplankton. We show that, during the Aptian (~120 million years ago) Oceanic Anoxic Event 1a, which resulted from a massive addition of volcanic CO2, the morphological features of calcareous nannofossils traced the biological response to acidified surface waters. We observe the demise of heavily calcified nannoconids and reduced calcite paleofluxes at the beginning of a pre-anoxia calcification crisis. Ephemeral coccolith dwarfism and malformation represent species-specific adjustments to survive lower pH, whereas later, abundance peaks indicate intermittent alkalinity recovery. Deepwater acidification occurred with a delay of 25,000 to 30,000 years. After the dissolution climax, nannoplankton and carbonate recovery developed over ~160,000 years under persisting global dysoxia-anoxia. ... : Supplement to: Erba, Elisabetta; Bottini, Cinzia; Weissert, Helmut J; Keller, Christina E (2010): Calcareous nannoplankton response to surface-water acidification around Oceanic Anoxic Event 1a. Science, 329(5990), 428-432 ... Article in Journal/Newspaper Ocean acidification DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg62
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Drilling/drill rig
Leg62
Glomar Challenger
Deep Sea Drilling Project DSDP
Erba, Elisabetta
Bottini, Cinzia
Weissert, Helmut J
Keller, Christina E
Morphometry of calcareous nannofossils from the Oceanic Anoxic Event 1a ...
topic_facet Drilling/drill rig
Leg62
Glomar Challenger
Deep Sea Drilling Project DSDP
description Ocean acidification induced by atmospheric CO2 may be a major threat to marine ecosystems, particularly to calcareous nannoplankton. We show that, during the Aptian (~120 million years ago) Oceanic Anoxic Event 1a, which resulted from a massive addition of volcanic CO2, the morphological features of calcareous nannofossils traced the biological response to acidified surface waters. We observe the demise of heavily calcified nannoconids and reduced calcite paleofluxes at the beginning of a pre-anoxia calcification crisis. Ephemeral coccolith dwarfism and malformation represent species-specific adjustments to survive lower pH, whereas later, abundance peaks indicate intermittent alkalinity recovery. Deepwater acidification occurred with a delay of 25,000 to 30,000 years. After the dissolution climax, nannoplankton and carbonate recovery developed over ~160,000 years under persisting global dysoxia-anoxia. ... : Supplement to: Erba, Elisabetta; Bottini, Cinzia; Weissert, Helmut J; Keller, Christina E (2010): Calcareous nannoplankton response to surface-water acidification around Oceanic Anoxic Event 1a. Science, 329(5990), 428-432 ...
format Article in Journal/Newspaper
author Erba, Elisabetta
Bottini, Cinzia
Weissert, Helmut J
Keller, Christina E
author_facet Erba, Elisabetta
Bottini, Cinzia
Weissert, Helmut J
Keller, Christina E
author_sort Erba, Elisabetta
title Morphometry of calcareous nannofossils from the Oceanic Anoxic Event 1a ...
title_short Morphometry of calcareous nannofossils from the Oceanic Anoxic Event 1a ...
title_full Morphometry of calcareous nannofossils from the Oceanic Anoxic Event 1a ...
title_fullStr Morphometry of calcareous nannofossils from the Oceanic Anoxic Event 1a ...
title_full_unstemmed Morphometry of calcareous nannofossils from the Oceanic Anoxic Event 1a ...
title_sort morphometry of calcareous nannofossils from the oceanic anoxic event 1a ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.771682
https://doi.pangaea.de/10.1594/PANGAEA.771682
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://dx.doi.org/10.1126/science.1188886
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.77168210.1126/science.1188886
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