Sedimentary microplankton distributions are shaped by oceanographically connected areas

<p>Having descended through the water column, microplankton in ocean sediments is representative of the ocean surface environment, where it originated. Sedimentary microplankton is therefore used as an archive of past and present surface oceanographic conditions. However, these particles are a...

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Main Authors: P. D. Nooteboom, P. K. Bijl, C. Kehl, E. van Sebille, M. Ziegler, A. S. von der Heydt, H. A. Dijkstra
Format: Article
Language:English
Published: Copernicus Publications 2022-02-01
Series:Earth System Dynamics
Online Access:https://esd.copernicus.org/articles/13/357/2022/esd-13-357-2022.pdf
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author P. D. Nooteboom
P. D. Nooteboom
P. K. Bijl
C. Kehl
E. van Sebille
E. van Sebille
M. Ziegler
A. S. von der Heydt
A. S. von der Heydt
H. A. Dijkstra
H. A. Dijkstra
author_facet P. D. Nooteboom
P. D. Nooteboom
P. K. Bijl
C. Kehl
E. van Sebille
E. van Sebille
M. Ziegler
A. S. von der Heydt
A. S. von der Heydt
H. A. Dijkstra
H. A. Dijkstra
author_sort P. D. Nooteboom
collection DOAJ
description <p>Having descended through the water column, microplankton in ocean sediments is representative of the ocean surface environment, where it originated. Sedimentary microplankton is therefore used as an archive of past and present surface oceanographic conditions. However, these particles are advected by turbulent ocean currents during their sinking journey. So far, it is unknown to what extent this particle advection shapes the microplankton composition in sediments. Here we use global simulations of sinking particles in a strongly eddying global ocean model, and define ocean bottom provinces based on the particle surface origin locations. We find that these provinces can be detected in global datasets of sedimentary microplankton assemblages, demonstrating the effect provincialism has on the composition of sedimentary remains of surface plankton. These provinces explain the microplankton composition, in addition to, e.g., the ocean surface environment. Connected provinces have implications for the optimal spatial extent of microplankton sediment sample datasets that are used for palaeoceanographic reconstruction, and for the optimal spatial averaging of sediment samples over global datasets.</p>
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spelling doaj.art-c3c5dd3da21547ff97698dbf876188142022-12-21T17:24:39ZengCopernicus PublicationsEarth System Dynamics2190-49792190-49872022-02-011335737110.5194/esd-13-357-2022Sedimentary microplankton distributions are shaped by oceanographically connected areasP. D. Nooteboom0P. D. Nooteboom1P. K. Bijl2C. Kehl3E. van Sebille4E. van Sebille5M. Ziegler6A. S. von der Heydt7A. S. von der Heydt8H. A. Dijkstra9H. A. Dijkstra10Institute for Marine and Atmospheric research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the NetherlandsCentre for Complex Systems Studies, Utrecht University, Utrecht, the NetherlandsLaboratory of Palaeobotany and Palynology, Marine Palynology and Paleoceanography, Department of Earth Sciences, Utrecht University, Utrecht, the NetherlandsInstitute for Marine and Atmospheric research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the NetherlandsInstitute for Marine and Atmospheric research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the NetherlandsCentre for Complex Systems Studies, Utrecht University, Utrecht, the NetherlandsLaboratory of Palaeobotany and Palynology, Marine Palynology and Paleoceanography, Department of Earth Sciences, Utrecht University, Utrecht, the NetherlandsInstitute for Marine and Atmospheric research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the NetherlandsCentre for Complex Systems Studies, Utrecht University, Utrecht, the NetherlandsInstitute for Marine and Atmospheric research Utrecht (IMAU), Department of Physics, Utrecht University, Utrecht, the NetherlandsCentre for Complex Systems Studies, Utrecht University, Utrecht, the Netherlands<p>Having descended through the water column, microplankton in ocean sediments is representative of the ocean surface environment, where it originated. Sedimentary microplankton is therefore used as an archive of past and present surface oceanographic conditions. However, these particles are advected by turbulent ocean currents during their sinking journey. So far, it is unknown to what extent this particle advection shapes the microplankton composition in sediments. Here we use global simulations of sinking particles in a strongly eddying global ocean model, and define ocean bottom provinces based on the particle surface origin locations. We find that these provinces can be detected in global datasets of sedimentary microplankton assemblages, demonstrating the effect provincialism has on the composition of sedimentary remains of surface plankton. These provinces explain the microplankton composition, in addition to, e.g., the ocean surface environment. Connected provinces have implications for the optimal spatial extent of microplankton sediment sample datasets that are used for palaeoceanographic reconstruction, and for the optimal spatial averaging of sediment samples over global datasets.</p>https://esd.copernicus.org/articles/13/357/2022/esd-13-357-2022.pdf
spellingShingle P. D. Nooteboom
P. D. Nooteboom
P. K. Bijl
C. Kehl
E. van Sebille
E. van Sebille
M. Ziegler
A. S. von der Heydt
A. S. von der Heydt
H. A. Dijkstra
H. A. Dijkstra
Sedimentary microplankton distributions are shaped by oceanographically connected areas
Earth System Dynamics
title Sedimentary microplankton distributions are shaped by oceanographically connected areas
title_full Sedimentary microplankton distributions are shaped by oceanographically connected areas
title_fullStr Sedimentary microplankton distributions are shaped by oceanographically connected areas
title_full_unstemmed Sedimentary microplankton distributions are shaped by oceanographically connected areas
title_short Sedimentary microplankton distributions are shaped by oceanographically connected areas
title_sort sedimentary microplankton distributions are shaped by oceanographically connected areas
url https://esd.copernicus.org/articles/13/357/2022/esd-13-357-2022.pdf
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