Saved in:
Bibliographic Details
Main Authors: van der Jagt, Helga, Friese, Carmen A, Stuut, Jan-Berend W, Fischer, Gerhard, Iversen, Morten Hvitfeldt
Format: Dataset Open Access
Language:en
Published: PANGAEA 2018
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.885930
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1867168571329609728
author van der Jagt, Helga
Friese, Carmen A
Stuut, Jan-Berend W
Fischer, Gerhard
Iversen, Morten Hvitfeldt
author_facet van der Jagt, Helga
Friese, Carmen A
Stuut, Jan-Berend W
Fischer, Gerhard
Iversen, Morten Hvitfeldt
collection Datos científicos de ciencias marinas y ambientales
contents Lithogenic material such as Saharan dust can be incorporated into organic aggregates and act as ballast, potentially enhancing the marine carbon export via increased sinking velocities of aggregates. We studied the ballasting effects of Saharan dust on the aggregate dynamics in the upwelling region off Cape Blanc (Mauritania). Aggregate formation from a natural plankton community exposed to Saharan dust deposition resulted in higher abundance of aggregates with higher sinking velocities compared to aggregate formation with low dust. This higher aggregate abundance and sinking velocities potentially increased the carbon export 10-fold when the aggregates were ballasted by Saharan dust. After aggregate formation in the surface waters, subsequent sinking through suspended Saharan dust minerals had no influence on aggregate sizes, abundance, and sinking velocities. We found that aggregates formed in the surface ocean off Mauritania were already heavily ballasted with lithogenic material and could therefore not scavenge any additional minerals during their descent. This suggests that carbon export to the deep ocean in regions with high dust deposition is strongly controlled by dust input to the surface ocean while suspended dust particles in deeper water layers do not significantly interact with sinking aggregates.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_885930
institution PANGAEA
language en
publishDate 2018
publisher PANGAEA
record_format pangaea
spellingShingle Ballasting effects of Saharan dust on the aggregate dynamics in the upwelling region off Cape Blanc (Mauritania)
van der Jagt, Helga
Friese, Carmen A
Stuut, Jan-Berend W
Fischer, Gerhard
Iversen, Morten Hvitfeldt
Center for Marine Environmental Sciences; MARUM; SeaPump; Seasonal and regional food web interactions with the biological pump
Lithogenic material such as Saharan dust can be incorporated into organic aggregates and act as ballast, potentially enhancing the marine carbon export via increased sinking velocities of aggregates. We studied the ballasting effects of Saharan dust on the aggregate dynamics in the upwelling region off Cape Blanc (Mauritania). Aggregate formation from a natural plankton community exposed to Saharan dust deposition resulted in higher abundance of aggregates with higher sinking velocities compared to aggregate formation with low dust. This higher aggregate abundance and sinking velocities potentially increased the carbon export 10-fold when the aggregates were ballasted by Saharan dust. After aggregate formation in the surface waters, subsequent sinking through suspended Saharan dust minerals had no influence on aggregate sizes, abundance, and sinking velocities. We found that aggregates formed in the surface ocean off Mauritania were already heavily ballasted with lithogenic material and could therefore not scavenge any additional minerals during their descent. This suggests that carbon export to the deep ocean in regions with high dust deposition is strongly controlled by dust input to the surface ocean while suspended dust particles in deeper water layers do not significantly interact with sinking aggregates.
title Ballasting effects of Saharan dust on the aggregate dynamics in the upwelling region off Cape Blanc (Mauritania)
topic Center for Marine Environmental Sciences; MARUM; SeaPump; Seasonal and regional food web interactions with the biological pump
url https://doi.org/10.1594/PANGAEA.885930