Nutrient regulation of late spring phytoplankton blooms in the midlatitude North Atlantic

The duration and magnitude of the North Atlantic spring bloom impacts both higher trophic levels and oceanic carbon sequestration. Nutrient exhaustion offers a general explanation for bloom termination, but detail on which nutrients and their relative influence on phytoplankton productivity, communi...

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Main Authors: Browning, Thomas J., Al-Hashem, Ali A., Hopwood, Mark J., Engel, Anja, Wakefield, Ewan D., Achterberg, Eric P.
Format: Text
Language:English
Published: FID GEO 2019
Subjects:
Online Access:https://dx.doi.org/10.23689/fidgeo-4967
https://e-docs.geo-leo.de/handle/11858/9313
id ftdatacite:10.23689/fidgeo-4967
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spelling ftdatacite:10.23689/fidgeo-4967 2023-05-15T17:29:21+02:00 Nutrient regulation of late spring phytoplankton blooms in the midlatitude North Atlantic Browning, Thomas J. Al-Hashem, Ali A. Hopwood, Mark J. Engel, Anja Wakefield, Ewan D. Achterberg, Eric P. 2019 https://dx.doi.org/10.23689/fidgeo-4967 https://e-docs.geo-leo.de/handle/11858/9313 en eng FID GEO Article article-journal Text ScholarlyArticle 2019 ftdatacite https://doi.org/10.23689/fidgeo-4967 2022-02-08T15:07:01Z The duration and magnitude of the North Atlantic spring bloom impacts both higher trophic levels and oceanic carbon sequestration. Nutrient exhaustion offers a general explanation for bloom termination, but detail on which nutrients and their relative influence on phytoplankton productivity, community structure, and physiology is lacking. Here, we address this using nutrient addition bioassay experiments conducted across the midlatitude North Atlantic in June 2017 (late spring). In four out of six experiments, phytoplankton accumulated over 48–72 h following individual additions of either iron (Fe) or nitrogen (N). In the remaining two experiments, Fe and N were serially limiting, that is, their combined addition sequentially enhanced phytoplankton accumulation. Silicic acid (Si) added in combination with N + Fe led to further chlorophyll a (Chl a) enhancement at two sites. Conversely, addition of zinc, manganese, cobalt, vitamin B12, or phosphate in combination with N + Fe did not. At two sites, the simultaneous supply of all six nutrients, in combination with N + Fe, also led to no further Chl a enhancement, but did result in an additional 30–60% particulate carbon accumulation. This particulate carbon accumulation was not matched by a Redfield equivalent of particulate N, characteristic of high C:N organic exudates that enhance cell aggregation and sinking. Our results suggest that growth rates of larger phytoplankton were primarily limited by Fe and/or N, making the availability of these nutrients the main bottom-up factors contributing to spring bloom termination. In addition, the simultaneous availability of other nutrients could modify bloom characteristics and carbon export efficiency. Text North Atlantic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
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language English
description The duration and magnitude of the North Atlantic spring bloom impacts both higher trophic levels and oceanic carbon sequestration. Nutrient exhaustion offers a general explanation for bloom termination, but detail on which nutrients and their relative influence on phytoplankton productivity, community structure, and physiology is lacking. Here, we address this using nutrient addition bioassay experiments conducted across the midlatitude North Atlantic in June 2017 (late spring). In four out of six experiments, phytoplankton accumulated over 48–72 h following individual additions of either iron (Fe) or nitrogen (N). In the remaining two experiments, Fe and N were serially limiting, that is, their combined addition sequentially enhanced phytoplankton accumulation. Silicic acid (Si) added in combination with N + Fe led to further chlorophyll a (Chl a) enhancement at two sites. Conversely, addition of zinc, manganese, cobalt, vitamin B12, or phosphate in combination with N + Fe did not. At two sites, the simultaneous supply of all six nutrients, in combination with N + Fe, also led to no further Chl a enhancement, but did result in an additional 30–60% particulate carbon accumulation. This particulate carbon accumulation was not matched by a Redfield equivalent of particulate N, characteristic of high C:N organic exudates that enhance cell aggregation and sinking. Our results suggest that growth rates of larger phytoplankton were primarily limited by Fe and/or N, making the availability of these nutrients the main bottom-up factors contributing to spring bloom termination. In addition, the simultaneous availability of other nutrients could modify bloom characteristics and carbon export efficiency.
format Text
author Browning, Thomas J.
Al-Hashem, Ali A.
Hopwood, Mark J.
Engel, Anja
Wakefield, Ewan D.
Achterberg, Eric P.
spellingShingle Browning, Thomas J.
Al-Hashem, Ali A.
Hopwood, Mark J.
Engel, Anja
Wakefield, Ewan D.
Achterberg, Eric P.
Nutrient regulation of late spring phytoplankton blooms in the midlatitude North Atlantic
author_facet Browning, Thomas J.
Al-Hashem, Ali A.
Hopwood, Mark J.
Engel, Anja
Wakefield, Ewan D.
Achterberg, Eric P.
author_sort Browning, Thomas J.
title Nutrient regulation of late spring phytoplankton blooms in the midlatitude North Atlantic
title_short Nutrient regulation of late spring phytoplankton blooms in the midlatitude North Atlantic
title_full Nutrient regulation of late spring phytoplankton blooms in the midlatitude North Atlantic
title_fullStr Nutrient regulation of late spring phytoplankton blooms in the midlatitude North Atlantic
title_full_unstemmed Nutrient regulation of late spring phytoplankton blooms in the midlatitude North Atlantic
title_sort nutrient regulation of late spring phytoplankton blooms in the midlatitude north atlantic
publisher FID GEO
publishDate 2019
url https://dx.doi.org/10.23689/fidgeo-4967
https://e-docs.geo-leo.de/handle/11858/9313
genre North Atlantic
genre_facet North Atlantic
op_doi https://doi.org/10.23689/fidgeo-4967
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