Roles of Iron Limitation in Phytoplankton Dynamics in the Western and Eastern Subarctic Pacific
The subarctic Pacific is one of the major high-nitrate, low-chlorophyll (HNLC) regions where marine productivity is greatly limited by the supply of iron (Fe) in the region. There is a distinct seasonal difference in the chlorophyll concentrations of the east and west sides of the subarctic Pacific...
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ftdoajarticles:oai:doaj.org/article:d7004130c7ed4dcf9ad5aabc84372fbb 2023-05-15T18:27:43+02:00 Roles of Iron Limitation in Phytoplankton Dynamics in the Western and Eastern Subarctic Pacific Hao-Ran Zhang Yuntao Wang Peng Xiu Yiquan Qi Fei Chai 2021-09-01T00:00:00Z https://doi.org/10.3389/fmars.2021.735826 https://doaj.org/article/d7004130c7ed4dcf9ad5aabc84372fbb EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fmars.2021.735826/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2021.735826 https://doaj.org/article/d7004130c7ed4dcf9ad5aabc84372fbb Frontiers in Marine Science, Vol 8 (2021) subarctic north Pacific iron limitation phytoplankton dynamics seasonal variation future change Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2021 ftdoajarticles https://doi.org/10.3389/fmars.2021.735826 2022-12-31T12:59:26Z The subarctic Pacific is one of the major high-nitrate, low-chlorophyll (HNLC) regions where marine productivity is greatly limited by the supply of iron (Fe) in the region. There is a distinct seasonal difference in the chlorophyll concentrations of the east and west sides of the subarctic Pacific because of the differences in their driving mechanisms. In the western subarctic Pacific, two chlorophyll concentration peaks occur: the peak in spring and early summer is dominated by diatoms, while the peak in late summer and autumn is dominated by small phytoplankton. In the eastern subarctic Pacific, a single chlorophyll concentration peak occurs in late summer, while small phytoplankton dominate throughout the year. In this study, two one-dimensional (1D) physical–biological models with Fe cycles were applied to Ocean Station K2 (Stn. K2) in the western subarctic Pacific and Ocean Station Papa (Stn. Papa) in the eastern subarctic Pacific. These models were used to study the role of Fe limitation in regulating the seasonal differences in phytoplankton populations by reproducing the seasonal variability in ocean properties in each region. The results were reasonably comparable with observational data, i.e., cruise and Biogeochemical-Argo data, showing that the difference in bioavailable Fe (BFe) between Stn. K2 and Stn. Papa played a dominant role in controlling the respective seasonal variabilities of diatom and small phytoplankton growth. At Stn. Papa, there was less BFe, and the Fe limitation of diatom growth was two times as strong as that at Stn. K2; however, the difference in the Fe limitation of small phytoplankton growth between these two regions was relatively small. At Stn. K2, the decrease in BFe during summer reduced the growth rate of diatoms, which led to a rapid reduction in diatom biomass. Simultaneously, the decrease in BFe had little impact on small phytoplankton growth, which helped maintain the relatively high small phytoplankton biomass until autumn. The experiments that stimulated a further ... Article in Journal/Newspaper Subarctic Directory of Open Access Journals: DOAJ Articles Pacific Frontiers in Marine Science 8 |
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op_collection_id |
ftdoajarticles |
language |
English |
topic |
subarctic north Pacific iron limitation phytoplankton dynamics seasonal variation future change Science Q General. Including nature conservation geographical distribution QH1-199.5 |
spellingShingle |
subarctic north Pacific iron limitation phytoplankton dynamics seasonal variation future change Science Q General. Including nature conservation geographical distribution QH1-199.5 Hao-Ran Zhang Yuntao Wang Peng Xiu Yiquan Qi Fei Chai Roles of Iron Limitation in Phytoplankton Dynamics in the Western and Eastern Subarctic Pacific |
topic_facet |
subarctic north Pacific iron limitation phytoplankton dynamics seasonal variation future change Science Q General. Including nature conservation geographical distribution QH1-199.5 |
description |
The subarctic Pacific is one of the major high-nitrate, low-chlorophyll (HNLC) regions where marine productivity is greatly limited by the supply of iron (Fe) in the region. There is a distinct seasonal difference in the chlorophyll concentrations of the east and west sides of the subarctic Pacific because of the differences in their driving mechanisms. In the western subarctic Pacific, two chlorophyll concentration peaks occur: the peak in spring and early summer is dominated by diatoms, while the peak in late summer and autumn is dominated by small phytoplankton. In the eastern subarctic Pacific, a single chlorophyll concentration peak occurs in late summer, while small phytoplankton dominate throughout the year. In this study, two one-dimensional (1D) physical–biological models with Fe cycles were applied to Ocean Station K2 (Stn. K2) in the western subarctic Pacific and Ocean Station Papa (Stn. Papa) in the eastern subarctic Pacific. These models were used to study the role of Fe limitation in regulating the seasonal differences in phytoplankton populations by reproducing the seasonal variability in ocean properties in each region. The results were reasonably comparable with observational data, i.e., cruise and Biogeochemical-Argo data, showing that the difference in bioavailable Fe (BFe) between Stn. K2 and Stn. Papa played a dominant role in controlling the respective seasonal variabilities of diatom and small phytoplankton growth. At Stn. Papa, there was less BFe, and the Fe limitation of diatom growth was two times as strong as that at Stn. K2; however, the difference in the Fe limitation of small phytoplankton growth between these two regions was relatively small. At Stn. K2, the decrease in BFe during summer reduced the growth rate of diatoms, which led to a rapid reduction in diatom biomass. Simultaneously, the decrease in BFe had little impact on small phytoplankton growth, which helped maintain the relatively high small phytoplankton biomass until autumn. The experiments that stimulated a further ... |
format |
Article in Journal/Newspaper |
author |
Hao-Ran Zhang Yuntao Wang Peng Xiu Yiquan Qi Fei Chai |
author_facet |
Hao-Ran Zhang Yuntao Wang Peng Xiu Yiquan Qi Fei Chai |
author_sort |
Hao-Ran Zhang |
title |
Roles of Iron Limitation in Phytoplankton Dynamics in the Western and Eastern Subarctic Pacific |
title_short |
Roles of Iron Limitation in Phytoplankton Dynamics in the Western and Eastern Subarctic Pacific |
title_full |
Roles of Iron Limitation in Phytoplankton Dynamics in the Western and Eastern Subarctic Pacific |
title_fullStr |
Roles of Iron Limitation in Phytoplankton Dynamics in the Western and Eastern Subarctic Pacific |
title_full_unstemmed |
Roles of Iron Limitation in Phytoplankton Dynamics in the Western and Eastern Subarctic Pacific |
title_sort |
roles of iron limitation in phytoplankton dynamics in the western and eastern subarctic pacific |
publisher |
Frontiers Media S.A. |
publishDate |
2021 |
url |
https://doi.org/10.3389/fmars.2021.735826 https://doaj.org/article/d7004130c7ed4dcf9ad5aabc84372fbb |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Subarctic |
genre_facet |
Subarctic |
op_source |
Frontiers in Marine Science, Vol 8 (2021) |
op_relation |
https://www.frontiersin.org/articles/10.3389/fmars.2021.735826/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2021.735826 https://doaj.org/article/d7004130c7ed4dcf9ad5aabc84372fbb |
op_doi |
https://doi.org/10.3389/fmars.2021.735826 |
container_title |
Frontiers in Marine Science |
container_volume |
8 |
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1766209874570510336 |