Small pigmented eukaryotes play a major role in carbon cycling in the P‐depleted western subtropical North Atlantic, which may be supported by mixotrophy
Abstract We found that in the phosphate (PO 4 )‐depleted western subtropical North Atlantic Ocean, small‐sized pigmented eukaryotes (P‐Euk; < 5 μ m) play a central role in the carbon (C) cycling. Although P‐Euk were only ~ 5% of the microbial phytoplankton cell abundance, they represented at leas...
Published in: | Limnology and Oceanography |
---|---|
Main Authors: | , , , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2019
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1002/lno.11193 https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11193 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.11193 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11193 |
id |
crwiley:10.1002/lno.11193 |
---|---|
record_format |
openpolar |
spelling |
crwiley:10.1002/lno.11193 2024-09-15T18:22:03+00:00 Small pigmented eukaryotes play a major role in carbon cycling in the P‐depleted western subtropical North Atlantic, which may be supported by mixotrophy Duhamel, Solange Kim, Eunsoo Sprung, Ben Anderson, O. Roger National Science Foundation 2019 http://dx.doi.org/10.1002/lno.11193 https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11193 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.11193 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11193 en eng Wiley http://creativecommons.org/licenses/by-nc/4.0/ http://creativecommons.org/licenses/by-nc/4.0/ Limnology and Oceanography volume 64, issue 6, page 2424-2440 ISSN 0024-3590 1939-5590 journal-article 2019 crwiley https://doi.org/10.1002/lno.11193 2024-07-23T04:16:04Z Abstract We found that in the phosphate (PO 4 )‐depleted western subtropical North Atlantic Ocean, small‐sized pigmented eukaryotes (P‐Euk; < 5 μ m) play a central role in the carbon (C) cycling. Although P‐Euk were only ~ 5% of the microbial phytoplankton cell abundance, they represented at least two thirds of the microbial phytoplankton C biomass and fixed more CO 2 than picocyanobacteria, accounting for roughly half of the volumetric CO 2 fixation by the microbial phytoplankton, or a third of the total primary production. Cell‐specific PO 4 assimilation rates of P‐Euk and nonpigmented eukaryotes (NP‐Euk; < 5 μ m) were generally higher than of picocyanobacteria. However, when normalized to biovolumes, picocyanobacteria assimilated roughly four times more PO 4 than small eukaryotes, indicating different strategies to cope with PO 4 limitation. Our results underline an imbalance in the CO 2 : PO 4 uptake rate ratios, which may be explained by phagotrophic predation providing mixotrophic protists with their largest source of PO 4 . 18S rDNA amplicon sequence analyses suggested that P‐Euk was dominated by members of green algae and dinoflagellates, the latter group commonly mixotrophic, whereas marine alveolates were the dominant NP‐Euk. Bacterivory by P‐Euk (0.9 ± 0.3 bacteria P‐Euk −1 h −1 ) was comparable to values previously measured in the central North Atlantic, indicating that small mixotrophic eukaryotes likely exhibit similar predatory pressure on bacteria. Interestingly, bacterivory rates were reduced when PO 4 was added during experimental incubations, indicating that feeding rate by P‐Euk is regulated by PO 4 availability. This may be in response to the higher cost associated with assimilating PO 4 by phagocytosis compared to osmotrophy. Article in Journal/Newspaper North Atlantic Wiley Online Library Limnology and Oceanography 64 6 2424 2440 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Abstract We found that in the phosphate (PO 4 )‐depleted western subtropical North Atlantic Ocean, small‐sized pigmented eukaryotes (P‐Euk; < 5 μ m) play a central role in the carbon (C) cycling. Although P‐Euk were only ~ 5% of the microbial phytoplankton cell abundance, they represented at least two thirds of the microbial phytoplankton C biomass and fixed more CO 2 than picocyanobacteria, accounting for roughly half of the volumetric CO 2 fixation by the microbial phytoplankton, or a third of the total primary production. Cell‐specific PO 4 assimilation rates of P‐Euk and nonpigmented eukaryotes (NP‐Euk; < 5 μ m) were generally higher than of picocyanobacteria. However, when normalized to biovolumes, picocyanobacteria assimilated roughly four times more PO 4 than small eukaryotes, indicating different strategies to cope with PO 4 limitation. Our results underline an imbalance in the CO 2 : PO 4 uptake rate ratios, which may be explained by phagotrophic predation providing mixotrophic protists with their largest source of PO 4 . 18S rDNA amplicon sequence analyses suggested that P‐Euk was dominated by members of green algae and dinoflagellates, the latter group commonly mixotrophic, whereas marine alveolates were the dominant NP‐Euk. Bacterivory by P‐Euk (0.9 ± 0.3 bacteria P‐Euk −1 h −1 ) was comparable to values previously measured in the central North Atlantic, indicating that small mixotrophic eukaryotes likely exhibit similar predatory pressure on bacteria. Interestingly, bacterivory rates were reduced when PO 4 was added during experimental incubations, indicating that feeding rate by P‐Euk is regulated by PO 4 availability. This may be in response to the higher cost associated with assimilating PO 4 by phagocytosis compared to osmotrophy. |
author2 |
National Science Foundation |
format |
Article in Journal/Newspaper |
author |
Duhamel, Solange Kim, Eunsoo Sprung, Ben Anderson, O. Roger |
spellingShingle |
Duhamel, Solange Kim, Eunsoo Sprung, Ben Anderson, O. Roger Small pigmented eukaryotes play a major role in carbon cycling in the P‐depleted western subtropical North Atlantic, which may be supported by mixotrophy |
author_facet |
Duhamel, Solange Kim, Eunsoo Sprung, Ben Anderson, O. Roger |
author_sort |
Duhamel, Solange |
title |
Small pigmented eukaryotes play a major role in carbon cycling in the P‐depleted western subtropical North Atlantic, which may be supported by mixotrophy |
title_short |
Small pigmented eukaryotes play a major role in carbon cycling in the P‐depleted western subtropical North Atlantic, which may be supported by mixotrophy |
title_full |
Small pigmented eukaryotes play a major role in carbon cycling in the P‐depleted western subtropical North Atlantic, which may be supported by mixotrophy |
title_fullStr |
Small pigmented eukaryotes play a major role in carbon cycling in the P‐depleted western subtropical North Atlantic, which may be supported by mixotrophy |
title_full_unstemmed |
Small pigmented eukaryotes play a major role in carbon cycling in the P‐depleted western subtropical North Atlantic, which may be supported by mixotrophy |
title_sort |
small pigmented eukaryotes play a major role in carbon cycling in the p‐depleted western subtropical north atlantic, which may be supported by mixotrophy |
publisher |
Wiley |
publishDate |
2019 |
url |
http://dx.doi.org/10.1002/lno.11193 https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11193 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.11193 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11193 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Limnology and Oceanography volume 64, issue 6, page 2424-2440 ISSN 0024-3590 1939-5590 |
op_rights |
http://creativecommons.org/licenses/by-nc/4.0/ http://creativecommons.org/licenses/by-nc/4.0/ |
op_doi |
https://doi.org/10.1002/lno.11193 |
container_title |
Limnology and Oceanography |
container_volume |
64 |
container_issue |
6 |
container_start_page |
2424 |
op_container_end_page |
2440 |
_version_ |
1810461344271433728 |