Variability of chlorophyll-a and diatoms in the frontal ecosystem of Indian Ocean sector of the Southern Ocean
Phytoplankton composition plays a major role in biogeochemical cycles of the ocean. The intensity of carbon fixation and export is strongly dependent on the phytoplankton community. Yet, the contribution of different types of phytoplankton to the total production on various communities is still poor...
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ftdoajarticles:oai:doaj.org/article:f10a6db7df6e462eb3e639c72bdce0f4 2023-05-15T13:40:15+02:00 Variability of chlorophyll-a and diatoms in the frontal ecosystem of Indian Ocean sector of the Southern Ocean Rajani Kanta Mishra Babula Jena Anilkumar Narayana Pillai Ravidas Krishna Naik Venkateswaran Bhaskar Parli Melena A Soares 2017-09-01T00:00:00Z https://doi.org/10.1515/popore-2017-0014 https://doaj.org/article/f10a6db7df6e462eb3e639c72bdce0f4 EN eng Polish Academy of Sciences http://www.degruyter.com/view/j/popore.2017.38.issue-3/popore-2017-0014/popore-2017-0014.xml?format=INT https://doaj.org/toc/2081-8262 2081-8262 doi:10.1515/popore-2017-0014 https://doaj.org/article/f10a6db7df6e462eb3e639c72bdce0f4 Polish Polar Research, Vol 38, Iss 3, Pp 375-392 (2017) Antarctic Southern Ocean chlorophyll-a diatoms Geology QE1-996.5 article 2017 ftdoajarticles https://doi.org/10.1515/popore-2017-0014 2022-12-31T03:46:43Z Phytoplankton composition plays a major role in biogeochemical cycles of the ocean. The intensity of carbon fixation and export is strongly dependent on the phytoplankton community. Yet, the contribution of different types of phytoplankton to the total production on various communities is still poorly understood in the Indian Ocean sector of Southern Ocean (SO). Therefore the variability of chlorophyll-a (Chl-a) and diatoms in the frontal ecosystems of the Indian sector of SO have been investigated along with the sea surface temperature (SST), sea surface wind (SSW), photosynthetically active radiation (PAR), and nutrients datasets for the period of 1998–2012. Combined analysis of in-situ, model and satellite observations indicate that the variability of Chl-a and diatoms were primarily influenced by light and wind. The Chl-a was higher at the sub-Antarctic front (SAF) followed by the sub-tropical front (STF) and the polar front (PF). The diatom concentration was higher at the SAF followed by the PF and STF. Maximum concentration of Chl-a and diatoms commonly observed at the SAF region are probably due to the moderate PAR, SST and wind. Dominance of diatoms at the PF may be attributed to their adaptability for low light conditions. The results from this study in the frontal ecosystems would help to understand the biogeochemical cycle of the Indian sector of the SO. Article in Journal/Newspaper Antarc* Antarctic Polar Research Southern Ocean Directory of Open Access Journals: DOAJ Articles Antarctic Indian Southern Ocean Polish Polar Research 38 3 375 392 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Antarctic Southern Ocean chlorophyll-a diatoms Geology QE1-996.5 |
spellingShingle |
Antarctic Southern Ocean chlorophyll-a diatoms Geology QE1-996.5 Rajani Kanta Mishra Babula Jena Anilkumar Narayana Pillai Ravidas Krishna Naik Venkateswaran Bhaskar Parli Melena A Soares Variability of chlorophyll-a and diatoms in the frontal ecosystem of Indian Ocean sector of the Southern Ocean |
topic_facet |
Antarctic Southern Ocean chlorophyll-a diatoms Geology QE1-996.5 |
description |
Phytoplankton composition plays a major role in biogeochemical cycles of the ocean. The intensity of carbon fixation and export is strongly dependent on the phytoplankton community. Yet, the contribution of different types of phytoplankton to the total production on various communities is still poorly understood in the Indian Ocean sector of Southern Ocean (SO). Therefore the variability of chlorophyll-a (Chl-a) and diatoms in the frontal ecosystems of the Indian sector of SO have been investigated along with the sea surface temperature (SST), sea surface wind (SSW), photosynthetically active radiation (PAR), and nutrients datasets for the period of 1998–2012. Combined analysis of in-situ, model and satellite observations indicate that the variability of Chl-a and diatoms were primarily influenced by light and wind. The Chl-a was higher at the sub-Antarctic front (SAF) followed by the sub-tropical front (STF) and the polar front (PF). The diatom concentration was higher at the SAF followed by the PF and STF. Maximum concentration of Chl-a and diatoms commonly observed at the SAF region are probably due to the moderate PAR, SST and wind. Dominance of diatoms at the PF may be attributed to their adaptability for low light conditions. The results from this study in the frontal ecosystems would help to understand the biogeochemical cycle of the Indian sector of the SO. |
format |
Article in Journal/Newspaper |
author |
Rajani Kanta Mishra Babula Jena Anilkumar Narayana Pillai Ravidas Krishna Naik Venkateswaran Bhaskar Parli Melena A Soares |
author_facet |
Rajani Kanta Mishra Babula Jena Anilkumar Narayana Pillai Ravidas Krishna Naik Venkateswaran Bhaskar Parli Melena A Soares |
author_sort |
Rajani Kanta Mishra |
title |
Variability of chlorophyll-a and diatoms in the frontal ecosystem of Indian Ocean sector of the Southern Ocean |
title_short |
Variability of chlorophyll-a and diatoms in the frontal ecosystem of Indian Ocean sector of the Southern Ocean |
title_full |
Variability of chlorophyll-a and diatoms in the frontal ecosystem of Indian Ocean sector of the Southern Ocean |
title_fullStr |
Variability of chlorophyll-a and diatoms in the frontal ecosystem of Indian Ocean sector of the Southern Ocean |
title_full_unstemmed |
Variability of chlorophyll-a and diatoms in the frontal ecosystem of Indian Ocean sector of the Southern Ocean |
title_sort |
variability of chlorophyll-a and diatoms in the frontal ecosystem of indian ocean sector of the southern ocean |
publisher |
Polish Academy of Sciences |
publishDate |
2017 |
url |
https://doi.org/10.1515/popore-2017-0014 https://doaj.org/article/f10a6db7df6e462eb3e639c72bdce0f4 |
geographic |
Antarctic Indian Southern Ocean |
geographic_facet |
Antarctic Indian Southern Ocean |
genre |
Antarc* Antarctic Polar Research Southern Ocean |
genre_facet |
Antarc* Antarctic Polar Research Southern Ocean |
op_source |
Polish Polar Research, Vol 38, Iss 3, Pp 375-392 (2017) |
op_relation |
http://www.degruyter.com/view/j/popore.2017.38.issue-3/popore-2017-0014/popore-2017-0014.xml?format=INT https://doaj.org/toc/2081-8262 2081-8262 doi:10.1515/popore-2017-0014 https://doaj.org/article/f10a6db7df6e462eb3e639c72bdce0f4 |
op_doi |
https://doi.org/10.1515/popore-2017-0014 |
container_title |
Polish Polar Research |
container_volume |
38 |
container_issue |
3 |
container_start_page |
375 |
op_container_end_page |
392 |
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1766131542361374720 |