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Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon

We studied the biodiversity of autotrophic calcareous coccolithophore assemblages at 30 locations in the Eastern Equatorial Indian Ocean (EEIO) (80°–94°E, 6°N–5°S) and evaluated the importance of regional hydrology. We documented 26 species based on the identification of coccospheres and coccoliths,...

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Detalles Bibliográficos
Autores principales: Liu, Haijiao, Sun, Jun, Wang, Dongxiao, Zhang, Xiaodong, Zhang, Cuixia, Song, Shuqun, Thangaraj, Satheeswaran
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6104084/
https://www.ncbi.nlm.nih.gov/pubmed/30131499
http://dx.doi.org/10.1038/s41598-018-29688-w
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author Liu, Haijiao
Sun, Jun
Wang, Dongxiao
Zhang, Xiaodong
Zhang, Cuixia
Song, Shuqun
Thangaraj, Satheeswaran
author_facet Liu, Haijiao
Sun, Jun
Wang, Dongxiao
Zhang, Xiaodong
Zhang, Cuixia
Song, Shuqun
Thangaraj, Satheeswaran
author_sort Liu, Haijiao
collection PubMed
description We studied the biodiversity of autotrophic calcareous coccolithophore assemblages at 30 locations in the Eastern Equatorial Indian Ocean (EEIO) (80°–94°E, 6°N–5°S) and evaluated the importance of regional hydrology. We documented 26 species based on the identification of coccospheres and coccoliths, respectively. The coccolithophore community was dominated by Gephyrocapsa oceanica, Emiliania huxleyi, Florisphaera profunda, Umbilicosphaera sibogae, and Helicosphaera carteri. The abundance of coccoliths and coccospheres ranged from 0.2 × 10(3) to 160 × 10(3) coccoliths l(−1) and 0.2 × 10(3) to 68 × 10(3) cells l(−1), averaged 23 × 10(3) coccoliths l(−1) and 9.4 × 10(3) cells l(−1), respectively. Biogenic PIC, POC, and rain ratio mean values were 0.50 μgC l(−1), 1.047 μgC l(−1), and 0.10 respectively. High abundances of both coccoliths and coccospheres in the surface ocean layer occurred on the north of the equator. Vertically, the great majority of coccoliths and coccospheres were concentrated in water taken from depths of <75 m. The ratios between the number of coccospheres and free coccoliths indicated that coccoliths experience different levels of dissolution when transported to deep water. Abundant coccolithophores mainly occurred at the west of 90°E, which is in accordance with the presence of Wyrtki jets. Patterns of coccolithosphores and of coccoliths have been reflected in hydrological processes.
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spelling pubmed-61040842018-08-27 Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon Liu, Haijiao Sun, Jun Wang, Dongxiao Zhang, Xiaodong Zhang, Cuixia Song, Shuqun Thangaraj, Satheeswaran Sci Rep Article We studied the biodiversity of autotrophic calcareous coccolithophore assemblages at 30 locations in the Eastern Equatorial Indian Ocean (EEIO) (80°–94°E, 6°N–5°S) and evaluated the importance of regional hydrology. We documented 26 species based on the identification of coccospheres and coccoliths, respectively. The coccolithophore community was dominated by Gephyrocapsa oceanica, Emiliania huxleyi, Florisphaera profunda, Umbilicosphaera sibogae, and Helicosphaera carteri. The abundance of coccoliths and coccospheres ranged from 0.2 × 10(3) to 160 × 10(3) coccoliths l(−1) and 0.2 × 10(3) to 68 × 10(3) cells l(−1), averaged 23 × 10(3) coccoliths l(−1) and 9.4 × 10(3) cells l(−1), respectively. Biogenic PIC, POC, and rain ratio mean values were 0.50 μgC l(−1), 1.047 μgC l(−1), and 0.10 respectively. High abundances of both coccoliths and coccospheres in the surface ocean layer occurred on the north of the equator. Vertically, the great majority of coccoliths and coccospheres were concentrated in water taken from depths of <75 m. The ratios between the number of coccospheres and free coccoliths indicated that coccoliths experience different levels of dissolution when transported to deep water. Abundant coccolithophores mainly occurred at the west of 90°E, which is in accordance with the presence of Wyrtki jets. Patterns of coccolithosphores and of coccoliths have been reflected in hydrological processes. Nature Publishing Group UK 2018-08-21 /pmc/articles/PMC6104084/ /pubmed/30131499 http://dx.doi.org/10.1038/s41598-018-29688-w Text en © The Author(s) 2018 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
spellingShingle Article
Liu, Haijiao
Sun, Jun
Wang, Dongxiao
Zhang, Xiaodong
Zhang, Cuixia
Song, Shuqun
Thangaraj, Satheeswaran
Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon
title Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon
title_full Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon
title_fullStr Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon
title_full_unstemmed Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon
title_short Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon
title_sort distribution of living coccolithophores in eastern indian ocean during spring intermonsoon
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6104084/
https://www.ncbi.nlm.nih.gov/pubmed/30131499
http://dx.doi.org/10.1038/s41598-018-29688-w
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