The Effect of Upwelling on Distribution and Abundance of Phytoplankton in Indonesia

East Monsoon is monsoon where upwelling process happened in Banda Sea. Information about upwelling effect to the abundance and distribution of phytoplankton in Banda Sea is not known much.yet. That way has been done the investigation in August 1997 as vice of east monsoon and October 1998 as vice of...

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Main Author: Agus Sediadi
Format: Article
Language:English
Published: Universitas Indonesia 2004-08-01
Series:Makara Seri Sains
Subjects:
Online Access:http://journal.ui.ac.id/science/article/view/409/405
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author Agus Sediadi
author_facet Agus Sediadi
author_sort Agus Sediadi
collection DOAJ
description East Monsoon is monsoon where upwelling process happened in Banda Sea. Information about upwelling effect to the abundance and distribution of phytoplankton in Banda Sea is not known much.yet. That way has been done the investigation in August 1997 as vice of east monsoon and October 1998 as vice of transition monsoon as comparation.. The abundance and distribution data collected by taken phytoplankton sample in 100 m depth to surface by using plankton net with diameter 31 cm, 120 cm length, and eyes net size 80 μm. The results in east monsoon (August 1997) where (upwelling) still done. This correlation seen from regresi value between temperature and salinity (r2 = 84,1 %), temperature and nitrate (94,5%) In east monsoon recorded 33 phytoplankton species, composition of phytoplankton is varied more compared to transition monsoon where found 26 phytoplankton species only. In east monsoon dominance phytoplankton is Chaetoceros sp. Further analysis by using multivariate analysis, nitrate factor affect to abundance, composition, and distribution ofphytoplankton.
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spelling doaj.art-c7a1d62d350d4c88bbb0522601476b1f2022-12-21T17:12:54ZengUniversitas IndonesiaMakara Seri Sains1693-66712004-08-010824351The Effect of Upwelling on Distribution and Abundance of Phytoplankton in IndonesiaAgus SediadiEast Monsoon is monsoon where upwelling process happened in Banda Sea. Information about upwelling effect to the abundance and distribution of phytoplankton in Banda Sea is not known much.yet. That way has been done the investigation in August 1997 as vice of east monsoon and October 1998 as vice of transition monsoon as comparation.. The abundance and distribution data collected by taken phytoplankton sample in 100 m depth to surface by using plankton net with diameter 31 cm, 120 cm length, and eyes net size 80 μm. The results in east monsoon (August 1997) where (upwelling) still done. This correlation seen from regresi value between temperature and salinity (r2 = 84,1 %), temperature and nitrate (94,5%) In east monsoon recorded 33 phytoplankton species, composition of phytoplankton is varied more compared to transition monsoon where found 26 phytoplankton species only. In east monsoon dominance phytoplankton is Chaetoceros sp. Further analysis by using multivariate analysis, nitrate factor affect to abundance, composition, and distribution ofphytoplankton.http://journal.ui.ac.id/science/article/view/409/405Chaetoceros sp.Banda Seamultivariate analysisupwelling
spellingShingle Agus Sediadi
The Effect of Upwelling on Distribution and Abundance of Phytoplankton in Indonesia
Makara Seri Sains
Chaetoceros sp.
Banda Sea
multivariate analysis
upwelling
title The Effect of Upwelling on Distribution and Abundance of Phytoplankton in Indonesia
title_full The Effect of Upwelling on Distribution and Abundance of Phytoplankton in Indonesia
title_fullStr The Effect of Upwelling on Distribution and Abundance of Phytoplankton in Indonesia
title_full_unstemmed The Effect of Upwelling on Distribution and Abundance of Phytoplankton in Indonesia
title_short The Effect of Upwelling on Distribution and Abundance of Phytoplankton in Indonesia
title_sort effect of upwelling on distribution and abundance of phytoplankton in indonesia
topic Chaetoceros sp.
Banda Sea
multivariate analysis
upwelling
url http://journal.ui.ac.id/science/article/view/409/405
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