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A 5-year study of the influence of the northeast and southwest monsoons on copepod assemblages in the boundary coastal waters between the East China Sea and the Taiwan Strait

Identifieur interne : 009A66 ( Main/Exploration ); précédent : 009A65; suivant : 009A67

A 5-year study of the influence of the northeast and southwest monsoons on copepod assemblages in the boundary coastal waters between the East China Sea and the Taiwan Strait

Auteurs : Jiang-Shiou Hwang [République populaire de Chine, Taïwan] ; Sami Souissi ; Li-Chun Tseng [République populaire de Chine] ; Laurent Seuront ; Franc Ois G. Schmitt ; Lee-Shing Fang ; Shao-Hung Peng [République populaire de Chine] ; Cheng-Han Wu [République populaire de Chine] ; Shih-Hui Hsiao [République populaire de Chine] ; Wen-Hung Twan ; Tsui-Ping Wei [République populaire de Chine] ; Ram Kumar [République populaire de Chine] ; Tien-Hsi Fang ; Qing-Chao Chen [République populaire de Chine] ; C. Kim Wong [République populaire de Chine]

Source :

RBID : ISTEX:503997D527637E8D6F773770FB23987E133E3E86

Descripteurs français

English descriptors

Abstract

Danshuei River in the northwestern tip of Taiwan discharges into the boundary coastal waters between the East China Sea and the Taiwan Strait. We conducted a 5-year study between October 1998 and September 2003 to assess the influence of the northeast (NE) and the southwest (SW) monsoons on copepod assemblages in the area. A total of 110 copepod species were identified. Temora turbinata, Paracalanus aculeatus, Acrocalanus gibber, Parvocalanus crassirostris and Oithona rigida comprised 80% of the copepod assemblages that consisted of coastal species from the East China Sea and species associated with the Kuroshio Branch Current. The effect of the NE monsoon was observed during a short period of each winter when species such as Calanus sinicus were transported into the study area by the China Coastal Current. In summer, species such as A. gibber, Acrocalanus gracilis and Canthocalanus pauper may be transported into the study area from Southern Taiwan by the combined effect of the SW monsoon and the Kuroshio Current. Influence of the NE monsoon on the copepod assemblages in terms of introduction of species from the Yellow Sea and the East China Sea during winter was observed every year but was unlikely to represent an important carbon source into the region due to its short-term nature. Local species such as T. turbinata, P. crassirostris and O. rigida form a major component of the copepod assemblage. The high copepod diversity in the area was caused by the year-round presence of many local species and the aggregation of different species from subtropical, tropical, and temperate water masses. Monsoon-driven water currents and the Kuroshio Branch Current appeared to mask the effect of river discharge in the region.

Url:
DOI: 10.1093/plankt/fbl031


Affiliations:


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Le document en format XML

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<term>June</term>
<term>Kuroshio</term>
<term>Kuroshio branch</term>
<term>Longispinosa</term>
<term>Marine biology</term>
<term>Monsoon</term>
<term>Monsoon influence</term>
<term>National taiwan ocean university</term>
<term>Northern part</term>
<term>Northern taiwan</term>
<term>November</term>
<term>October</term>
<term>Oithona</term>
<term>Oncaea</term>
<term>Paracalanus</term>
<term>Parvocalanus crassirostris</term>
<term>Pauper</term>
<term>Plankton</term>
<term>Plankton research</term>
<term>Planktonic copepods</term>
<term>Present study</term>
<term>Relative abundance</term>
<term>Rigida</term>
<term>River discharge</term>
<term>Salinity</term>
<term>Sampling date</term>
<term>Sampling dates</term>
<term>Sampling period</term>
<term>Sampling stations</term>
<term>Seasonal variations</term>
<term>September</term>
<term>Shih</term>
<term>Sinicus</term>
<term>Southwestern taiwan</term>
<term>Spatial heterogeneity</term>
<term>Species composition</term>
<term>Species occurrence</term>
<term>Study area</term>
<term>Study period</term>
<term>Subcrassus</term>
<term>Surface waters</term>
<term>Taiwan</term>
<term>Taiwan strait</term>
<term>Temora</term>
<term>Temora turbinata</term>
<term>Temporal heterogeneity</term>
<term>Tseng</term>
<term>Turbinata</term>
<term>Vulgaris</term>
<term>Water circulation</term>
<term>Water currents</term>
<term>Water masses</term>
<term>Water temperature</term>
<term>Wong</term>
<term>Zhang</term>
<term>Zool</term>
<term>Zooplankton</term>
</keywords>
<keywords scheme="Wicri" type="geographic" xml:lang="fr">
<term>Taïwan</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr">
<term>Détroit</term>
<term>Estuaire</term>
<term>Milieu marin</term>
<term>Plancton</term>
</keywords>
</textClass>
<langUsage>
<language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front>
<div type="abstract" xml:lang="en">Danshuei River in the northwestern tip of Taiwan discharges into the boundary coastal waters between the East China Sea and the Taiwan Strait. We conducted a 5-year study between October 1998 and September 2003 to assess the influence of the northeast (NE) and the southwest (SW) monsoons on copepod assemblages in the area. A total of 110 copepod species were identified. Temora turbinata, Paracalanus aculeatus, Acrocalanus gibber, Parvocalanus crassirostris and Oithona rigida comprised 80% of the copepod assemblages that consisted of coastal species from the East China Sea and species associated with the Kuroshio Branch Current. The effect of the NE monsoon was observed during a short period of each winter when species such as Calanus sinicus were transported into the study area by the China Coastal Current. In summer, species such as A. gibber, Acrocalanus gracilis and Canthocalanus pauper may be transported into the study area from Southern Taiwan by the combined effect of the SW monsoon and the Kuroshio Current. Influence of the NE monsoon on the copepod assemblages in terms of introduction of species from the Yellow Sea and the East China Sea during winter was observed every year but was unlikely to represent an important carbon source into the region due to its short-term nature. Local species such as T. turbinata, P. crassirostris and O. rigida form a major component of the copepod assemblage. The high copepod diversity in the area was caused by the year-round presence of many local species and the aggregation of different species from subtropical, tropical, and temperate water masses. Monsoon-driven water currents and the Kuroshio Branch Current appeared to mask the effect of river discharge in the region.</div>
</front>
</TEI>
<affiliations>
<list>
<country>
<li>République populaire de Chine</li>
<li>Taïwan</li>
</country>
<region>
<li>Guangdong</li>
</region>
<settlement>
<li>Jiangmen</li>
<li>Sha Tin</li>
</settlement>
<orgName>
<li>Université chinoise de Hong Kong</li>
</orgName>
</list>
<tree>
<noCountry>
<name sortKey="Fang, Lee Shing" sort="Fang, Lee Shing" uniqKey="Fang L" first="Lee-Shing" last="Fang">Lee-Shing Fang</name>
<name sortKey="Fang, Tien Hsi" sort="Fang, Tien Hsi" uniqKey="Fang T" first="Tien-Hsi" last="Fang">Tien-Hsi Fang</name>
<name sortKey="Schmitt, Franc Ois G" sort="Schmitt, Franc Ois G" uniqKey="Schmitt F" first="Franc Ois G." last="Schmitt">Franc Ois G. Schmitt</name>
<name sortKey="Seuront, Laurent" sort="Seuront, Laurent" uniqKey="Seuront L" first="Laurent" last="Seuront">Laurent Seuront</name>
<name sortKey="Souissi, Sami" sort="Souissi, Sami" uniqKey="Souissi S" first="Sami" last="Souissi">Sami Souissi</name>
<name sortKey="Twan, Wen Hung" sort="Twan, Wen Hung" uniqKey="Twan W" first="Wen-Hung" last="Twan">Wen-Hung Twan</name>
</noCountry>
<country name="République populaire de Chine">
<noRegion>
<name sortKey="Hwang, Jiang Shiou" sort="Hwang, Jiang Shiou" uniqKey="Hwang J" first="Jiang-Shiou" last="Hwang">Jiang-Shiou Hwang</name>
</noRegion>
<name sortKey="Chen, Qing Chao" sort="Chen, Qing Chao" uniqKey="Chen Q" first="Qing-Chao" last="Chen">Qing-Chao Chen</name>
<name sortKey="Hsiao, Shih Hui" sort="Hsiao, Shih Hui" uniqKey="Hsiao S" first="Shih-Hui" last="Hsiao">Shih-Hui Hsiao</name>
<name sortKey="Kumar, Ram" sort="Kumar, Ram" uniqKey="Kumar R" first="Ram" last="Kumar">Ram Kumar</name>
<name sortKey="Peng, Shao Hung" sort="Peng, Shao Hung" uniqKey="Peng S" first="Shao-Hung" last="Peng">Shao-Hung Peng</name>
<name sortKey="Tseng, Li Chun" sort="Tseng, Li Chun" uniqKey="Tseng L" first="Li-Chun" last="Tseng">Li-Chun Tseng</name>
<name sortKey="Wei, Tsui Ping" sort="Wei, Tsui Ping" uniqKey="Wei T" first="Tsui-Ping" last="Wei">Tsui-Ping Wei</name>
<name sortKey="Wong, C Kim" sort="Wong, C Kim" uniqKey="Wong C" first="C. Kim" last="Wong">C. Kim Wong</name>
<name sortKey="Wu, Cheng Han" sort="Wu, Cheng Han" uniqKey="Wu C" first="Cheng-Han" last="Wu">Cheng-Han Wu</name>
</country>
<country name="Taïwan">
<noRegion>
<name sortKey="Hwang, Jiang Shiou" sort="Hwang, Jiang Shiou" uniqKey="Hwang J" first="Jiang-Shiou" last="Hwang">Jiang-Shiou Hwang</name>
</noRegion>
</country>
</tree>
</affiliations>
</record>

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