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Coastal upwelling circulation and its influence on the population dynamics of Calanus chilensis (Brodski, 1959) off northern Chile (23°S)
Marine pelagic copepods must cope with a highly heterogeneous environment in coastal upwelling systems. In addition to spatial and temporal heterogeneity in temperature and food supply, advective forces may strongly influence their populations. Off northern Chile, the population of Calanus chilensis...
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Published in: | Marine biology research 2009-05, Vol.5 (3), p.244-256 |
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description | Marine pelagic copepods must cope with a highly heterogeneous environment in coastal upwelling systems. In addition to spatial and temporal heterogeneity in temperature and food supply, advective forces may strongly influence their populations. Off northern Chile, the population of Calanus chilensis, a dominant copepod associated with upwelling centres, is subjected to large interannual variations in abundance, not explained by changing temperature regimes occurring upon cold and warm phases of the ENSO (El Niño Southern Oscillation) cycle. During two spring and two summer periods (1998-2000), we studied the abundance, distribution and growth of the copepodids of C. chilensis. The instantaneous mean weight-specific growth rate was estimated as 0.29 day
−1
and was not significantly different among cruises. Weights of late stages did not differ either. However, the numerical abundance and biomass substantially differed among cruises, such that daily production of copepodids increased with greater biomasses. Chlorophyll-a was significantly greater in spring 1999 and summer 2000, as compared to spring 1998 and summer 1999, coinciding with greater abundances of copepodids and stronger upwelling. The current field in the upper 200 m indicated that strong upwelling favoured nearshore water retention, whereas weak or moderate upwelling caused more offshore advection. This finding is opposite to the usual view that strong upwelling favours offshore advection. We further concluded that neither food or temperature had much influence on growth, abundance and production of C. chilensis, but instead seasonal and interannual variation in upwelling caused by changes in local winds may be the primary cause for the observed fluctuations in population abundance. |
doi_str_mv | 10.1080/17451000802425635 |
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−1
and was not significantly different among cruises. Weights of late stages did not differ either. However, the numerical abundance and biomass substantially differed among cruises, such that daily production of copepodids increased with greater biomasses. Chlorophyll-a was significantly greater in spring 1999 and summer 2000, as compared to spring 1998 and summer 1999, coinciding with greater abundances of copepodids and stronger upwelling. The current field in the upper 200 m indicated that strong upwelling favoured nearshore water retention, whereas weak or moderate upwelling caused more offshore advection. This finding is opposite to the usual view that strong upwelling favours offshore advection. We further concluded that neither food or temperature had much influence on growth, abundance and production of C. chilensis, but instead seasonal and interannual variation in upwelling caused by changes in local winds may be the primary cause for the observed fluctuations in population abundance.</description><identifier>ISSN: 1745-1000</identifier><identifier>EISSN: 1745-1019</identifier><identifier>DOI: 10.1080/17451000802425635</identifier><language>eng</language><publisher>Taylor & Francis Group</publisher><subject>23° 00' S ; 70 ° 30' W ; 70° 30′ W ; Antofagasta ; Calanus ; Calanus chilensis ; Chile ; coastal upwelling ; copepodid growth ; hoppekreps ; Humboldt current ; Marine</subject><ispartof>Marine biology research, 2009-05, Vol.5 (3), p.244-256</ispartof><rights>Copyright Taylor & Francis Group, LLC 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c411t-6630d173a7e5cf587f5c77d394dcd9716275af8ebdabf8f754df626745dead3c3</citedby><cites>FETCH-LOGICAL-c411t-6630d173a7e5cf587f5c77d394dcd9716275af8ebdabf8f754df626745dead3c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttps://doi.org/10.1080/17451000802425635$$dView source from Norart (may be restricted)$$Hfree_for_read</backlink></links><search><creatorcontrib>Giraldo, Alan</creatorcontrib><creatorcontrib>Escribano, Ruben</creatorcontrib><creatorcontrib>Marín, Victor</creatorcontrib><creatorcontrib>Hidalgo, Pamela</creatorcontrib><title>Coastal upwelling circulation and its influence on the population dynamics of Calanus chilensis (Brodski, 1959) off northern Chile (23°S)</title><title>Marine biology research</title><description>Marine pelagic copepods must cope with a highly heterogeneous environment in coastal upwelling systems. In addition to spatial and temporal heterogeneity in temperature and food supply, advective forces may strongly influence their populations. Off northern Chile, the population of Calanus chilensis, a dominant copepod associated with upwelling centres, is subjected to large interannual variations in abundance, not explained by changing temperature regimes occurring upon cold and warm phases of the ENSO (El Niño Southern Oscillation) cycle. During two spring and two summer periods (1998-2000), we studied the abundance, distribution and growth of the copepodids of C. chilensis. The instantaneous mean weight-specific growth rate was estimated as 0.29 day
−1
and was not significantly different among cruises. Weights of late stages did not differ either. However, the numerical abundance and biomass substantially differed among cruises, such that daily production of copepodids increased with greater biomasses. Chlorophyll-a was significantly greater in spring 1999 and summer 2000, as compared to spring 1998 and summer 1999, coinciding with greater abundances of copepodids and stronger upwelling. The current field in the upper 200 m indicated that strong upwelling favoured nearshore water retention, whereas weak or moderate upwelling caused more offshore advection. This finding is opposite to the usual view that strong upwelling favours offshore advection. We further concluded that neither food or temperature had much influence on growth, abundance and production of C. chilensis, but instead seasonal and interannual variation in upwelling caused by changes in local winds may be the primary cause for the observed fluctuations in population abundance.</description><subject>23° 00' S</subject><subject>70 ° 30' W</subject><subject>70° 30′ W</subject><subject>Antofagasta</subject><subject>Calanus</subject><subject>Calanus chilensis</subject><subject>Chile</subject><subject>coastal upwelling</subject><subject>copepodid growth</subject><subject>hoppekreps</subject><subject>Humboldt current</subject><subject>Marine</subject><issn>1745-1000</issn><issn>1745-1019</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNqFkM-KFDEQxhtRcF19AG85yQ44mko6nW7woo27Cgse1HOozR83mknaJM06r-DT-Aw-mRlGvSxooEhR_L4qvq_rHgN9BnSkz0H2AihtLeuZGLi4050cZlugMN3921N6v3tQymdK-QhSnnTf54SlYiDrcmND8PET0T7rNWD1KRKMhvhaiI8urDZqS9qwXluypOUPY_YRd14XkhyZMWBcC9HXPthYfCFnr3Iy5Yt_SmAS06ZBjsSU244cyXzAyBnjP3-83zzs7jkMxT76_Z92H89ff5jfbC_fXbydX15udQ9Qt8PAqQHJUVqhnRilE1pKw6feaDNJGJgU6EZ7ZfDKjU6K3riBDc2_sWi45qfdk-PeJaevqy1V7XzRzTxGm9aiGB3GQfK-gXAEdU6lZOvUkv0O814BVYfU1a3Um2Zz1DSPmKtq5XWwRU3tMRgmOcEIlDEKjX1xZFu6Ke_wJuVgVMV9SNlljNoXxf91Sv5Xfkul6rfKfwFKHKf9</recordid><startdate>200905</startdate><enddate>200905</enddate><creator>Giraldo, Alan</creator><creator>Escribano, Ruben</creator><creator>Marín, Victor</creator><creator>Hidalgo, Pamela</creator><general>Taylor & Francis Group</general><scope>3HL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7TN</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>200905</creationdate><title>Coastal upwelling circulation and its influence on the population dynamics of Calanus chilensis (Brodski, 1959) off northern Chile (23°S)</title><author>Giraldo, Alan ; Escribano, Ruben ; Marín, Victor ; Hidalgo, Pamela</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c411t-6630d173a7e5cf587f5c77d394dcd9716275af8ebdabf8f754df626745dead3c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>23° 00' S</topic><topic>70 ° 30' W</topic><topic>70° 30′ W</topic><topic>Antofagasta</topic><topic>Calanus</topic><topic>Calanus chilensis</topic><topic>Chile</topic><topic>coastal upwelling</topic><topic>copepodid growth</topic><topic>hoppekreps</topic><topic>Humboldt current</topic><topic>Marine</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Giraldo, Alan</creatorcontrib><creatorcontrib>Escribano, Ruben</creatorcontrib><creatorcontrib>Marín, Victor</creatorcontrib><creatorcontrib>Hidalgo, Pamela</creatorcontrib><collection>Norart - Norske tidsskriftartikler 1980-</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Marine biology research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Giraldo, Alan</au><au>Escribano, Ruben</au><au>Marín, Victor</au><au>Hidalgo, Pamela</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Coastal upwelling circulation and its influence on the population dynamics of Calanus chilensis (Brodski, 1959) off northern Chile (23°S)</atitle><jtitle>Marine biology research</jtitle><date>2009-05</date><risdate>2009</risdate><volume>5</volume><issue>3</issue><spage>244</spage><epage>256</epage><pages>244-256</pages><issn>1745-1000</issn><eissn>1745-1019</eissn><abstract>Marine pelagic copepods must cope with a highly heterogeneous environment in coastal upwelling systems. In addition to spatial and temporal heterogeneity in temperature and food supply, advective forces may strongly influence their populations. Off northern Chile, the population of Calanus chilensis, a dominant copepod associated with upwelling centres, is subjected to large interannual variations in abundance, not explained by changing temperature regimes occurring upon cold and warm phases of the ENSO (El Niño Southern Oscillation) cycle. During two spring and two summer periods (1998-2000), we studied the abundance, distribution and growth of the copepodids of C. chilensis. The instantaneous mean weight-specific growth rate was estimated as 0.29 day
−1
and was not significantly different among cruises. Weights of late stages did not differ either. However, the numerical abundance and biomass substantially differed among cruises, such that daily production of copepodids increased with greater biomasses. Chlorophyll-a was significantly greater in spring 1999 and summer 2000, as compared to spring 1998 and summer 1999, coinciding with greater abundances of copepodids and stronger upwelling. The current field in the upper 200 m indicated that strong upwelling favoured nearshore water retention, whereas weak or moderate upwelling caused more offshore advection. This finding is opposite to the usual view that strong upwelling favours offshore advection. We further concluded that neither food or temperature had much influence on growth, abundance and production of C. chilensis, but instead seasonal and interannual variation in upwelling caused by changes in local winds may be the primary cause for the observed fluctuations in population abundance.</abstract><pub>Taylor & Francis Group</pub><doi>10.1080/17451000802425635</doi><tpages>13</tpages></addata></record> |
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subjects | 23° 00' S 70 ° 30' W 70° 30′ W Antofagasta Calanus Calanus chilensis Chile coastal upwelling copepodid growth hoppekreps Humboldt current Marine |
title | Coastal upwelling circulation and its influence on the population dynamics of Calanus chilensis (Brodski, 1959) off northern Chile (23°S) |
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