Immigration and emigration of a pelagic fish assemblage to seamounts in the Gulf of California related to water mass movements using satellite imagery
The appearance of an assemblage of 11 planktivorous and predatory fishes at El Bajo Gorda seamount within the Gulf of California in May 1981 coincided with an increase in surface water temperature and chlorophyll concentration. The assemblage may have either concentrated at the seamount from the sur...
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Veröffentlicht in: | Marine ecology. Progress series (Halstenbek) 1988-01, Vol.49 (1/2), p.11-20 |
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creator | Klimley, A. P. Butler, S. B. |
description | The appearance of an assemblage of 11 planktivorous and predatory fishes at El Bajo Gorda seamount within the Gulf of California in May 1981 coincided with an increase in surface water temperature and chlorophyll concentration. The assemblage may have either concentrated at the seamount from the surrounding pelagic environment or immigrated from south of the Gulf of California. At this time the fall to early spring current flow southeastward toward the Gulf of Tehuantepec reverses to the spring to summer flow northeastward along the mainland into the Gulf to California. One assemblage member, the scalloped hammerhead shark Sphyrna lewini, was monitored as an indicator of assemblage movements in response to water mass changes. The occurrences of 18 individuals tagged with individually recognizable transmitters were recorded over a 10 d period in July and August 1981 by 2 microprocessor monitors deployed at El Bajo Espiritu Santo seamount. Shark returns diminished as a mass of upwelled cold water, originating in the Bay of La Paz, moved over that seamount. The return rate then increased on a single day coincident with the incursion of a warm water mass before the rate decreased as this water mass cooled. |
doi_str_mv | 10.3354/meps049011 |
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The occurrences of 18 individuals tagged with individually recognizable transmitters were recorded over a 10 d period in July and August 1981 by 2 microprocessor monitors deployed at El Bajo Espiritu Santo seamount. Shark returns diminished as a mass of upwelled cold water, originating in the Bay of La Paz, moved over that seamount. The return rate then increased on a single day coincident with the incursion of a warm water mass before the rate decreased as this water mass cooled.</description><identifier>ISSN: 0171-8630</identifier><identifier>EISSN: 1616-1599</identifier><identifier>DOI: 10.3354/meps049011</identifier><language>eng</language><publisher>Inter-Research</publisher><subject>Advanced very high resolution radiometers ; Chlorophylls ; Gulfs ; Marine ; Pigments ; Pisces ; Pixels ; Sea surface temperature ; Sea water ; Seamounts ; Sharks ; Sphyrna lewini ; Upwelling water</subject><ispartof>Marine ecology. 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B.</creatorcontrib><title>Immigration and emigration of a pelagic fish assemblage to seamounts in the Gulf of California related to water mass movements using satellite imagery</title><title>Marine ecology. Progress series (Halstenbek)</title><description>The appearance of an assemblage of 11 planktivorous and predatory fishes at El Bajo Gorda seamount within the Gulf of California in May 1981 coincided with an increase in surface water temperature and chlorophyll concentration. The assemblage may have either concentrated at the seamount from the surrounding pelagic environment or immigrated from south of the Gulf of California. At this time the fall to early spring current flow southeastward toward the Gulf of Tehuantepec reverses to the spring to summer flow northeastward along the mainland into the Gulf to California. One assemblage member, the scalloped hammerhead shark Sphyrna lewini, was monitored as an indicator of assemblage movements in response to water mass changes. The occurrences of 18 individuals tagged with individually recognizable transmitters were recorded over a 10 d period in July and August 1981 by 2 microprocessor monitors deployed at El Bajo Espiritu Santo seamount. Shark returns diminished as a mass of upwelled cold water, originating in the Bay of La Paz, moved over that seamount. The return rate then increased on a single day coincident with the incursion of a warm water mass before the rate decreased as this water mass cooled.</description><subject>Advanced very high resolution radiometers</subject><subject>Chlorophylls</subject><subject>Gulfs</subject><subject>Marine</subject><subject>Pigments</subject><subject>Pisces</subject><subject>Pixels</subject><subject>Sea surface temperature</subject><subject>Sea water</subject><subject>Seamounts</subject><subject>Sharks</subject><subject>Sphyrna lewini</subject><subject>Upwelling water</subject><issn>0171-8630</issn><issn>1616-1599</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1988</creationdate><recordtype>article</recordtype><recordid>eNqNkU1r3DAQhkVoIdu0l9wDOvVQcKuxvuxjWJo0EOglORutPd7VYlkbjZyQP9LfGy1bmmtPM6N53hfNDGOXIL5LqdWPgAcSqhUAZ2wFBkwFum0_sJUAC1VjpDhnn4j2QoBR1qzYn7sQ_Da57OPM3TxwfC_jyB0_4OS2vuejpx13RBg25QF5jpzQhbjMmbifed4hv12m8ahau8mPMc3e8VTkGYcj_lKSxEPx4CE-Y8CjciE_bzmV1jT5jNyHYp5eP7OPo5sIv_yNF-zx5ufD-ld1__v2bn19X_V1A7ky4LRF3cjWaWMN1qavAcQgQCmrR2slWByEkINUpoV646xzzWA2qlcgN0JesK8n30OKTwtS7oKnvvzFzRgX6kDXZWm2_Q8QdNPouoDfTmCfIlHCsTukMlR67UB0xxt17zcq8NUJ3lOO6R9Zq6a2FrR8A8OykD4</recordid><startdate>19880101</startdate><enddate>19880101</enddate><creator>Klimley, A. 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B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c281t-61a57e5839a5676e26c2110d014475f77317ed003d346912ba7aa8d6b4c413b03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1988</creationdate><topic>Advanced very high resolution radiometers</topic><topic>Chlorophylls</topic><topic>Gulfs</topic><topic>Marine</topic><topic>Pigments</topic><topic>Pisces</topic><topic>Pixels</topic><topic>Sea surface temperature</topic><topic>Sea water</topic><topic>Seamounts</topic><topic>Sharks</topic><topic>Sphyrna lewini</topic><topic>Upwelling water</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Klimley, A. P.</creatorcontrib><creatorcontrib>Butler, S. B.</creatorcontrib><collection>CrossRef</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) Professional</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Marine ecology. Progress series (Halstenbek)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Klimley, A. P.</au><au>Butler, S. B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Immigration and emigration of a pelagic fish assemblage to seamounts in the Gulf of California related to water mass movements using satellite imagery</atitle><jtitle>Marine ecology. Progress series (Halstenbek)</jtitle><date>1988-01-01</date><risdate>1988</risdate><volume>49</volume><issue>1/2</issue><spage>11</spage><epage>20</epage><pages>11-20</pages><issn>0171-8630</issn><eissn>1616-1599</eissn><abstract>The appearance of an assemblage of 11 planktivorous and predatory fishes at El Bajo Gorda seamount within the Gulf of California in May 1981 coincided with an increase in surface water temperature and chlorophyll concentration. The assemblage may have either concentrated at the seamount from the surrounding pelagic environment or immigrated from south of the Gulf of California. At this time the fall to early spring current flow southeastward toward the Gulf of Tehuantepec reverses to the spring to summer flow northeastward along the mainland into the Gulf to California. One assemblage member, the scalloped hammerhead shark Sphyrna lewini, was monitored as an indicator of assemblage movements in response to water mass changes. The occurrences of 18 individuals tagged with individually recognizable transmitters were recorded over a 10 d period in July and August 1981 by 2 microprocessor monitors deployed at El Bajo Espiritu Santo seamount. Shark returns diminished as a mass of upwelled cold water, originating in the Bay of La Paz, moved over that seamount. The return rate then increased on a single day coincident with the incursion of a warm water mass before the rate decreased as this water mass cooled.</abstract><pub>Inter-Research</pub><doi>10.3354/meps049011</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record> |
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ispartof | Marine ecology. Progress series (Halstenbek), 1988-01, Vol.49 (1/2), p.11-20 |
issn | 0171-8630 1616-1599 |
language | eng |
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source | Inter-Research; JSTOR Archive Collection A-Z Listing; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection |
subjects | Advanced very high resolution radiometers Chlorophylls Gulfs Marine Pigments Pisces Pixels Sea surface temperature Sea water Seamounts Sharks Sphyrna lewini Upwelling water |
title | Immigration and emigration of a pelagic fish assemblage to seamounts in the Gulf of California related to water mass movements using satellite imagery |
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