{"refrec":{"BRefID":222590,"RR":"<b>Verheye, H.M.</b> (1991). Short-term variability during an anchor station study in the southern Benguela upwelling system: abundance, distribution and estimated production of mesozooplankton with special reference to <i>Calanoides carinatus</i> (Krøyer, 1849). <i>Prog. Oceanogr. 28(1-2)</i>: 91-119. <a href=\"http://dx.doi.org/10.1016/0079-6611(91)90022-E\" target=\"_blank\">http://dx.doi.org/10.1016/0079-6611(91)90022-E</a>","BEntID":214315,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Prog. Oceanogr. 28(1-2)</i>: 91-119. <a href=\"http://dx.doi.org/10.1016/0079-6611(91)90022-E\" target=\"_blank\">http://dx.doi.org/10.1016/0079-6611(91)90022-E</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Verheye, H.M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Verheye, H.M.","Englishabstract":"Daytime zooplankton samples collected at a fixed station position in St Helena Bay during a 27-day time series in March–April 1987 were used to describe the variability in the vertical distribution, abundance and population age structure of <em>Calanoides carinatus</em> in response to upwelling-related processes, and to provide an estimate of their production.</p><p id=\"\">The vertical distribution of <em>C. carinatus</em> was characterized by ontogenetic layering of copepodites and adults. The thermocline delimited the maximum depth of young copepodites (CI–CIII). Older stages avoided low-oxygen (<1ml O<sub>2</sub>l<sup>-1</sup>) bottom water. <em>C. carinatus</em> was usually not associated with the chlorophyll <em>a</em> maximum. The spatial segregation of young and older stages is briefly discussed in relation to differential feeding habits and diel vertical migration behaviour.</p><p id=\"\">The demographic structure of the <em>C. carinatus</em> population showed evidence of a stable age distribution of copepodites and adults during the first of two upwelling cycles observed during the study. Overall mean abundance was 360 animals m<sup>-3</sup>. However, during the second upwelling cycle their mean abundance was reduced to 183 animals m<sup>-3</sup> and adults dominated the population by 54%. These changes in abundance and age structure are discussed in relation to upwelling-induced advective processes. Surface-dwelling young copepodites (CI–CIII) are thought to be transported away from the study site, while re-seeding of the reduced nearshore population probably took place through advection of diapausal pre-adults (CV) in the upwelled water.</p><p id=\"\">Daily production of juvenile <em>C. carinatus</em> was estimated at 0.7 mg C m<sup>-3</sup>d<sup>-1</sup> which, combined with an egg production of 1.0mg C m<sup>-3</sup>d<sup>-1</sup> by addult females, is equivalent to 2% of the observed daily primary production. The mean P:B ratio for the copepodite stages was 0.167d<sup>-1</sup>. The role of this dominant copepod and the mesozooplankton in the carbon budget in St Helena Bay is discussed. Consumption by mesozooplankters was estimated at 22% of the daily primary production indicating that there was a considerable imbalance between primary producers and production by these heterotrophs.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Short-term variability during an anchor station study in the southern Benguela upwelling system: abundance, distribution and estimated production of mesozooplankton with special reference to <i>Calanoides carinatus</i> (Krøyer, 1849)","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-05-08 01:32:34.695881","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1991,"MonPub":null,"DateUpdate":"2013-05-10","DateCreate":"2013-02-05","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:A1991GR39600005","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/0079-6611(91)90022-E"},"refs":null,"anarec":{"AnaID":222590,"PubliDate":1991,"Pagination":"91-119","XtraPublOfAnaID":null,"ISBN":null,"Volume":"28","Issue":"1-2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43700,"SerRR":"Progress in Oceanography. 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