{"refrec":{"BRefID":339445,"RR":"<b>Guerreiro, C.V.; Baumann, K.-H.; Brummer, G.-J. A.; Valente, A.; Fischer, G.; Ziveri, P.; Brotas, V.; Stuut, J.-B</b> (2021). Carbonate fluxes by coccolithophore species between NW Africa and the Caribbean: implications for the biological carbon pump. <i>Limnol. Oceanogr. 66(8)</i>: 3190-3208. <a href=\"https://dx.doi.org/10.1002/lno.11872\" target=\"_blank\">https://dx.doi.org/10.1002/lno.11872</a>","BEntID":336080,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Limnol. Oceanogr. 66(8)</i>: 3190-3208. <a href=\"https://dx.doi.org/10.1002/lno.11872\" target=\"_blank\">https://dx.doi.org/10.1002/lno.11872</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Guerreiro, C.V.; Baumann, K.-H.; Brummer, G.-J. A.; Valente, A.; Fischer, G.; Ziveri, P.; Brotas, V.; Stuut, J.-B","OrigTitleTranslFlag":0,"Authorstringtrunc":"Guerreiro, C.V. <i>et al.</i>","Englishabstract":"<p>    Coccolithophores are among the most important calcifying pelagic organisms.    To assess how coccolithophore species with different coccolith-carbonate    mass and distinct ecological resilience to ocean warming will influence the    “rain ratio” and the “biological carbon pump”, 1 yr of species-specific    coccolith-carbonate export fluxes were quantified using sediment traps    moored at four sites between NW Africa and the Caribbean (i.e.,    CB-20°N/21°W, at 1214 m; M1-12°N/23°W, at 1150 m; M2-14°N/37°W, at 1235 m;    M4-12°N/49°W, at 1130 m). Highest coccolith-CaCO<sub>3</sub> fluxes at the    westernmost site M4, where the nutricline is deepest along the tropical    North Atlantic, were dominated by deep-dwelling small-sized coccolithspecies <em>Florisphaera profunda</em> and    <em>Gladiolithus flabellatus</em>. Total coccolith-CaCO<sub>3</sub> fluxesof 371 mg m<sup>−2</sup> yr<sup>−1</sup> at M4 were followed by 165 mg m<sup>−2</sup> yr<sup>−1</sup> at the north-easternmost CB, 130 mg m<sup>−2</sup> yr<sup>−1</sup> at M1, and 114 mg m<sup>−2</sup> yr    <sup>−1</sup> at M2 in between. Coccoliths accounted for nearly half of the    total carbonate flux at M4 (45%), much higher compared to 23% at M2 and 15%    at M1 and CB. At site M4, highest ratios of coccolith-CaCO<sub>3</sub> to    particulate organic carbon fluxes and weak correlations between the    carbonate of deep-dwelling species and particulate organic carbon suggest    that increasing productivity in the lower photic zone in response to ocean    warming might enhance the <em>rain ratio</em> and reduce the    coccolith-ballasting efficiency. The resulting weakened biological carbon    pump could, however, be counterbalanced by increasing frequency of Saharan    dust outbreaks across the tropical Atlantic, providing mineral ballast as    well as nutrients to fuel fast-blooming and ballast-efficient    coccolithophore species.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Carbonate fluxes by coccolithophore species between NW Africa and the Caribbean: implications for the biological carbon pump","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-21 01:33:01.504659","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2021-08-31","DateCreate":"2021-06-30","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000663846300001","VABBcode":null,"OpenAcc":1,"DOI":"10.1002/lno.11872"},"refs":null,"anarec":{"AnaID":339445,"PubliDate":2021,"Pagination":"3190-3208","XtraPublOfAnaID":null,"ISBN":null,"Volume":"66","Issue":"8","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43511,"SerRR":"Limnology and Oceanography. 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