{"refrec":{"BRefID":32628,"RR":"<b>Cardinal, D.; Dehairs, F.; Cattaldo, T.; André, L.</b> (2001). Geochemistry of suspended particles in the Subantarctic and Polar Frontal Zones south of Australia: constraints on export and advection processes. <i>J. Geophys. Res. 106(C12)</i>: 31637-31656. <a href=\"https://dx.doi.org/10.1029/2000JC000251\" target=\"_blank\">https://dx.doi.org/10.1029/2000JC000251</a>","BEntID":32628,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Geophys. Res. 106(C12)</i>: 31637-31656. <a href=\"https://dx.doi.org/10.1029/2000JC000251\" target=\"_blank\">https://dx.doi.org/10.1029/2000JC000251</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Cardinal, D.; Dehairs, F.; Cattaldo, T.; André, L.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Cardinal, D. <i>et al.</i>","Englishabstract":"Filtered particles from a Southern Ocean meridional transect (from 42°S to 54°S along 142°E) off Tasmania were studied between surface and 600-m water depth (SAZ 1998 expedition, February-April 1998). Particulate Ba, Sr, Ca, P, U, Th, Ti, Al, Mn, light rare earth elements, and Zr contents were analyzed by inductively coupled plasma-mass spectrometry and inductively coupled plasma-atomic emission spectroscopy. Mesopelagic Ba<sub>xs</sub> (total Ba minus a lithogenic fraction estimated from Al) contents were higher within the Polar Front Zone (PFZ) in comparison with the northern areas, indicating that C export to the intermediate and deep ocean is more important in the PFZ. Average surface U<sub>xs</sub> versus latitude covaries with mesopelagic Ba<sub>xs</sub>, contrasting with organic matter proxies such as P<sub>p</sub> and chlorophyll <i>a</i>. This similar behavior suggests that U might be preferentially adsorbed on organic material, which subsequently becomes involved with barite precipitation. Sr<sub>p</sub> and Ca<sub>p</sub> contents decrease sharply with depth, following total particle content. For the northern area (42°-47°S), surface Ce anomaly reflects essentially a lithogenic signature (0.6 < Ce/Ce* < 1) ascribed to the supply from the Tasmanian continental shelf. Suspended matter from surface waters at stations south of 47°S shows an enhanced seawater signature (0.3 < Ce/Ce* < 0.6). In all stations, Ce anomalies increase with depth, toward values close to 1. This is likely due to the increase of lithogenic/authigenic ratio of particles with depth, rather than redox processes. Finally, an advective event is identified at 45°S below 200 m by a strong increase of lithogenic element contents, which affects Ba<sub>xs</sub>.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Geochemistry of suspended particles in the Subantarctic and Polar Frontal Zones south of Australia: constraints on export and advection processes","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2001,"MonPub":null,"DateUpdate":"2018-08-14","DateCreate":"2003-02-24","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000173402400049","VABBcode":null,"OpenAcc":0,"DOI":"10.1029/2000JC000251"},"refs":null,"anarec":{"AnaID":32628,"PubliDate":2001,"Pagination":"31637-31656","XtraPublOfAnaID":null,"ISBN":null,"Volume":"106","Issue":"C12","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":90908,"SerRR":"Journal of Geophysical Research. American Geophysical Union: Richmond.  ISSN 0148-0227; e-ISSN 2156-2202","StandardTitleSer":"Journal of Geophysical Research","ISSN":"0148-0227","AbbrevSer":"J. Geophys. 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