{"refrec":{"BRefID":333482,"RR":"<b>Luostarinen, T.; Ribeiro, S.; Weckström, K.; Sejr, M.K.; Meire, L.; Tallberg, P.; Heikkila, M.</b> (2020). An annual cycle of diatom succession in two contrasting Greenlandic fjords: from simple sea-ice indicators to varied seasonal strategists. <i>Mar. Micropaleontol. 158</i>: 101873. <a href=\"https://doi.org/10.1016/j.marmicro.2020.101873\" target=\"_blank\">https://doi.org/10.1016/j.marmicro.2020.101873</a>","BEntID":327094,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Mar. Micropaleontol. 158</i>: 101873. <a href=\"https://doi.org/10.1016/j.marmicro.2020.101873\" target=\"_blank\">https://doi.org/10.1016/j.marmicro.2020.101873</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Luostarinen, T.; Ribeiro, S.; Weckström, K.; Sejr, M.K.; Meire, L.; Tallberg, P.; Heikkila, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Luostarinen, T. <i>et al.</i>","Englishabstract":"We recorded diatom species succession over one full year (May 2017–May    2018) using automated sediment traps installed in two contrasting    Greenlandic fjords: the seasonally ice-covered Young Sound in high-arctic    Northeast Greenland and the nearly sea-ice free Godthåbsfjord in subarctic    Southwest Greenland. The traps were positioned at differing water depths    (37 m in Young Sound vs. 300 m in Godthåbsfjord). Distinct differences    between the study sites were observed in both sediment and diatom fluxes.    In Young Sound, total diatom flux was extremely seasonal and as high as    880 × 10<sup>6</sup> valves m<sup>−2</sup> d<sup>−1</sup> in the spring. In    Godthåbsfjord, total diatom flux was more stable throughout the year, with    a maximum of 320 × 10<sup>6</sup> valves m<sup>−2</sup> d<sup>−1</sup> in    the summer. The diatom assemblage in Young Sound was dominated by thesea-ice species <i>Fragilariopsis oceanica</i>,    <i>Fragilariopsis reginae-jahniae</i> and <i>Fossula arctica</i>, which    exhibited pulse-like deposition in the trap during and after the ice melt.    In Godthåbsfjord, the fluxes were dominated by <i>Chaetoceros</i> (resting    spores), while the remaining assemblage was characterised by the cold-waterindicator species <i>Detonula confervacea</i> (resting spores) and    <i>Thalassiosira antarctica</i> var. <i>borealis</i> (resting spores)together with <i>Fragilariopsis cylindrus</i>. Our data show that,    <i>F. oceanica</i>, <i>F. reginae-jahniae</i> and <i>F. arctica</i> exhibitsimilar seasonal behaviour and a clear link to sea ice.    <i>Fragilariopsis cylindrus</i> seems to have a more flexible niche, and    based on our study, cannot be considered an unequivocal ice indicator.    Taking into account these ecological and seasonal preferences of individual    diatom species is crucial when reconstructing past sea-ice conditions both    qualitatively and quantitatively.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"An annual cycle of diatom succession in two contrasting Greenlandic fjords: from simple sea-ice indicators to varied seasonal strategists","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-18 01:32:21.162196","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Diatom; Seasonal; Sea ice; Sediment trap; Arctic; Palaeoceanography; Fjord; Northeast Greenland; Southwest Greenland; Godthåbsfjord; Young Sound","OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2023-02-21","DateCreate":"2021-02-03","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000551341800007","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.marmicro.2020.101873"},"refs":null,"anarec":{"AnaID":333482,"PubliDate":2020,"Pagination":"101873","XtraPublOfAnaID":null,"ISBN":null,"Volume":"158","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43516,"SerRR":"Marine Micropaleontology. 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