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  • 09070100; ANTARES-I_KBE3; ANTARES-I_KTB11; ANTARES-I_KTB13; ANTARES-I_KTB16; ANTARES-I_KTB19; ANTARES-I_KTB21; ANTARES-I_KTB5; ANTARES-I_KTB6; ANTARES-I,35MF75_1; Carbon/Nitrogen ratio; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Latitude of event; Longitude of event; Marion Dufresne (1972); MD75; MUC; MultiCorer; Nathaniel B. Palmer; NBP9604; NBP9604-02-2; Southern Ocean  (1)
  • Calcein
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  • 1
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    PANGAEA
    In:  Supplement to: Sigman, Daniel M; Altabet, Mark A; Francois, Roger; McCorkle, Daniel C; Gaillard, Jean-Francois (1999): The isotopic composition of diatom-bound nitrogen in Southern Ocean sediments. Paleoceanography, 14(2), 118-134, https://doi.org/10.1029/1998PA900018
    Publication Date: 2023-12-12
    Description: Treatment of diatom microfossils from Southern Ocean sediments with hot perchloric acid leaves a "diatom-bound" N fraction which is 0-4 per mil lower in d15N than the bulk sediment, typically 3 per mil lower in recent Antarctic diatom ooze. Results from Southern Ocean surface sediments indicate that early diagenetic changes in bulk sediment N content and d15N are not reflected in diatom-bound N, suggesting that diatom-bound N is physically protected from early diagenesis by the microfossil matrix. A meridional transect of multicores from the Indian sector of the Southern Ocean shows a northward increase in the d15N of diatom-bound N, suggesting that diatom-bound d15N, like bulk sedimentary d15N, varies with nitrate utilization in the overlying surface waters. The d15N of diatom-bound N is 3-4 per mil higher in glacial age Antarctic sediments than in Holocene sediments, supporting the hypothesis, previously based on bulk sediment d15N, that nitrate utilization in the surface Antarctic was higher during the last ice age. While there are important uncertainties, the inferred range of utilization changes could potentially explain the entire ~80 ppm amplitude of observed glacial/interglacial variations in atmospheric CO2.
    Keywords: 09070100; ANTARES-I_KBE3; ANTARES-I_KTB11; ANTARES-I_KTB13; ANTARES-I_KTB16; ANTARES-I_KTB19; ANTARES-I_KTB21; ANTARES-I_KTB5; ANTARES-I_KTB6; ANTARES-I,35MF75_1; Carbon/Nitrogen ratio; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Latitude of event; Longitude of event; Marion Dufresne (1972); MD75; MUC; MultiCorer; Nathaniel B. Palmer; NBP9604; NBP9604-02-2; Southern Ocean
    Type: Dataset
    Format: text/tab-separated-values, 27 data points
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2012. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of Experimental Marine Biology and Ecology 440 (2013): 126-131, doi:10.1016/j.jembe.2012.12.003.
    Description: In situ skeletal markers have been widely used to quantify skeletal growth rates of scleractinian corals on sub-annual time-scales. Nevertheless, an evaluation of different techniques, both in terms of their efficacy and potential impacts on the growth process itself, has not been undertaken. Here the effects of exposure to four different dyes (alizarin, alizarin complexone, calcein, oxytetracycline) and isotope spikes (Ba and Sr) on the growth rates of scleractinian corals are compared. Oxytetracycline increased coral growth. Alizarin, alizarin complexone, calcein, and Sr and Ba isotope spikes had no significant effect on coral growth, but polyp extension appeared reduced during exposure to alizarin and alizarin complexone. Calcein provided a more intense fluorescent mark than either alizarin or alizarin complexone. Isotope spikes were challenging to locate using isotope ratio analysis techniques. Thus, calcein appears best suited for marking short-term calcification increments in corals, while a combination of alizarin or alizarin complexone and calcein may be useful for dual labeling experiments as there is little overlap in their fluorescence spectra.
    Description: Funding for this work was provided by a Lizard Island Doctoral Fellowship, the Ocean Life Institute, NSF OCE-1041106, and an International Society for Reef Studies / Ocean Conservancy Fellowship. This material is based upon work supported under a National Science Foundation Graduate Research Fellowship and a National Science Foundation International Post-Doctoral Fellowship.
    Keywords: Alizarin ; Calcein ; Isotope ; Coral ; Calcification ; Stain
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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