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  • 6-TOW; 6-TOW-001GGC; 6-TOW-002GGC; 6-TOW-003GGC; 6-TOW-005GGC; 6-TOW-006GGC; 6-TOW-007GGC; 6-TOW-008GGC; 6-TOW-011GGC; 6-TOW-011PC; 6-TOW-012GGC; 6-TOW-013GGC; 6-TOW-014GGC; 6-TOW-015GGC; 6-TOW-016GGC; Akademik A. Vinogradov; AVI19-4; BC; Box corer; GGC; Giant gravity corer; Moana Wave; MW9109; MW9109-13BC; MW9109-16BC; MW9109-22BC; MW9109-33BC; MW9109-37BC; MW9109-3BC; MW9109-47BC; MW9109-53BC; MW9109-54BC; MW9109-58BC; MW9109-59BC; MW9109-63BC; MW9109-66BC; MW9109-70BC; MW9109-74BC; MW9109-7BC; Pacific; PC; Piston corer; RAMA; RAMA03WT; RAMA-44P; RNDB-11GGC; RNDB-11PC; RNDB-12GGC; RNDB-13GGC; RNDB-14GGC; RNDB-15GGC; RNDB-16GGC; RNDB-1GGC; RNDB-2GGC; RNDB-3GGC; RNDB-5GGC; RNDB-6GGC; RNDB-7GGC; RNDB-8GGC; Thomas Washington; Vi-26BC; Vi-35GC; Vi-37GC; VINO-26BC; VINO-35GGC; VINO-37GGC  (1)
  • Calcein
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: McCorkle, Daniel C; Keigwin, Lloyd D (1994): Depth profiles of d13C in bottom water and core top C. wuellerstorfi on the Ontong Java Plateau and Emperor Seamounts. Paleoceanography, 9(2), 197-208, https://doi.org/10.1029/93PA03271
    Publication Date: 2023-08-15
    Description: We have measured the carbon isotopic composition of dissolved inorganic carbon in bottom waters of the Ontong Java Plateau (western equatorial Pacific) and on the northern Emperor Seamounts (northwest Pacific). Each of these locations is several hundred miles from the nearest Geochemical Ocean Sections Study (GEOSECS) stations, and the observed delta13C values at each site differ substantially from regionally averaged GEOSECS delta13C profiles. We discuss the possible causes of these differences, including horizontal variability, near-bottom effects, and problems with the Pacific GEOSECS delta13C data. We also measured the isotopic composition (C and O) of core top C. wuellerstorfi from a depth transect of cores at each location. The delta18O data are used to verify that our samples are Holocene. Comparison of foraminiferal and bottom water delta13C values shows that this species faithfully records bottom water delta13C at both sites and demonstrates that there is no depth-related artifact in the dissolved inorganic carbon-C. wuellerstorfi delta13C relationship at these sites.
    Keywords: 6-TOW; 6-TOW-001GGC; 6-TOW-002GGC; 6-TOW-003GGC; 6-TOW-005GGC; 6-TOW-006GGC; 6-TOW-007GGC; 6-TOW-008GGC; 6-TOW-011GGC; 6-TOW-011PC; 6-TOW-012GGC; 6-TOW-013GGC; 6-TOW-014GGC; 6-TOW-015GGC; 6-TOW-016GGC; Akademik A. Vinogradov; AVI19-4; BC; Box corer; GGC; Giant gravity corer; Moana Wave; MW9109; MW9109-13BC; MW9109-16BC; MW9109-22BC; MW9109-33BC; MW9109-37BC; MW9109-3BC; MW9109-47BC; MW9109-53BC; MW9109-54BC; MW9109-58BC; MW9109-59BC; MW9109-63BC; MW9109-66BC; MW9109-70BC; MW9109-74BC; MW9109-7BC; Pacific; PC; Piston corer; RAMA; RAMA03WT; RAMA-44P; RNDB-11GGC; RNDB-11PC; RNDB-12GGC; RNDB-13GGC; RNDB-14GGC; RNDB-15GGC; RNDB-16GGC; RNDB-1GGC; RNDB-2GGC; RNDB-3GGC; RNDB-5GGC; RNDB-6GGC; RNDB-7GGC; RNDB-8GGC; Thomas Washington; Vi-26BC; Vi-35GC; Vi-37GC; VINO-26BC; VINO-35GGC; VINO-37GGC
    Type: Dataset
    Format: application/zip, 3 datasets
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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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