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  • 1
    Publikationsdatum: 2022-05-25
    Beschreibung: © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Paleoceanography and Paleoclimatology 33 (2018): 443-456, doi:10.1029/2017PA003276.
    Beschreibung: Sr/Ca ratios recorded in the aragonite skeleton of massive coral colonies are commonly used to reconstruct seasonal‐ to centennial‐scale variability in sea surface temperature (SST). While the Sr/Ca paleothermometer is robust in individual colonies, Sr/Ca‐SST relationships between colonies vary, leading to questions regarding the utility of the proxy. We present biweekly‐resolution calibrations of Sr/Ca from five Porites spp. corals to satellite SST across 10° of latitude in the Red Sea to evaluate the Sr/Ca proxy across both spatial and temporal scales. SST is significantly correlated with coral Sr/Ca at each site, accounting for 69–84% of Sr/Ca variability (P ≪ 0.01). Intercolony variability in Sr/Ca‐SST sensitivities reveals a latitudinal trend, where calibration slopes become shallower with increasing mean annual temperature. Mean annual temperature is strongly correlated with the biweekly‐resolution calibration slopes across five Red Sea sites (r2 = 0.88, P = 0.05), while also correlating significantly to Sr/Ca‐SST slopes for 33 Porites corals from across the entire Indo‐Pacific region (r2 = 0.26, P 〈 0.01). Although interannual summer, winter, and mean annual calibrations for individual Red Sea colonies are inconsistently robust, combined multicoral calibrations are significant at summer (r2 = 0.53, P ≪ 0.01), winter (r2 = 0.62, P ≪ 0.01), and mean annual time scales (r2 = 0.79, P ≪ 0.01). Our multicoral, multisite study indicates that the Sr/Ca paleothermometer is accurate across both temporal and spatial scales in the Red Sea and also potentially explains for the first time variability in Sr/Ca‐SST calibration slopes across the Indo‐Pacific region. Our study provides strong evidence supporting the robustness of the coral Sr/Ca proxy for examining seasonal to multicentury variability in global climate phenomena.
    Beschreibung: Singapore Ministry of Education; National Research Foundation Singapore Grant Number: NRFF‐2012‐03; U.S. National Science Foundation Grant Number: OCE‐1031288; King Abdullah University of Science and Technology Grant Numbers: USA 00002, KSA 00011
    Schlagwort(e): Porites ; Sr/Ca ; Sea surface temperature ; Calibration ; Red Sea
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publikationsdatum: 2022-05-26
    Beschreibung: Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September 2013
    Beschreibung: Predicting the response of net community calcification (NCC) to ocean acidification (OA) and declining aragonite saturation state (Ωa) requires a thorough understanding of controls on NCC. The diurnal control of light and net community production (NCP) on NCC confounds the underlying control of Ωa on NCC and must be averaged out in order to predict the general response of NCC to OA. I did this by generating a general NCC-Ωa correlation based on data from 15 field and mesocosm studies around the globe. The general relationship agrees well with results from mesocosm experiments. This general relationship implies that NCC will transition from net calcification to net dissolution at a Ωa of 1.0 ± 0.6 and predicts that NCC will decline by 50% from 1880 to 2100, for a reef of any percent calcifier cover and short reef water residence time. NCC will also decline if percent calcifier cover declines, as evidenced by estimates of NCC in two Caribbean reefs having declined by an estimated 50-90% since 1880. The general NCC-Ωa relationship determined here, along with changes in percent calcifier cover, will be useful in predicting changes in NCC in response to OA and for refining models of reef water Ωa.
    Beschreibung: This research was supported by WHOI Coastal Ocean Institute Student Research Award, MIT EAPS Student Research Award, WHOI Academic Program Office Ocean Ventures Fund, MIT Student Assistance Fund and MIT Houghton Fund. Additional research funds were provided by OCE1031288, WHOI Access to the Sea 27500040 and WHOI Access to the Sea-Special Call 25110104 to K.A.Hughen; NSF OCE0628406 and NOAA's Coral Reef Conservation Program Atlantic Ocean Acidification Test Bed project funding to C. Langdon; King Abdullah University of Science and Technology USA 00002 and KSA 00011 to S.J. Lentz; and King Abdullah University of Science and Technology to D. McCorkle. I was supported throughout this graduate program by the NSF Graduate Research Fellowship Program, WHOI Ocean Life Insitute, WHOI Academic Program Office funds, and NSF-DUE-1043405 (PI James Yoder).
    Schlagwort(e): Ocean acidification ; Chemical oceanography
    Repository-Name: Woods Hole Open Access Server
    Materialart: Thesis
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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