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  • AGE; Age, error; Carter Seamount, East Equatorial Atlantic; CE0806; CE0806_Reykjanes_Ridge_CWC; Celtic Explorer; Comment; Coral biogeography; Dredge; DRG; ELEVATION; Event label; Holocene; James Cook; JC094; JC094_Carter_Seamount_CWC; JC094_Knipovich_Seamount_CWC; JC142; JC142_Tropic_Seamount_CWC; Knipovich Seamount, East Equatorial Atlantic; last deglaciation; Last glaciation; LATITUDE; Location; LONGITUDE; MarineE-tech; Northeast Atlantic; Remote operated vehicle; Reykjanes Ridge; ROV; Sample ID; Taxa; Thorium-230/Uranium-238 activity ratio; Thorium-230/Uranium-238 activity ratio, standard deviation; Thorium-232; Thorium-232, standard deviation; TROPICS; Tropic Seamount; Uranium-238; Uranium-238, standard deviation; U-Th dating; δ234 Uranium (0); δ234 Uranium (0), standard deviation; δ238 Uranium; δ238 Uranium, standard deviation  (1)
  • AGE; Age, uncertainty; Barium/Calcium ratio; Benthic foraminifera; circulation; cold-water corals; Comment; Depth, bathymetric; DH117; DH74; DH75; DR27; DR34; DR35; DR38; DR40; Drake Passage; Dredge; DRG; Elevation of event; Event label; Genus; Latitude of event; Longitude of event; Nathaniel B. Palmer; NBP0805; NBP0805-DR27; NBP0805-DR34; NBP0805-DR35; NBP0805-DR36; NBP0805-DR38; NBP0805-DR40; NBP0805-TB04; NBP1103; NBP1103-DH07; NBP1103-DH11; NBP1103-DH112; NBP1103-DH113; NBP1103-DH117; NBP1103-DH120; NBP1103-DH14; NBP1103-DH15; NBP1103-DH16; NBP1103-DH19; NBP1103-DH74; NBP1103-DH75; pH; productivity; Reference/source; Sample ID; Site; South Pacific Ocean; δ11B, carbonate  (1)
  • Geochemistry  (1)
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  • 1
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 31 (2016): 626–638, doi:10.1002/2015PA002908.
    Description: Coral skeletons archive past climate variability with unrivaled temporal resolution. However, extraction of accurate temperature information from coral skeletons has been limited by “vital effects,” which confound, and sometimes override, the temperature dependence of geochemical proxies. We present a new approach to coral paleothermometry based on results of abiogenic precipitation experiments interpreted within a framework provided by a quantitative model of the coral biomineralization process. DeCarlo et al. (2015a) investigated temperature and carbonate chemistry controls on abiogenic partitioning of Sr/Ca and U/Ca between aragonite and seawater and modeled the sensitivity of skeletal composition to processes occurring at the site of calcification. The model predicts that temperature can be accurately reconstructed from coral skeleton by combining Sr/Ca and U/Ca ratios into a new proxy, which we refer to hereafter as the Sr-U thermometer. Here we test the model predictions with measured Sr/Ca and U/Ca ratios of 14 Porites sp. corals collected from the tropical Pacific Ocean and the Red Sea, with a subset also analyzed using the boron isotope (δ11B) pH proxy. Observed relationships among Sr/Ca, U/Ca, and δ11B agree with model predictions, indicating that the model accounts for the key features of the coral biomineralization process. By calibrating to instrumental temperature records, we show that Sr-U captures 93% of mean annual temperature variability (26–30°C) and has a standard deviation of prediction of 0.5°C, compared to 1°C using Sr/Ca alone. The Sr-U thermometer may offer significantly improved reliability for reconstructing past ocean temperatures from coral skeletons.
    Description: NSF Grant Numbers: OCE-1338320, OCE-1031971, OCE-1220529; NSF Graduate Research Fellowships
    Description: 2016-12-11
    Keywords: Coral ; Paleoclimate ; Sea surface temperature ; Geochemistry ; Biomineralization
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-02-02
    Description: The Antarctic Cold Reversal (ACR; 14.7 to 13 ka) phase of the last deglaciation saw a pause in the rise of atmospheric pCO2 and Antarctic temperature, contrasted with warming in the North. Mechanisms associated with interhemispheric heat transfer have been proposed to explain features of this event, but the response of marine biota and the carbon cycle are debated. The Southern Ocean is a key site of deep-water exchange with the atmosphere, hence deglacial changes in nutrient cycling, circulation, and productivity in this region may have global impact. Here we present a new perspective on the sequence of events in the deglacial Southern Ocean, that includes multi-faunal benthic assemblage (foraminifera and cold-water corals) and geochemical data (Ba/Ca, 14C, δ11B) from the Drake Passage. Our records feature anomalies during peak ACR conditions indicative of circulation, biogeochemistry, and regional ecosystem perturbations. Within this cold episode, peak abundances of thick-walled benthic foraminifera and cold-water corals are observed at shallow depths in the sub-Antarctic (~300 m), while coral populations at greater depths and further south diminished. Geochemical data indicate that habitat shifts were associated with enhanced primary productivity in the sub-Antarctic, a more stratified water column, and poorly oxygenated bottom water. These results are consistent with northward migration of primary production in response to Antarctic cooling and widespread biotic turnover across the Southern Ocean. We suggest that expanding sea ice, suppressed ventilation, and shifting centres of upwelling drove changes in planktic and benthic ecology, and were collectively instrumental in halting CO2 rise in the mid-deglaciation.
    Keywords: AGE; Age, uncertainty; Barium/Calcium ratio; Benthic foraminifera; circulation; cold-water corals; Comment; Depth, bathymetric; DH117; DH74; DH75; DR27; DR34; DR35; DR38; DR40; Drake Passage; Dredge; DRG; Elevation of event; Event label; Genus; Latitude of event; Longitude of event; Nathaniel B. Palmer; NBP0805; NBP0805-DR27; NBP0805-DR34; NBP0805-DR35; NBP0805-DR36; NBP0805-DR38; NBP0805-DR40; NBP0805-TB04; NBP1103; NBP1103-DH07; NBP1103-DH11; NBP1103-DH112; NBP1103-DH113; NBP1103-DH117; NBP1103-DH120; NBP1103-DH14; NBP1103-DH15; NBP1103-DH16; NBP1103-DH19; NBP1103-DH74; NBP1103-DH75; pH; productivity; Reference/source; Sample ID; Site; South Pacific Ocean; δ11B, carbonate
    Type: Dataset
    Format: text/tab-separated-values, 1741 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-07-01
    Description: Uranium series dated cold-water corals from Tropic Seamount, Reykjanes Ridge, and East Equatorial Atlantic. Ages are reported in years before present (BP; where present is the year of 1950 CE) both uncorrected and corrected for initial 232Th. Some samples did not pass our quality control. Selection code column indicates samples not included on age distribution discussion: [238U] 〈2 ppm (Low U), [232Th] 〉6 ppb (High Th), [δ234Ui] 〉157‰ (High δU) and lowest quality sub-sample (duplicate).
    Keywords: AGE; Age, error; Carter Seamount, East Equatorial Atlantic; CE0806; CE0806_Reykjanes_Ridge_CWC; Celtic Explorer; Comment; Coral biogeography; Dredge; DRG; ELEVATION; Event label; Holocene; James Cook; JC094; JC094_Carter_Seamount_CWC; JC094_Knipovich_Seamount_CWC; JC142; JC142_Tropic_Seamount_CWC; Knipovich Seamount, East Equatorial Atlantic; last deglaciation; Last glaciation; LATITUDE; Location; LONGITUDE; MarineE-tech; Northeast Atlantic; Remote operated vehicle; Reykjanes Ridge; ROV; Sample ID; Taxa; Thorium-230/Uranium-238 activity ratio; Thorium-230/Uranium-238 activity ratio, standard deviation; Thorium-232; Thorium-232, standard deviation; TROPICS; Tropic Seamount; Uranium-238; Uranium-238, standard deviation; U-Th dating; δ234 Uranium (0); δ234 Uranium (0), standard deviation; δ238 Uranium; δ238 Uranium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 1752 data points
    Location Call Number Limitation Availability
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