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  • Abaiang_Kiribati; Acid-base regulation; Aitutaki_Cook_New_Zeland; Alkalinity, total; Anakena_Isla_de_Pascua_Chile; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Calcification/Dissolution; Calcification rate; Calcifying fluid, aragonite saturation state; Calcifying fluid, carbonate ion; Calcifying fluid, dissolved inorganic carbon; Calcifying fluid, pH; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Clipperton_France; Cnidaria; Coast and continental shelf; Coiba_Panama; CSR_11_Wallis_France; Date/Time of event; Density; DEPTH, water; Diploastrea heliopora; E_Vangunu_Salomon; Event label; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Green_Island_Taiwan; Growth/Morphology; Guam_USA; Helen_Reef_Palau_1; Helen_Reef_Palau_2; Heron_S_GBR_Australia; Identification; Kimbe_Hoskins_District_PNG; Koror_Palau; LATITUDE; Linear extension; Location; LONGITUDE; Losuia_Tabungora_Island_PNG; Moorea_French_Polynesia_1; Moorea_French_Polynesia_2; Motu_Taka_Rua_Isla_de_Pascua_Chile; N_Hoskins_District_PNG; North_Palau; North Pacific; Noumea_Lagoon_New_Caledonia; NW_Fiji; OA-ICC; Ocean Acidification International Coordination Centre; Ogasawara_Japan; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Pisinun_Chuuk_Micronesia; Porites sp.; Potentiometric titration; S_Niue_New_Zeland; Salinity; Sample ID; Secas_islands_Panama; Sesoko_Okinawa_Japan; Single species; South Pacific; Species; SW_Cockatoo_Reef_GBR_Australia; Tekava_Gambier_French_Polynesia; Temperate; Temperature, water; Tropical; Type of study; Upolu_Samoa; W_Niue_New_Zeland; δ11B  (1)
  • foraminifera  (1)
Collection
Keywords
Years
  • 1
    Publication Date: 2022-05-27
    Description: Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography and Paleoclimatology, 36(4), (2021): e2020PA004153, https://doi.org/10.1029/2020PA004153.
    Description: Variations in Mediterranean thermohaline circulation of the Quaternary are still not well constrained whereas they have been considered to have an influence on the Atlantic Meridional Overturning Circulation and on the oxygenation of waters in the deep basins of the Mediterranean Sea. εNd analyses have been carried out on planktonic foraminifera of cores collected in the central Mediterranean Sea to constrain water mass exchange between the Eastern and Western Mediterranean Sea (EMS and WMS) during the last climatic cycle. εNd records from the WMS and EMS display similar higher values during warm substages of interglacial Marine Isotopic Stage (MIS) 1 and 5. This suggests an efficient connection between the two Mediterranean sub-basins and the transfer of radiogenic waters to the Tyrrhenian Sea via the Levantine Intermediate Water (LIW). Conversely, during glacial MIS, εNd of the intermediate depth of the Tyrrhenian Sea are less radiogenic than the EMS, implying limited hydrological connection between sub-basins during low sea-level stands. Superimposed on these glacial-interglacial variations, increased εNd occurred during Heinrich Stadial events. This suggests a reduction in the formation of unradiogenic WIW in the Gulf of Lions due to the input of relatively fresh surface Atlantic water to the WMS and/or the inflow of radiogenic glacial LIW and upper EMDW to the Tyrrhenian Sea as a result of an active EMS convection related to saltier and colder conditions. Such potential millennial-scale pulses of LIW intrusion into the Tyrrhenian Sea may have led to an enhanced Mediterranean Outflow Water intensity in the Gibraltar Strait.
    Description: The research leading to this paper was funded by the French National Research Agency under the “Investissements d'avenir” program (Grant ANR-11-IDEX-0004-17-EURE-0006), the MEDSENS Project (Grant ANR-19-CE01-0019) and the INSU LEFE-IMAGO PALMEDS Project. The authors gratefully acknowledge the support provided by Louise Bordier during Nd isotopic composition analyses.
    Description: 2021-08-15
    Keywords: Central Mediterranean Sea ; foraminifera ; last climatic cycle ; Neodymium isotopic composition ; paleo-hydrology ; sapropels
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-05-07
    Description: The Tara Pacifc expedition (2016–2018) provided an opportunity to investigate calcifcation patterns in extant corals throughout thePacifc Ocean. Cores from colonies of the massive Porites and Diploastrea genera were collected fromdiferent environments to assess calcifcation parameters of long-lived reef-building corals. In this study, we compared the calcifcation and carbonate chemistryup-regulation of Diploastrea heliopora and Porites corals from across a range of environments. To this, we analyzed the skeletal geochemistry and growth parameters of 39 colonies of Porites (n=33) and Diploastrea (n=6) collected across the tropical Pacifc Ocean during the Tara Pacifc expedition (2016–2018). Te collected corals represent a suite of cores exposed to various hydrological conditions of seawater temperature (SST: 22.4–29.8 °C), salinity (SSS: 31.5–36.1), and carbonate chemistry (total scale pHsw: 8.01–8.09). Te average chemical composition of the calcifying fuid (pHcf, [CO32−]cf, DICcf, Ωcf) was derived from paired boron isotope (δ11B) and B/Ca analyses of core-top samples corresponding to the last 6 years of growth (2010–2016). Based on these data, we assessed the impact of the ambient seawater properties (SST, salinity, carbonate chemistry) on the cf composition of these slow-growing reef-building genera at the Pacifc basin scale.
    Keywords: Abaiang_Kiribati; Acid-base regulation; Aitutaki_Cook_New_Zeland; Alkalinity, total; Anakena_Isla_de_Pascua_Chile; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Calcification/Dissolution; Calcification rate; Calcifying fluid, aragonite saturation state; Calcifying fluid, carbonate ion; Calcifying fluid, dissolved inorganic carbon; Calcifying fluid, pH; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Clipperton_France; Cnidaria; Coast and continental shelf; Coiba_Panama; CSR_11_Wallis_France; Date/Time of event; Density; DEPTH, water; Diploastrea heliopora; E_Vangunu_Salomon; Event label; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Green_Island_Taiwan; Growth/Morphology; Guam_USA; Helen_Reef_Palau_1; Helen_Reef_Palau_2; Heron_S_GBR_Australia; Identification; Kimbe_Hoskins_District_PNG; Koror_Palau; LATITUDE; Linear extension; Location; LONGITUDE; Losuia_Tabungora_Island_PNG; Moorea_French_Polynesia_1; Moorea_French_Polynesia_2; Motu_Taka_Rua_Isla_de_Pascua_Chile; N_Hoskins_District_PNG; North_Palau; North Pacific; Noumea_Lagoon_New_Caledonia; NW_Fiji; OA-ICC; Ocean Acidification International Coordination Centre; Ogasawara_Japan; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Pisinun_Chuuk_Micronesia; Porites sp.; Potentiometric titration; S_Niue_New_Zeland; Salinity; Sample ID; Secas_islands_Panama; Sesoko_Okinawa_Japan; Single species; South Pacific; Species; SW_Cockatoo_Reef_GBR_Australia; Tekava_Gambier_French_Polynesia; Temperate; Temperature, water; Tropical; Type of study; Upolu_Samoa; W_Niue_New_Zeland; δ11B
    Type: Dataset
    Format: text/tab-separated-values, 1532 data points
    Location Call Number Expected Availability
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