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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] During the Younger Dryas event, about 12,000 years ago, the Northern Hemisphere cooled by between 2 and 10 °C (refs 1, 2) whereas East Antarctica experienced warming. But the spatial signature of the event in the southern mid-latitudes and tropics is less well ...
    Type of Medium: Electronic Resource
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  • 2
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    PANGAEA
    In:  Supplement to: Corrège, Thierry; Delcroix, Thierry; Recy, Jacques; Beck, Warren; Cabioch, Guy; Le Cornec, Florence (2000): Evidence for stronger El Niño-Southern Oscillation (ENSO) Events in a Mid-Holocene massive coral. Paleoceanography, 15(4), 465-470, https://doi.org/10.1029/1999PA000409
    Publication Date: 2023-05-12
    Description: We present a 47-year-long record of sea surface temperature (SST) derived from Sr/Ca and U/Ca analysis of a massive Porites coral which grew at ~4150 calendar years before present (B.P.) in Vanuatu (southwest tropical Pacific Ocean). Mean SST is similar in both the modern instrumental record and paleorecord, and both exhibit El Niño-Southern Oscillation (ENSO) frequency SST oscillations. However, several strong decadal-frequency cooling events and a marked modulation of the seasonal SST cycle, with power at both ENSO and decadal frequencies, are observed in the paleorecord, which are unprecedented in the modern record.
    Keywords: CDRILL; Core drilling; Drill9A_Tasmaloum
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-05-12
    Keywords: CDRILL; Core drilling; Drill9A_Tasmaloum; ORDINAL NUMBER; Strontium/Calcium ratio; Uranium/Calcium ratio
    Type: Dataset
    Format: text/tab-separated-values, 917 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-05-12
    Keywords: Calculated; CDRILL; Core drilling; Drill9A_Tasmaloum; ORDINAL NUMBER; Sea surface temperature, annual mean
    Type: Dataset
    Format: text/tab-separated-values, 568 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Wu, Henry C; Dissard, Delphine; Douville, Eric; Blamart, Dominique; Bordier, Louise; Tribollet, Aline; Le Cornec, Florence; Pons-Branchu, Edwige; Dapoigny, Arnaud; Lazareth, Claire E (2018): Surface ocean pH variations since 1689 CE and recent ocean acidification in the tropical South Pacific. Nature Communications, 9(1), 2543, https://doi.org/10.1038/s41467-018-04922-1
    Publication Date: 2024-02-21
    Description: Increasing atmospheric CO2 from man-made climate change is reducing surface ocean pH. Due to limited instrumental measurements and historical pH records in the world's oceans, seawater pH variability at the decadal and centennial scale remains largely unknown and requires documentation. Here we present evidence of striking secular trends of decreasing pH since the late nineteenth century with pronounced interannual to decadal–interdecadal pH variability in the South Pacific Ocean from 1689 to 2011 CE. High-amplitude oceanic pH changes, likely related to atmospheric CO2 uptake and seawater dissolved inorganic carbon fluctuations, reveal a coupled relationship to sea surface temperature variations and highlight the marked influence of El Niño/Southern Oscillation and Interdecadal Pacific Oscillation. We suggest changing surface winds strength and zonal advection processes as the main drivers responsible for regional pH variability up to 1881 CE, followed by the prominent role of anthropogenic CO2 in accelerating the process of ocean acidification.
    Keywords: Age; AGE; Diploastrea heliopora, δ11B; Diploastrea heliopora, δ11B, standard deviation; Diploastrea heliopora, δ13C; Diploastrea heliopora, δ18O; New_Caledonia
    Type: Dataset
    Format: text/tab-separated-values, 1598 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Wu, Henry C; Dissard, Delphine; Le Cornec, Florence; Thil, François; Tribollet, Aline; Moya, Aurélie; Douville, Eric (2017): Primary Life Stage Boron Isotope and Trace Elements Incorporation in Aposymbiotic Acropora millepora Coral under Ocean Acidification and Warming. Frontiers in Marine Science, 4, https://doi.org/10.3389/fmars.2017.00129
    Publication Date: 2024-03-15
    Description: Early-life stages of reef-building corals are vital to coral existence and reef maintenance. It is therefore crucial to study juvenile coral response to future climate change pressures. Moreover, corals are known to be reliable recorders of environmental conditions in their skeletal materials. Aposymbiotic Acropora millepora larvae were cultured in different seawater temperature (27 and 29ºC) and pCO2 (390 and 750 µatm) conditions to understand the impacts of 'end of century' ocean acidification (OA) and ocean warming (OW) conditions on skeletal morphology and geochemistry. The experimental conditions impacted primary polyp juvenile coral skeletal morphology and growth resulting in asymmetric translucent appearances with brittle skeleton features. The impact of OA resulted in microstructure differences with decreased precipitation or lengthening of fasciculi and disorganized aragonite crystals that led to more concentrations of centers of calcifications. The coral skeletal delta 11B composition measured by laser ablation MC-ICP-MS was significantly affected by pCO2 (p = 0.0024) and water temperature (p = 1.46 x 10-5). Reconstructed pH of the primary polyp skeleton using the ?11B proxy suggests a difference in coral calcification site and seawater pH consistent with previously observed coral pH up-regulation. Similarly, trace element results measured by laser ablation ICP-MS indicate the impact of pCO2. Primary polyp juvenile Sr/Ca ratio indicates a bias in reconstructed sea surface temperature (SST) under higher pCO2 conditions. Coral microstructure content changes (center of calcification and fasciculi) due to OA possibly contributed to the variability in B/Ca ratios. Our results imply that increasing OA and OW may lead to coral acclimation issues and species-specific inaccuracies of the commonly used Sr/Ca-SST proxy.
    Keywords: Acropora millepora; Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthic animals; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Boron/Calcium ratio, standard deviation; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Cnidaria; Coast and continental shelf; Containers and aquaria (20-1000 L or 〈 1 m**2); Experiment duration; Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laboratory experiment; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Registration number of species; Salinity; Single species; South Pacific; Species; Strontium/Calcium ratio; Strontium/Calcium ratio, standard deviation; Table; Temperature; Temperature, water; Temperature, water, standard deviation; Treatment; Tropical; Type; Uniform resource locator/link to reference; Uranium/Calcium ratio; Uranium/Calcium ratio, standard deviation; δ11B; δ11B, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 9334 data points
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  • 7
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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