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  • 2010-2014  (11)
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  • 1
    Publication Date: 2015-10-21
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry, Geophysics, Geosystems 14 (2013): 3730–3750, doi:10.1002/ggge.20230.
    Description: The Sr/Ca ratio of coral aragonite is used to reconstruct past sea surface temperature (SST). Twenty-one laboratories took part in an interlaboratory study of coral Sr/Ca measurements. Results show interlaboratory bias can be significant, and in the extreme case could result in a range in SST estimates of 7°C. However, most of the data fall within a narrower range and the Porites coral reference material JCp-1 is now characterized well enough to have a certified Sr/Ca value of 8.838 mmol/mol with an expanded uncertainty of 0.089 mmol/mol following International Association of Geoanalysts (IAG) guidelines. This uncertainty, at the 95% confidence level, equates to 1.5°C for SST estimates using Porites, so is approaching fitness for purpose. The comparable median within laboratory error is 〈0.5°C. This difference in uncertainties illustrates the interlaboratory bias component that should be reduced through the use of reference materials like the JCp-1. There are many potential sources contributing to biases in comparative methods but traces of Sr in Ca standards and uncertainties in reference solution composition can account for half of the combined uncertainty. Consensus values that fulfil the requirements to be certified values were also obtained for Mg/Ca in JCp-1 and for Sr/Ca and Mg/Ca ratios in the JCt-1 giant clam reference material. Reference values with variable fitness for purpose have also been obtained for Li/Ca, B/Ca, Ba/Ca, and U/Ca in both reference materials. In future, studies reporting coral element/Ca data should also report the average value obtained for a reference material such as the JCp-1.
    Description: E.C.H. (MARUM Fellowship) and T.F. were supported by the DFG-Research Center/Excellence Cluster ‘‘The Ocean in the Earth System,’’ University of Bremen. HVM was supported by an AINSE Research Fellowship.
    Description: 2014-03-23
    Keywords: Coral Sr/Ca ratios
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 3
    Publication Date: 2022-05-26
    Description: © The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature Communications 5 (2014): 4102, doi:10.1038/ncomms5102.
    Description: Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and δ18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1–2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.
    Description: Funding was provided by Deutsche Forschungsgemeinschaft (FE 615/4-1), Australian Research Council (Discovery grant DP1094001), Australia and New Zealand IODP Consortium, Australian Institute of Nuclear Science and Engineering, Natural Environmental Research Council (NE/H014136/1, NE/H014268/1), the Cooperative Research Program of the Center for Advanced Marine Core Research (10B039, 11A013, 11B041), Ministry of Earth Sciences, Govt. of India (with partial support from DST & ISRO-GBP) and Japan Society for the Promotion of Science (JSPS NEXT-GR031).
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 4
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    PANGAEA
    In:  Supplement to: Inoue, Mayuri; Yokoyama, Yusuke; Harada, Mariko; Suzuki, Atsushi; Kawahata, Hodaka; Matsuzaki, Hiroyuki; Iryu, Yasufumi (2010): Trace element variations in fossil corals from Tahiti collected by IODP Expedition 310: Reconstruction of marine environments during the last deglaciation (15 to 9 ka). Marine Geology, 271(3-4), 303-306, https://doi.org/10.1016/j.margeo.2010.02.016
    Publication Date: 2024-01-25
    Description: Climate responses and changes in marine environments during the last deglaciation have been controversial and few paleoceanographic data are available from the tropical South Pacific, though this region is crucial in the investigations of ocean-atmosphere interactions. Integrated Ocean Drilling Program Expedition 310 was conducted to establish the time course of the postglacial sea-level rise at Tahiti in the South Pacific. A principal objective of this expedition was to examine the variation of marine environments during the last deglaciation. As fossil Porites coral is ideal for assessing past marine environments, we selected only Porites specimens from the many coral specimens retrieved, examined them by XRD, and dated them by the 14C method. In all, we obtained 17 pristine Porites specimens composed of only aragonite with ages from 15 to 9 ka. Then, we measured Mg/Ca, Ba/Ca, and U/Ca ratios and Cd contents as proxies for upwelling and sea surface temperature. Higher Ba/Ca ratios and Cd content together with lower reconstructed SSTs using U/Ca ratios in the coral specimens between 12.6 and 9.8 cal ka compared to around 15 cal ka suggest that upwelling and/or entrainment of subsurface water into mixed layer was enhanced around Tahiti during this period. This finding is consistent with previous reports and supports the idea that the South Pacific was characterized by La Niña-like conditions at least from 12.6 to 9.8 cal ka.
    Keywords: 310-M0005B; 310-M0005C; 310-M0007A; 310-M0007B; 310-M0009D; 310-M0018A; 310-M0023A; Age, 14C AMS; Age, dated; Age, dated standard deviation; Area/locality; Calendar age; Calendar age, standard deviation; Depth, reconstructed; DP Hunter; DRILL; Drilling/drill rig; Elevation of event; Event label; Exp310; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Porites, Barium/Cadmium ratio; Porites, Cadmium; Porites, Magnesium/Calcium ratio; Porites, Uranium/Calcium ratio; Sample code/label; Sample ID; TAH-02A-4F; TAH-02A-5C; TAH-03A-1E; TAH-03A-3; TAH-03A-3A; TAH-03A-4A; TAH-03A-4B; Tahiti, offshore Maraa; Tahiti, offshore Tiarei; Tahiti Sea Level
    Type: Dataset
    Format: text/tab-separated-values, 203 data points
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  • 5
    Publication Date: 2024-01-25
    Keywords: 325-M0031A; 325-M0033A; 325-M0035A; 325-M0036A; 325-M0039A; 325-M0053A; 325-M0057A; Age, dated; Age, dated standard deviation; Date; DRILL; Drilling/drill rig; Event label; Exp325; Great Barrier Reef, Australia; Great Barrier Reef Environmental Changes; Greatship Maya; HYD_01CSite11; HYD_01Csite6; HYD_01CSite6; HYD_01CSite8; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Laboratory; NOG_01BSite2; NOG_01BSite6; Sample code/label; Site; Standard deviation; Thorium-230/Uranium-238 activity ratio; Thorium-232/Uranium-238 activity ratio; Thorium-232/Uranium-238 activity ratio, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-234/Uranium-238 activity ratio (0); Uranium-234/Uranium-238 activity ratio (0), standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 486 data points
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  • 6
    Publication Date: 2024-01-25
    Keywords: 325-M0031A; 325-M0033A; 325-M0035A; 325-M0036A; 325-M0039A; 325-M0053A; 325-M0057A; Age, dated; Age, dated standard deviation; Aragonite; Comment; DIVER; DRILL; Drilling/drill rig; Event label; Exp325; GBR-1023; GBR-1024; GBR-1108; GBR-206; GBR-219; GBR-307; GBR-318; GBR-537; GBR-947; GBR-954; Great Barrier Reef, Australia; Great Barrier Reef Environmental Changes; Greatship Maya; HYD_01CSite11; HYD_01Csite6; HYD_01CSite6; HYD_01CSite8; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Magnesium/Calcium ratio; NOG_01BSite2; NOG_01BSite6; Number; Papua New Guinea; PNG-21A; PNG-36; PNG-89B; Sample code/label; Sample comment; Sampling by diver; Site; Standard deviation; Strontium/Calcium ratio; δ13C, skeletal carbonate; δ18O, skeletal carbonate
    Type: Dataset
    Format: text/tab-separated-values, 739 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Inoue, Mayuri; Suwa, Ryota; Suzuki, Atsushi; Sakai, Kazuhiko; Kawahata, Hodaka (2011): Effects of seawater pH on growth and skeletal U/Ca ratios of Acropora digitifera coral polyps. Geophysical Research Letters, 38, L12809, https://doi.org/10.1029/2011GL047786
    Publication Date: 2024-03-15
    Description: The impact of ocean acidification caused by the increasing atmospheric CO2 has been studied in marine calcifiers, including hermatypic corals. However, the effect of elevated pCO2 on the early developmental life-cycle stage of corals has been little studied. In this study, we reared polyps of Acropora digitifera in seawater at pHT 6.55, 7.31, 7.64, 7.77, and 8.03, controlled by CO2 bubbling. We measured the dry weights of polyp skeletons after the 40-d experiment to investigate the relationship between the seawater aragonite saturation state and polyp growth. In addition, we measured skeletal U/Ca ratio to estimate their pH dependence. Skeletal weights of coral polyps increased with the aragonite saturation state and reached an apparent saturation plateau above pH 7.77. U/Ca ratios had a strong inverse relationship with pH and a negligible relationship with skeletal growth rate (polyp weight), suggesting that skeletal U/Ca could be useful for reconstructing paleo-pH.
    Keywords: Acropora digitifera; Acropora digitifera, weight; Acropora digitifera, weight, standard deviation; Alkalinity, total; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcification rate; 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; Cnidaria; Coast and continental shelf; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Laboratory experiment; Measured; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; pH meter (Metrohm electrodes); Replicates; Salinity; Salinity, standard deviation; Single species; Temperate; Temperature, standard deviation; Temperature, water; Uranium/Calcium ratio
    Type: Dataset
    Format: text/tab-separated-values, 710 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Tanaka, Yasuaki; Iguchi, Akira; Nishida, Kozue; Inoue, Mayuri; Nakamura, Takashi; Suzuki, Atsushi; Sakai, Kazuhiko (2014): Nutrient availability affects the response of juvenile corals and the endosymbionts to ocean acidification. Limnology and Oceanography, 59(5), 1468-1476, https://doi.org/10.4319/lo.2014.59.5.1468
    Publication Date: 2024-03-15
    Description: The interactive effects of nutrient availability and ocean acidification on coral calcification were investigated using post-settlement juvenile corals of Acropora digitifera cultured in nutrient-sufficient or nutrient-depleted seawater for 4 d and then exposed to seawater with different partial pressure of carbon dioxide () conditions (38.8 or 92.5 Pa) for 10 d. After the nutrient pretreatment, corals in the high nutrient condition (HN corals) had a significantly higher abundance of endosymbiotic algae than did those in the low nutrient condition (LN corals). The high abundance of endosymbionts in HN corals was reduced as a result of subsequent seawater acidification, and the chlorophyll a per algal cell increased. The photosynthetic oxygen production rate by endosymbionts was enhanced by the acidified seawater regardless of the nutrient treatment, indicating that the reduction in endosymbiont density in HN corals due to acidification was compensated for by the increase in chlorophyll a per cell. Though the photosynthetic rate increased in the acidified conditions for both LN and HN corals, the calcification rate significantly decreased for LN corals but not for HN corals. The acquisition of nutrients from seawater, rather than the increase in alkalinity caused by photosynthesis, might effectively alleviate the negative response of coral calcification to seawater acidification, suggesting that the response of corals and their endosymbionts to ocean acidification can be influenced by nutrient conditions.
    Keywords: Acropora digitifera; Alkalinity, total; Animalia; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthic animals; Benthos; Bicarbonate ion; Bicarbonate ion, standard deviation; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcification rate; Calcification rate, standard error; 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; Chlorophyll a; Chlorophyll a, standard error; Chlorophyll a per cell; Cnidaria; Coast and continental shelf; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laboratory experiment; Macro-nutrients; Net photosynthesis rate, oxygen; Net photosynthesis rate, oxygen, standard error; North Pacific; 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; Primary production/Photosynthesis; Salinity; Sesoko_Island; Single species; Species; Symbiont cell density; Symbiont cell density, standard error; Temperate; Temperature, water; Temperature, water, standard deviation; Treatment; δ13C; δ13C, standard error; δ18O; δ18O, standard error
    Type: Dataset
    Format: text/tab-separated-values, 156 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Felis, Thomas; McGregor, Helen V; Linsley, Braddock K; Tudhope, Alexander W; Gagan, Michael K; Suzuki, Atsushi; Inoue, Mayuri; Thomas, Alexander L; Esat, Tezer M; Thompson, William G; Tiwari, Manish; Potts, Donald C; Mudelsee, Manfred; Yokoyama, Yusuke; Webster, Jody M (2014): Intensification of the meridional temperature gradient in the Great Barrier Reef following the Last Glacial Maximum. Nature Communications, 5, 4102, https://doi.org/10.1038/ncomms5102
    Publication Date: 2024-04-20
    Description: Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and d18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.
    Keywords: Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 10
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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