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  • 1
    Publication Date: 2019-09-23
    Description: [1] The Integrated Ocean Drilling Program (IODP) Expedition 310 recovered drill cores from the drowned reefs around the island of Tahiti (17°40′S, 149°30′W), many of which contained samples of massive corals from the genus Porites. Herein we report on one well-preserved fossil coral sample: a 13.6 cm long Porites sp. dated by uranium series techniques at 9523 ± 33 years. Monthly δ18O and Sr/Ca determinations reveal nine clear and robust annual cycles. Coral δ18O and Sr/Ca determinations estimate a mean temperature of ∼24.3°C (∼3.2°C colder than modern) for Tahiti at 9.5 ka; however, this estimate is viewed with caution since potential sources of cold bias in coral geochemistry remain to be resolved. The interannual variability in coral δ18O is similar between the 9.5 ka coral record and a modern record from nearby Moorea. The seasonal cycle in coral Sr/Ca is approximately the same or greater in the 9.5 ka coral record than in modern coral records from Tahiti. Paired analysis of coral δ18O and Sr/Ca indicates cold/wet (warm/dry) interannual anomalies, opposite from those observed in the modern instrumental record.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-12-22
    Keywords: AGE; Alkenone, C37, δ13C; Alkenone, C37, δ13C, standard deviation; Alkenone, unsaturation index UK'37; CALYPSO; Calypso Corer; IMAGES II; Marion Dufresne (1995); MD105; MD96-2080; MD962080, ABS; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Southern Agulhas Bank; Tetraether index of 86 carbon atoms, high-temperature region; δ Deuterium, alkenone, C37; δ Deuterium, alkenone, C37, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 127 data points
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  • 3
    Publication Date: 2023-12-22
    Keywords: AGE; Alkenone, C37, δ13C; Alkenone, C37, δ13C, standard deviation; Alkenone, unsaturation index UK'37; CALYPSO; Calypso Corer; Marion Dufresne (1995); MD02-2594; MD128; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Southern Ocean; SWAF; Tetraether index of 86 carbon atoms, high-temperature region; δ Deuterium, alkenone, C37; δ Deuterium, alkenone, C37, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Kasper, Sebastian; van der Meer, Marcel T J; Castañeda, Isla S; Tjallingii, Rik; Brummer, Geert-Jan A; Sinninghe Damsté, Jaap S; Schouten, Stefan (2015): Testing alkenone D/H ratio as a paleo indicator of sea surface salinity in a coastal ocean margin (Mozambique Channel). Organic Geochemistry, 78, 62-68, https://doi.org/10.1016/j.orggeochem.2014.10.011
    Publication Date: 2023-12-22
    Description: Reconstructing past ocean salinity is important for assessing paleoceanographic change and therefore past climatic dynamics. Commonly, sea water salinity reconstruction is based on foraminifera oxygen isotope ratio values combined with sea surface temperature reconstruction. However, the approach relies on multiple proxies, resulting in relatively large uncertainty and, consequently, relatively low accuracy of salinity estimates. An alternative tool for past ocean salinity reconstruction is the hydrogen isotope composition of long chain (C37) alkenones (dDalkenone). Here, we applied dDalkenone to a 39 ka long coastal sediment record from the Eastern South African continental shelf in the Mozambique Channel, close to the Zambezi River mouth. Despite changes in global sea water dD related to glacial - interglacial ice volume effects, no clear changes were observed in the dDalkenone record throughout the entire 39 ka. The BIT index record from the same core showed high BIT values during the glacial and low values during the Holocene. This indicates a more pronounced freshwater influence at the core location during the glacial, resulting in alkenones depleted in deuterium during that time and, thereby, explains the lack of a clear glacial-interglacial alkenone dD shift. Correlation between the BIT index and dDalkenone during the glacial period suggests that increased continental runoff potentially changed the growth conditions of the alkenone producing haptophytes, promoting coastal haptophyte species with generally more enriched dDalkenone values. We therefore suggest that the application of dDalkenone for reconstructing past salinity in coastal settings may be complicated by changes in the alkenone producing haptophyte community.
    Keywords: 64PE304; 64PE304-80; AGE; Alkenone C37/C38 ratio; Branched and isoprenoid tetraether index; DEPTH, sediment/rock; GC; Gravity corer; INATEX-GEO; Pelagia; South-East African margin; δ Deuterium, alkenone; δ Deuterium, alkenone, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 591 data points
    Location Call Number Limitation Availability
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