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  • 2005-2009  (9)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: van Breugel, Yvonne; Baas, Marianne; Schouten, Stefan; Mattioli, Emanuela; Sinninghe Damsté, Jaap S (2006): Isorenieratane record in black shales from the Paris Basin, France: Constraints on recycling of respired CO2 as a mechanism for negative carbon isotope shifts during the Toarcian oceanic anoxic even. Paleoceanography, 21(4), PA4220, https://doi.org/10.1029/2006PA001305
    Publication Date: 2023-08-04
    Description: The prominent negative stable carbon isotope excursion in both carbonate and organic carbon recorded in organic-rich sediments deposited during the Toarcian oceanic anoxic event (OAE) has commonly been explained by recycling of 13C-depleted CO2 (the so-called Küspert model). More recently, the massive release of 13C-depleted methane or other forms of 13C-depleted carbon was also proposed to account for the observed negative d13C excursions in organic carbon of terrigenous as well as of marine origin. The occurrence of diagenetic products of the carotenoid isorenieratene (isorenieratane and other aryl isoprenoids) in Toarcian black shales has been regarded as supporting evidence for the Küspert hypothesis as they point to strong stratification of the epicontinental seas. A section of a drill core straddling the Toarcian of the Paris Basin (Cirfontaine-en-Ornois) contained intact isorenieratane, providing evidence that photosynthetic green sulphur bacteria were present at the time of deposition, even prior to the OAE. However, the isorenieratane abundances are very low in the section where the negative d13C excursion in organic carbon and phytane, a chemical fossil derived from chlorophyll, occurs. The abundance of the isorenieratene derivatives increases, once the d13C records have shifted to more positive values. The d13C of isorenieratane (generally circa -13.1 ± 0.5 per mil) indicates that the respired CO2 contribution at the chemocline was low and is thus not likely to be the main cause of the prominent up to 7per mil negative d13C shift recorded in Toarcian organic carbon records.
    Keywords: -; ANDRA_HTM102; Calculated; DEPTH, sediment/rock; DRILL; Drilling/drill rig; France; Isorenieratane, δ13C; Isorenieratane, δ13C, standard deviation; Isotope ratio monitoring (IRM) mass spectrometry; Mass spectrometer Finnigan Delta Plus; δ13C, carbon dioxide, aquatic; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-01-09
    Keywords: 151-913B; AGE; Branched and isoprenoid tetraether index; Cyclization ratio of branched tetraethers; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg151; Methylation index of branched tetraethers; North Greenland Sea; Ocean Drilling Program; ODP; Sample code/label; Temperature, air, annual mean
    Type: Dataset
    Format: text/tab-separated-values, 159 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-01-09
    Keywords: 151-913B; AGE; Counting 〉135 µm fraction; DRILL; Drilling/drill rig; Ice rafted debris; Joides Resolution; Leg151; North Greenland Sea; Ocean Drilling Program; ODP
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-01-09
    Keywords: 104-643; 151-913; 162-985; AGE; COMPCORE; Composite Core; Elevation of event; Event label; Joides Resolution; Latitude of event; Leg104; Leg151; Leg162; Longitude of event; North Greenland Sea; Norwegian Sea; Ocean Drilling Program; ODP; Temperature, air, annual mean; Temperature, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-01-09
    Keywords: 207-1258; Branched and isoprenoid tetraether index; Calcium carbonate; Carbon, organic, total; Carbon, organic, total, standard deviation; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Isotope ratio mass spectrometry; Isotopic event; Joides Resolution; Leg207; Ocean Drilling Program; ODP; Positive-ion thermal-ionization mass spectrometry; Sample, optional label/labor no; Sample code/label; Sea surface temperature, annual mean; Sea surface temperature, standard deviation; South Atlantic Ocean; Tetraether index of 86 carbon atoms; Time zone; δ13C; δ13C, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 529 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-01-09
    Keywords: 207-1259; Branched and isoprenoid tetraether index; Calcium carbonate; Carbon, organic, total; Carbon, organic, total, standard deviation; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Isotope ratio mass spectrometry; Isotopic event; Joides Resolution; Leg207; Ocean Drilling Program; ODP; Positive-ion thermal-ionization mass spectrometry; Sample, optional label/labor no; Sample code/label; Sea surface temperature, annual mean; Sea surface temperature, standard deviation; South Atlantic Ocean; Tetraether index of 86 carbon atoms; Time zone; δ13C; δ13C, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 410 data points
    Location Call Number Limitation Availability
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Forster, Astrid; Schouten, Stefan; Baas, Marianne; Sinninghe Damsté, Jaap S (2007): Mid-Cretaceous (Albian-Santonian) sea surface temperature record of the tropical Atlantic Ocean. Geology, 35(10), 919-922, https://doi.org/10.1130/G23874A.1
    Publication Date: 2024-01-09
    Description: Paleoclimate records of geologic time periods characterized by extreme global warmth such as the mid-Cretaceous are important for a better understanding of the Earth's climate system operating in an exceptionally warm mode. Here we applied an organic geochemical proxy (TEX86) on organic matter-rich Albian-Santonian sediments, recovered from Ocean Drilling Program Leg 207 Sites 1258 and 1259 on Demerara Rise, to reconstruct sea surface temperatures (SSTs) in the western equatorial Atlantic. Preceded by a stepwise Cenomanian warming trend (~31-35°C), the onset of the Cretaceous thermal maximum coincided here with the Cenomanian-Turonian boundary event. Once established, this extreme warm climate regime, characterized by averaged tropical SSTs close to 35°C, lasted up to the Turonian-Coniacian transition. Two pronounced cooler intervals (~2-3°C) interrupt this otherwise remarkably stable record, providing the first d18O independent evidence for middle Turonian cooling that previously has been attributed to glacioeustatic sea-level lowering. Coniacian SSTs decline stepwise, reaching a minimum in the Santonian (~32-33°C), where cooling is most pronounced, presumably concomitant with the first progressive opening of a deep-water passage through the equatorial Atlantic gateway.
    Keywords: 207-1258; 207-1259; COMPCORE; Composite Core; Joides Resolution; Leg207; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Schouten, Stefan; Eldrett, James S; Greenwood, David R; Harding, Ian C; Baas, Marianne; Sinninghe Damsté, Jaap S (2008): Onset of long-term cooling of Greenland near the Eocene-Oligocene boundary as revealed by branched tetraether lipids. Geology, 36(2), 147, https://doi.org/10.1130/G24332A.1
    Publication Date: 2024-01-09
    Description: The Eocene-Oligocene (E-O) boundary interval is considered to be one of the major transitions in Earth's climate, witnessing the first major expansion of the East Antarctic Ice Sheet. However, the extent of the associated climatic cooling, especially for high northern latitude continental landmasses, is poorly constrained. In this study we reconstruct the first mean annual air temperature (MAAT) for the Greenland landmass during the late Eocene and early Oligocene by applying a new proxy based on the distribution of branched tetraether lipids derived from soil bacteria preserved in a marine sediment core from the Greenland Basin. The temperature estimates are compared with a composite continental temperature record based on bio-climatic analysis of pollen assemblages. Both proxies reveal comparable late Eocene MAATs of ~13-15 °C and a gradual long-term cooling of ~3-5 °C starting near the E-O boundary. These data are in agreement with other MAAT reconstructions from northern midlatitude continents and suggest a general cooling of the Northern Hemisphere during the E-O transition.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2022-05-25
    Description: Author Posting. © Elsevier B.V., 2007. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Organic Geochemistry 39 (2008): 135-146, doi:10.1016/j.orggeochem.2007.09.002.
    Description: The ubiquitous isoprenoid phytol was isolated from a range of algae, terrestrial plants and a bacterium and its two terminal carbon atoms were quantitatively removed by chemical oxidation. The product, 6,10,14-trimethylpentadecan-2-one, was depleted in 13C by 1-4‰ relative to the parent phytol. This difference is significant, and indicates that the pathway for biosynthesis of phytol induces substantial intramolecular stable carbon isotopic fractionations. The nature and magnitude of the fractionations suggest strongly that it is associated both with the biosynthesis of isopentenyl pyrophosphate via the 2-C-methylerythritol-4-phosphate pathway and with the formation of carotenoids and phytol from geranyl-geraniolphosphate. As a result of these large, intramolecular isotopic differences, diagenetic products formed by loss of C, such as pristane, may be naturally depleted in 13C by several permil relative to phytane.
    Description: Shell International Petroleum Maatschappij BV is thanked for financial support for the irm- GC-MS facility
    Keywords: Phytol ; Phytane ; Pristane ; Stable carbon isotope ; Mevalonic acid pathway ; 2-C-methylerythritol-4-phosphate pathway ; 2,6,10-trimethylpentadecan-2-one
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
    Location Call Number Limitation Availability
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