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  • %OC; %TN; Basin; C3/C4 plants; Carbon, organic, total; Comment; DEPTH, water; Godavari River; India; LATITUDE; Local Time; Location; LONGITUDE; Monsoon; Nitrogen, total; precipitation; Precipitation, annual, mean; riverbed sediment; Rock type; Sample ID; Sample type; Season; Site; Size fraction; Soil; SPM; Sub-basin; Years; δ13C; δ13C, organic carbon; δ15N  (1)
  • 2,6,10-trimethylpentadecan-2-one  (1)
  • 202-1234; Age, dated; Age, dated standard deviation; age depth model; Age model, Bacon (Blaauw & Christen, 2011); calculated, 1 sigma; chilean margin; COMPCORE; Composite Core; DEPTH, sediment/rock; Foraminifera; Joides Resolution; Laboratory code/label; Leg202; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Ocean Drilling Program; ODP; radiocarbon age model; rbacon calibration curve choice; Reference/source; Reservoir age; Reservoir age, standard deviation; South Pacific Ocean; Student's t-test
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  • 1
    Publication Date: 2024-06-12
    Description: %OC, %TN, δ13C and δ15N analysed in C3 and C4 plants, soils, SPM and riverbed sediments in the Godavari River basin (India), located in the Core Monsoon Zone. Above-ground plant parts of C3 and C4 vegetation were collected at the end of the dry season (February/March 2015) across the Godavari basin, including trees, shrubs, herbaceous plants, grasses and dominant crops. Surface soils (0-10 cm) were collected near the Godavari River, and SPM (10-80 L, filtered over 0.7 μm GFF filters) and bulk and fine (≤63 μm) riverbed sediments were collected in a dry (February/March 2015) and wet season (July/August 2015). Mean Annual Precipitation (MAP) data were retrieved from Dearing Crampton-Flood et al. (2019) (https://doi.org/10.1594/PANGAEA.907818) and India Water Resources Information System (https://indiawris.gov.in/)
    Keywords: %OC; %TN; Basin; C3/C4 plants; Carbon, organic, total; Comment; DEPTH, water; Godavari River; India; LATITUDE; Local Time; Location; LONGITUDE; Monsoon; Nitrogen, total; precipitation; Precipitation, annual, mean; riverbed sediment; Rock type; Sample ID; Sample type; Season; Site; Size fraction; Soil; SPM; Sub-basin; Years; δ13C; δ13C, organic carbon; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 7070 data points
    Location Call Number Limitation Availability
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  • 2
    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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