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9 datasets found! (Query time: 6 ms)
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Expedition 357 Scientists (2016): Total carbon, total inorganic carbon and total organic carbon content in standard shipboard samples from IODP Hole 357-M0071A
https://doi.org/10.1594/PANGAEA.867576 - Score: 31.605
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Expedition 357 Scientists (2016): Total carbon, total inorganic carbon and total organic carbon content in standard shipboard samples from IODP Hole 357-M0069A
https://doi.org/10.1594/PANGAEA.867575 - Score: 31.572
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Expedition 357 Scientists (2016): Total carbon, total inorganic carbon and total organic carbon content in standard shipboard samples from IODP Hole 357-M0076B
https://doi.org/10.1594/PANGAEA.867580 - Score: 31.239
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Expedition 357 Scientists (2016): Total carbon, total inorganic carbon and total organic carbon content in standard shipboard samples from IODP Hole 357-M0068A
https://doi.org/10.1594/PANGAEA.867573 - Score: 31.239
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Expedition 357 Scientists (2016): Total carbon, total inorganic carbon and total organic carbon content in standard shipboard samples from IODP Hole 357-M0068B
https://doi.org/10.1594/PANGAEA.867574 - Score: 31.067
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Expedition 357 Scientists (2016): Total carbon, total inorganic carbon and total organic carbon content in standard shipboard samples from IODP Hole 357-M0071C
https://doi.org/10.1594/PANGAEA.867577 - Score: 31.067
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Expedition 357 Scientists (2016): Total carbon, total inorganic carbon and total organic carbon content in standard shipboard samples from IODP Hole 357-M0072B
https://doi.org/10.1594/PANGAEA.867578 - Score: 31.067
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Expedition 357 Scientists (2016): Total carbon, total inorganic carbon and total organic carbon content in standard shipboard samples from IODP Hole 357-M0075B
https://doi.org/10.1594/PANGAEA.867579 - Score: 31.067
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Ternieten, L; Früh-Green, GL; Bernasconi, SM (2021): Content and carbon and oxygen isotope composition of total carbon, total non-carbonate carbon, and total inorganic carbon of basement rocks from the southern wall of the Atlantis Massif, IODP Expedition 357
Abstract: |
The carbon geochemistry of serpentinized peridotites, gabbroic rocks, and sediments recovered during IODP Expedition 357 (October to December 2015) on the Atlantis Massif, Mid-Atlantic Ridge was examined to characterize carbon sources and the fate of dissolved organic (DOC) and inorganic carbon (DIC) in seawater during long-lived hydrothermal circulation and serpentinization. The measurements were performed at the ETH Zurich, Geological Institute from 2017 to 2020 using a FlashEA 1112 Elemental Analyzer (EA) interfaced via a Conflo IV to a Delta V Plus Isotope Ratio Mass Spectrometer for total carbon (TC) and total non-carbonate carbon (NCC) content and isotope composition, a CM 5012 CO2 coulometer interfaced with a CM 5130 Acidification Module for the total inorganic carbon (TIC) content, and a GasBench II connected to a Delta V Mass Spectrometer for the total inorganic carbon isotope composition. The Results are reported as replicates. |
Size: |
1955 data points |
https://doi.org/10.1594/PANGAEA.935278 - Score: 26.318
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