(Table 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vienna-SMOW standard ...

During the coring of Hole 525B with the hydraulic piston corer, a number of sediment samples were squeezed and the pore waters retained for stable isotope study. Both 18O/16O and D/H ratios were determined on the same samples. Within the limits of experimental error the measurements are consistent w...

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Bibliographic Details
Main Authors: Bath, Adrian, Shackleton, Nicholas J
Format: Dataset
Language:English
Published: PANGAEA 1984
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.810514
https://doi.pangaea.de/10.1594/PANGAEA.810514
id ftdatacite:10.1594/pangaea.810514
record_format openpolar
spelling ftdatacite:10.1594/pangaea.810514 2024-09-15T17:47:24+00:00 (Table 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vienna-SMOW standard ... Bath, Adrian Shackleton, Nicholas J 1984 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.810514 https://doi.pangaea.de/10.1594/PANGAEA.810514 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.74.121.1984 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample code/label DEPTH, sediment/rock δ18O, water δ Deuterium δ18O, standard deviation Drilling/drill rig DSDP/ODP/IODP sample designation see references Leg74 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1984 ftdatacite https://doi.org/10.1594/pangaea.81051410.2973/dsdp.proc.74.121.1984 2024-08-01T10:52:43Z During the coring of Hole 525B with the hydraulic piston corer, a number of sediment samples were squeezed and the pore waters retained for stable isotope study. Both 18O/16O and D/H ratios were determined on the same samples. Within the limits of experimental error the measurements are consistent with the variations resulting from evaporation-precipitation processes; there is no evidence that diagenetic processes in the sediment affected the isotopic composition of the waters, which therefore reflect changes in the isotopic composition of the ocean during the Cenozoic. The data are consistent with the hypothesis that a change of about 0.9 per mil (18O/16O) occurred during the middle Miocene, reflecting the growth of the Antarctic ice sheet at that time. ... : Supplement to: Bath, Adrian; Shackleton, Nicholas J (1984): Oxygen and hydrogen isotope studies in squeezed pore waters, Deep Sea Drilling Project Leg 74, Hole 525B: Evidence for mid-Miocene ocean isotopic change. In: Moore, TC Jr; Rabinowitz, PD; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 74, 697-699 ... Dataset Antarc* Antarctic Ice Sheet DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Sample code/label
DEPTH, sediment/rock
δ18O, water
δ Deuterium
δ18O, standard deviation
Drilling/drill rig
DSDP/ODP/IODP sample designation
see references
Leg74
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Sample code/label
DEPTH, sediment/rock
δ18O, water
δ Deuterium
δ18O, standard deviation
Drilling/drill rig
DSDP/ODP/IODP sample designation
see references
Leg74
Glomar Challenger
Deep Sea Drilling Project DSDP
Bath, Adrian
Shackleton, Nicholas J
(Table 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vienna-SMOW standard ...
topic_facet Sample code/label
DEPTH, sediment/rock
δ18O, water
δ Deuterium
δ18O, standard deviation
Drilling/drill rig
DSDP/ODP/IODP sample designation
see references
Leg74
Glomar Challenger
Deep Sea Drilling Project DSDP
description During the coring of Hole 525B with the hydraulic piston corer, a number of sediment samples were squeezed and the pore waters retained for stable isotope study. Both 18O/16O and D/H ratios were determined on the same samples. Within the limits of experimental error the measurements are consistent with the variations resulting from evaporation-precipitation processes; there is no evidence that diagenetic processes in the sediment affected the isotopic composition of the waters, which therefore reflect changes in the isotopic composition of the ocean during the Cenozoic. The data are consistent with the hypothesis that a change of about 0.9 per mil (18O/16O) occurred during the middle Miocene, reflecting the growth of the Antarctic ice sheet at that time. ... : Supplement to: Bath, Adrian; Shackleton, Nicholas J (1984): Oxygen and hydrogen isotope studies in squeezed pore waters, Deep Sea Drilling Project Leg 74, Hole 525B: Evidence for mid-Miocene ocean isotopic change. In: Moore, TC Jr; Rabinowitz, PD; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 74, 697-699 ...
format Dataset
author Bath, Adrian
Shackleton, Nicholas J
author_facet Bath, Adrian
Shackleton, Nicholas J
author_sort Bath, Adrian
title (Table 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vienna-SMOW standard ...
title_short (Table 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vienna-SMOW standard ...
title_full (Table 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vienna-SMOW standard ...
title_fullStr (Table 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vienna-SMOW standard ...
title_full_unstemmed (Table 1) Pore water isotopes from DSDP Hole 74-525B, with respect to the Vienna-SMOW standard ...
title_sort (table 1) pore water isotopes from dsdp hole 74-525b, with respect to the vienna-smow standard ...
publisher PANGAEA
publishDate 1984
url https://dx.doi.org/10.1594/pangaea.810514
https://doi.pangaea.de/10.1594/PANGAEA.810514
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_relation https://dx.doi.org/10.2973/dsdp.proc.74.121.1984
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.81051410.2973/dsdp.proc.74.121.1984
_version_ 1810496663197843456