(Table 1) Stable oxygen isotope ratios of interstitial waters from ODP Sites 164-994 and 164-997
The d18O values of interstitial waters from Site 994 and Site 997 sediments, Blake Ridge, western Atlantic, tend to decrease with depth from 0.3 per mil to -0.5 per mil Standard Mean Ocean Water in the upper 200 mbsf, then fluctuate with significant positive spikes of Delta = 0.2 per mil - 0.5 per m...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2000
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.803618 https://doi.org/10.1594/PANGAEA.803618 |