作者: Carrie Morrill , Paul L. Koch
DOI: 10.1130/0091-7613(2002)030<0151:EOAEOI>2.0.CO;2
关键词: Snowmelt 、 Isotope 、 Seawater 、 Drainage basin 、 Geology 、 Diagenesis 、 Paleontology 、 Geochemistry 、 Green River Formation 、 Calcite 、 Isotopes of oxygen
摘要: Low oxygen isotope values (∼−16‰, relative to Peedee belemnite standard) obtained from microbial carbonates of the Green River Formation have been interpreted as evidence for snowmelt and high elevations surrounding this early Eocene lake basin. However, low precipitates could also represent a diagenetic overprint. We investigate these alternate hypotheses by measuring composition altered unaltered freshwater bivalves analyzed subannual samples 3 individuals bulk 54 individuals. Subannual exhibit clear seasonal fluctuations in values. These are large enough require shifts temperature and/or value water. lowest any sample (either or resolution) corresponds lake-water δ 18 O ∼−12‰ (relative standard mean ocean water) is not addition lake. A few very values, which would seem suggest snowmelt. show calcite X-ray diffraction patterns, demonstrating presence precipitates. Given that (1) alteration plausible explanation (2) has examined carbonates, (3) aragonitic provide no independent waters, we conclude robust isotopic Basin during currently lacking.