Coupled Stable-Isotope and Trace-Element Measurements of Lacustrine Carbonates as Paleoclimatic Indicators
Open Access
- 2 April 2013
- book chapter
- Published by Wiley
- p. 113-121
- https://doi.org/10.1029/gm078p0113
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- Magnesium content of non-marine ostracod shells: A new palaeosalinometer and palaeothermometerPublished by Elsevier ,2003
- Trace-element chemistry of non-marine ostracods as a means of palaeolimnological reconstruction: An example from the Quaternary of Kashmir, northern IndiaChemical Geology, 1992
- Change in the size of Walker Lake during the past 5000 yearsPalaeogeography, Palaeoclimatology, Palaeoecology, 1991
- A review of the palaeohydrological interpretation of carbon and oxygen isotopic ratios in primary lacustrine carbonatesChemical Geology: Isotope Geoscience section, 1990
- Determination of both chemical and stable isotope composition in milligramme-size carbonate samplesSedimentary Geology, 1989
- Biological remains, geochemistry and stable isotopes for the reconstruction of environmental and hydrological changes in the holocene lakes from North SaharaPalaeogeography, Palaeoclimatology, Palaeoecology, 1987
- Strontium content of ostracods indicates lacustrine palaeosalinityNature, 1985
- Great Salt Lake, and precursors, Utah: The last 30,000 yearsContributions to Mineralogy and Petrology, 1984
- Strontium-Calcium Thermometry in Coral SkeletonsScience, 1979
- Late Quaternary Stratigraphy and Radiocarbon Chronology of Water Level Fluctuations in Lake Keilambete, VictoriaNature, 1971