The DOI matches its Crossref record; 9 of the 9 references it cites were found in a registry or an index.
ISOTOPIC RECONSTRUCTION OF PAST CONTINENTAL ENVIRONMENTS
Abstract
▪ Abstract Vertebrate fossils and continental sediments provide a rich record of variations in the isotopic composition of surface environments. To interpret these records, a greater understanding of isotopic sources, as well as fractionations associated with animal physiology, soil geochemistry, and diagenesis, has been essential. Tooth enamel and fish otoliths yield subannual records of surface environments, whereas soil minerals may integrate signals over many thousands of years. Carbon isotope variations in fossil vertebrates and soils record changes in the structure of vegetation and the isotope composition and concentration of atmospheric CO 2. Oxygen isotope variations may be indirectly related to climate, through reconstruction of the oxygen isotope composition of meteoric water, or directly related to temperature, through application of oxygen isotope paleothermometry to soil minerals or otoliths. In Africa, nitrogen isotope variations show promise as a proxy for rainfall abundance, though the generality of this association elsewhere has not been demonstrated.
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Cites
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Apatites in biological systems
Zapanta LeGeros, R. (1981) · Progress in Crystal Growth and Characterization · doi:10.1016/0146-3535(81)90046-0 · Cited by 622 · cited 1×
“It contains 5 wt% organic matter (chiefly non-collagenous proteins), and it has much larger crystals (∼1000 × 130 × 30 nm) with fewer defects and substitutions (LeGeros 1981).”
BackgroundThe Rise of Plants and Their Effect on Weathering and Atmospheric CO 2
Berner, R. A. (1997) · Science · doi:10.1126/science.276.5312.544 · Cited by 546
Calculation of oxygen isotope fractionation in metal oxides
Yong-fei, Z. (1991) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(91)90105-e · Cited by 337
Middle to Late Paleozoic Atmospheric CO 2 Levels from Soil Carbonate and Organic Matter
Mora, C. I., Driese, S. G., & Colarusso, L. A. (1996) · Science · doi:10.1126/science.271.5252.1105 · Cited by 239
Cited by
Assessing the Causes of Late Pleistocene Extinctions on the Continents
Barnosky, A. D., Koch, P. L., Feranec, R. S., Wing, S. L., & Shabel, A. B. (2004) · Science · doi:10.1126/science.1101476 · Cited by 1,084
Self-citationGuo, W. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.07.055 · Cited by 108
Guo, W., & Zhou, C. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.11.018 · Cited by 55
Geographic origins and dietary transitions during the Bronze Age in the Oman Peninsula
Gregoricka, L. A. (2013) · American Journal of Physical Anthropology · doi:10.1002/ajpa.22360 · Cited by 34
Extraction and sequencing of human and Neanderthal mature enamel proteins using MALDI-TOF/TOF MS
Nielsen-Marsh, C. M., Stegemann, C., Hoffmann, R., Smith, T., Feeney, R., Toussaint, M., Harvati, K., Panagopoulou, E., Hublin, J.-J., & Richards, M. P. (2009) · Journal of Archaeological Science · doi:10.1016/j.jas.2009.04.004 · Cited by 33
Metadata
- Authors
- Koch, P. L.
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 1998-05
- Volume
- 26
- Issue
- 1
- Pages
- 573-613
- ISSN
- 0084-6597 (ISSN-L)
- 1545-4495
- OpenAlex
- W2123085228
- Cited by
- 566
- References
- 9
- FWCI
- 3.72
- Type
- journal article
- Language
- en
- Open access
- closed
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- Koch, P. L. (1998). ISOTOPIC RECONSTRUCTION OF PAST CONTINENTAL ENVIRONMENTS. Annual Review of Earth and Planetary Sciences. https://doi.org/10.1146/annurev.earth.26.1.573
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.