Oxygen isotope composition of human tooth enamel from medieval Greenland: Linking climate and society: Comment and Reply

Geology

Volumn 24, Issue 5, 1996, Pages 478-479

  Fricke, Henry C ^a   O'Neil, James R ^a   Lynnerup, Niels ^b  

^a UNIVERSITY OF MICHIGAN   (United States)

^b UNIVERSITY OF COPENHAGEN   (Denmark)

Author keywords

[No Author keywords available]

Indexed keywords

ISOTOPIC COMPOSITION; MEDIEVAL; OXYGEN ISOTOPE; TOOTH;

ARCTIC; GREENLAND;

EID: 2642607371     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/0091-7613(1996)024<0477:OICOHT>2.3.CO;2     Document Type: Letter

References (9)

1. Cooper, L. W., Solis, C., Kane, D. L., and Hinzman, L. D., 1993, Application of oxygen-18 tracer techniques to Arctic hydrological processes: Arctic and Alpine Research, v. 25, p. 247-255.
2. Dansgaard, W., 1964, Stable isotopes in precipitation: Tellus, v. 16, p. 436-468.
3. Fricke, H. C., and O'Neil, J. R., 1996, Inter- and intra-tooth variation in mammalian tooth enamel phosphate: Implications for paleoclimatological and paleobiological research: Paleogeography, Paleoclimatology, and Paleoecology (in press).
4. Fricke, H. C., O'Neil, J. R., and Lynnerup, N., 1995, Oxygen isotope composition of human tooth enamel from medieval Greenland: Linking climate and society: Geology, v. 23, p. 869-872.
5. Halffman, C. M., Scott, G. R., and Pedersen, P. O., 1992, Palatine torus in the Greenlandic Norse: American Journal of Physical Anthropology, v. 88, p. 145-161.
6. Lynnerup, N., 1995, The Greenland Norse: A biological anthropology study [Ph.D. thesis]: Copenhagen, Denmark, University of Copenhagen, 287 p.
7. McGovern, T. H., 1980, Cows, harp seals, and churchbells: Adaptation and extinction in Norse Greenland: Human Ecology, v. 8, p. 245-275.
8. Maulé, C. P., Chanasyk, D. S., and Muelenbachs, K., 1994, Isotopic determination of snow-water contribution to soil water and groundwater: Journal of Hydrology, v. 155, p. 73-91.
9. Stuiver, M., Grootes, P. M., and Braziunas, T. F., 1995, The GISP2 d18O climate record of the past 16 500 years and the role of the sun, ocean, and volcanoes: Quaternary Research(24[5]), v. 44, p. 341-354.