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Oxygen isotopic composition of mammalian skeletal phosphate from the Natufian Period, Hayonim Cave, Israel: Diagenesis and paleoclimate
Author(s) -
ShahackGross Ruth,
Tchernov Eitan,
Luz Boaz
Publication year - 1999
Publication title -
geoarchaeology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.696
H-Index - 44
eISSN - 1520-6548
pISSN - 0883-6353
DOI - 10.1002/(sici)1520-6548(199901)14:1<1::aid-gea1>3.0.co;2-8
Subject(s) - diagenesis , enamel paint , geology , carbonate , isotopes of oxygen , δ18o , cave , paleoclimatology , geochemistry , paleontology , mineralogy , stable isotope ratio , chemistry , archaeology , climate change , oceanography , geography , dentistry , medicine , physics , organic chemistry , quantum mechanics
Recent and fossil (prehistoric, Natufian) gazelle bones, dentin and enamel were analyzed for their oxygen isotopic composition (δ 18 O) of the phosphate and carbonate, as well as their crystallinity. Fossil bones and dentin have better crystallinity than recent specimens, indicating diagenetic change. Fossil enamel, on the other hand, is identical in crystallinity to recent enamel, indicating the lack of diagenetic alteration. Comparison of δ 18 O of carbonate and phosphate of the skeletal elements suggests that the coexisting phosphate and carbonate of both the recent and fossil specimens are close to isotopic equilibrium. This might suggest that both phases were affected by the same degree of diagenetic alteration, and that comparison of their δ 18 O is not useful for the selection of pristine material for paleoclimatic reconstruction purposes. Oxygen isotope analysis of gazelle enamel from the Natufian period from Hayonim Cave, Israel, show depletion in δ 18 O in comparison with recent enamel. This depletion is interpreted to represent a colder and/or wetter climate in the Natufian of northern Israel. © 1999 John Wiley & Sons, Inc.