Arid
Stable isotopes of speleothems from the Yucatan Peninsula, Mexico
Ayers, Meredith
出版年2010
学位类型硕士
导师Perry, Eugene
学位授予单位Northern Illinois University
英文摘要Two stalagmites, SAN-H and TABI-I were collected from caves in the northern Yucatan Peninsula to analyze for the stable isotopes of carbon and oxygen. The δ13C value can be used to determine whether C3 or C4/CAM vegetation was dominant and the δ 18O value can theoretically be used to determine whether the climate was wet or arid. Samples were cut, polished, dated using U/Th dating, and sampled using a micromill. SAN-H was dated as Early Classic (1650-1350 B.P.) to the Middle Preclassic 2850-2250 B.P) and the δ13C and δ18O appears to reinforce the interpretations from similar studies. The range of isotope values for δ18O and δ13C were -2.3 to -5.5‰ and -4.0 to -10.3‰, respectively. Although the U/Th dates for TABI-I range from Historical to Late Classic(1350-1050 B.P.), the early Late Classic date is almost certainly invalid, and is the result of presence of clastic material in the sample. TABI-I's range of isotope values for δ18O and δ 13C were –2.1 to -4.9‰ and –4.7 to -9.6‰, respectively. TABI-I's δ18O values appear to be supportive of interpretations found in the literature based on lakecore, stalagmite and sediment studies, and δ13C values could be informative about possible vegetation and land use in the immediate vicinity. Problems with dating reversal and dating accuracy prevented more detailed interpretations of the data.
英文关键词Maya Paleoclimate Speleothems Stable isotopes Stalagmites Yucatan Peninsula
语种英语
国家United States
来源学科分类Geology; Paleoclimate Science; Geochemistry
URLhttps://pqdtopen.proquest.com/doc/522105404.html?FMT=AI
来源机构Northern Illinois University
资源类型学位论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/244427
推荐引用方式
GB/T 7714
Ayers, Meredith. Stable isotopes of speleothems from the Yucatan Peninsula, Mexico[D]. Northern Illinois University,2010.
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