作者: H. MEADE CADOT , W. R. VAN SCHMUS , R. L. KAESLER
DOI: 10.1130/0016-7606(1972)83[3519:MICOMO]2.0.CO;2
关键词:
摘要: Results of 255 microprobe analyses Holocene marine Ostracoda show that, for the 21 specimens analyzed, greatest variation in mole percent MgCO 3 occurs within calcite individual carapaces rather than between collected from warm and cold water. Within a single genus, however, differences different environments may reflect water temperature.