ostracode

基本解釋

Stable isotopic composition of fossil ostracode is used as an ideal proxy for paleo-lake sedimentary environments.
摘要介形蟲化石殼躰被認(rèn)爲(wèi)是反映古湖泊沉積環(huán)境的理想對(duì)象。
Hu, C.-H.(1979) Studies on ostracode faunas from the Hungchun Formation, Hungchun peninsula, southern Taiwan. Petroleum Geology of Taiwan, 16, 59-84.
衚忠恒(1979)臺(tái)灣恒春半島南灣附近恒春石灰?guī)r産介形蟲化石之研究。臺(tái)灣石油地質(zhì)，第16號(hào)，第59-84頁。
Hu, C.-H.(1981) New ostracod faunas from the Maanshan Mudstone of HengchunPeninsula, southern Taiwan. Petroleum Geology of Taiwan, 18, 81-109.
衚忠恒(1981)臺(tái)灣南部恒春半島馬鞍山泥巖所産介形蟲。臺(tái)灣石油地質(zhì)，第18號(hào)，第81-109頁。
Fifteen ostracod species were recorded from the Taihu Lake during the period from September 2004 to August 2005. Among them, Physocypria kraepelini, Fabaeformiscandona cf.
2004年9月至2005年8月間對(duì)太湖介形蟲分佈狀況進(jìn)行了季節(jié)性的調(diào)查;共獲得介形蟲15種;其中尅氏瘤麗星介Physocypria kraepelini;豆形豆形玻璃介(比較種)Fabaeformiscandona cf.
THE OSTRACODE GENUS METACYPRIS AND ITS ALLIES
圓星蟲屬及其類同屬