Middle Pliocene temperature implications based on the Bryozoa Hippothoa (Cheilostomata-Ascophora)
Middle Pliocene temperature implications based on the Bryozoa Hippothoa (Cheilostomata-Ascophora)
复制标题
基于苔藓虫属 (Cheilostomata-Ascophora) 的中上新世温度影响
DOI：
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发表时间：
1976
期刊：
影响因子：
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通讯作者：
P. Morris
中科院分区：
文献类型：
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作者：
P. Morris
今天常见于北美太平洋沿岸潮间带和潮下带的三种希波索动物需要特定的温度才能形成孵卵室或卵细胞。这些物种在西海岸作为化石被发现，温度要求被用来解释费尔南多组、埃切戈因组、皮科组和里奥戴尔组中上新世化石组合的古温度。
Three species of Hippothoa which are commonly found today in the intertidal and subtidal zones along the Pacific Coast of North America require specific temperatures for the formation of a brood chamber or ovicell. These species are found as fossils on the west coast and the temperature requirements are used to interpret paleotemperatures of Middle Pliocene fossil assemblages in the Fernando, Etchegoin, Pico, and Rio Dell Formations.