The preceding Palaeocene epoch was also brought to an end, the rocks suggest, by a sudden release of methane.
岩石层研究表明甲烷的突然释放导致了之前的古新世时期结束。
单词 | Palaeocene epoch |
释义 |
Palaeocene epoch
原声例句
经济学人-科技 The preceding Palaeocene epoch was also brought to an end, the rocks suggest, by a sudden release of methane. 岩石层研究表明甲烷的突然释放导致了之前的古新世时期结束。
中文百科
古新世 Paleocene(重定向自Palaeocene epoch)
古新世(英语:Paleocene)是地质时代中古近纪(英语:Paleogene)的第一个主要时期,大约开始于6500万年前,终于5580万年前,介于中生代白垩纪的马斯特里赫特阶(Maastrichtian)与始新世(Eocene)之间。古新世来自希腊文的“παλαιός”(palaios,古)与“καινός”(kainos,新)。古新世接续在白垩纪末期的白垩纪-第三纪灭绝事件之后。
英语百科
Paleocene 古新世(重定向自Palaeocene epoch)
![]() ![]() ![]() The Paleocene (pronunciation: /ˈpæliəˌsiːn, ˈpæ-, -lioʊ-/; symbol Pε) or Palaeocene, the "old recent", is a geologic epoch that lasted from about 66 to 56 million years ago. It is the first epoch of the Paleogene Period in the modern Cenozoic Era. As with many geologic periods, the strata that define the epoch's beginning and end are well identified, but the exact ages remain uncertain. |
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