ライフサイエンスコーパス: snowball earth

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1 eomagnetic studies, possibly resulting in a 'snowball Earth'.

2 A Paleoproterozoic snowball Earth at 2.4 Giga-annum before present (Ga) imm

3 Termination of such 'hard snowball Earth' climate states has been proposed to proc

4 al intervals of intense, global glaciation ("snowball Earth" conditions) during Precambrian time.

5 oterozoic low-latitude glaciation, known as 'snowball Earth', could have been periods of intense dive

6 alaeomagnetic latitudes can be explained by 'snowball Earth' episodes, high orbital obliquity or mark

7 initiation mechanism of these Neoproterozoic Snowball Earth events has remained a mystery, the broad

8 low-latitude glaciation, which are probable "Snowball Earth" events.

9 biogenic evolution, polar paleo climatology, snowball earth geology, and present day atmospheric scie

10 Neoproterozoic oxygen increase and Sturtian Snowball Earth glaciation, which accompanied emplacement

11 The snowball Earth glaciations and Neoproterozoic oxidation

12 oic Earth was punctuated by two low-latitude Snowball Earth glaciations.

13 period ( 720-635 Ma) is marked by extensive Snowball Earth glaciations.

14 n the aftermath of widespread, low-latitude 'snowball Earth' glaciations.

15 ore the approximately 2.3-2.2 Ga Makganyene "snowball Earth" (global glaciation).

16 ts and intense silicate weathering in a post-Snowball Earth hothouse.

17 most of the past two billion years, and the snowball Earth hypothesis accordingly remains the most v

18 nmental disturbance than that implied by the snowball Earth hypothesis.

19 tra-high CO2 concentrations proposed by the "snowball' Earth hypothesis produce a typical MOSD durati

20 ides important constraints for parts of the "Snowball Earth" hypothesis.

21 Our finding is consistent with the 'snowball Earth' hypothesis and/or a massive methane rele

22 ave extended well down into the tropics-the 'snowball Earth' hypothesis-or the present zonation of cl

23 millions of years during such ice ages--the 'snowball Earth' hypothesis.

24 s in Earth history, the end of the Marinoan 'snowball Earth' ice age, approximately 635 Myr ago.

25 In any case, a snowball Earth is a precondition for the observed MOSD e

26 na that are expected to be significant in a 'snowball Earth' scenario, but which have not been consid

27 rather narrow escape from a fully glaciated Snowball Earth state given the low levels and large fluc

28 and that trophic complexity survived through snowball Earth times.

29 tion would have resulted in a warming of the snowball Earth to extreme greenhouse conditions.

30 To simulate a snowball Earth, we use only a reduction in the solar con

31 explained by a global glaciation (that is, a snowball Earth), which ended abruptly when subaerial vol

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