The application of the alkenone organic proxy to the study of Plio-Pleistocene climate

2018 ◽  
pp. 539-562 ◽  
Author(s):  
K.T. Lawrence ◽  
T.D. Herbert ◽  
P.S. Dekens ◽  
A.C. Ravelo
Keyword(s):  
Pleistocene Climate

ONSET OF PLEISTOCENE CLIMATE GENERATED A PULSE OF COARSE SEDIMENT, PRESERVED AS THE SHARPYLDAK FORMATION IN THE TIEN SHAN RANGE OF KYRGYZSTAN

2016 ◽  
Author(s):  
Nyle Major Weldon ◽  
◽  
Ray J. Weldon ◽  
Win N.F. McLaughlin ◽  
Samantha S.B. Hopkins ◽  
...  
Keyword(s):  
Tien Shan ◽  
Coarse Sediment ◽  
Pleistocene Climate

scholarly journals Late Pleistocene climate induced changes in paleo-vegetation in Borneo: Possible implications to human divergence

2021 ◽  
Vol 267 ◽  
pp. 107109
Author(s):  
Zaibao Yang ◽  
Yanli Lei ◽  
Yair Rosenthal ◽  
Tiegang Li ◽  
Zhimin Jian
Keyword(s):  
Late Pleistocene ◽  
Pleistocene Climate ◽  
Induced Changes

scholarly journals A rapid loss of stripes: the evolutionary history of the extinct quagga

2005 ◽  
Vol 1 (3) ◽  
pp. 291-295 ◽  
Author(s):  
Jennifer A Leonard ◽  
Nadin Rohland ◽  
Scott Glaberman ◽  
Robert C Fleischer ◽  
Adalgisa Caccone ◽  
...  
Keyword(s):  
South African ◽  
Dna Sequences ◽  
Evolutionary History ◽  
Climate Changes ◽  
Rapid Loss ◽  
Mt Dna ◽  
Pleistocene Climate ◽  
Equus Burchelli ◽  
History Of ◽  
Plains Zebra

Twenty years ago, the field of ancient DNA was launched with the publication of two short mitochondrial (mt) DNA sequences from a single quagga ( Equus quagga ) museum skin, an extinct South African equid ( Higuchi et al . 1984 Nature 312 , 282–284). This was the first extinct species from which genetic information was retrieved. The DNA sequences of the quagga showed that it was more closely related to zebras than to horses. However, quagga evolutionary history is far from clear. We have isolated DNA from eight quaggas and a plains zebra (subspecies or phenotype Equus burchelli burchelli ). We show that the quagga displayed little genetic diversity and very recently diverged from the plains zebra, probably during the penultimate glacial maximum. This emphasizes the importance of Pleistocene climate changes for phylogeographic patterns in African as well as Holarctic fauna.

Emergence of critical climate states during the Pleistocene

2021 ◽  
Author(s):  
Nicholas Golledge
Keyword(s):  
Dynamical Systems ◽  
Late Pleistocene ◽  
Dominant Frequency ◽  
Climate System ◽  
Ice Age ◽  
Early Pleistocene ◽  
Glacial Cycles ◽  
Pleistocene Climate ◽  
System Nodes ◽  
Systems Framework

<p>During the Pleistocene (approximately 2.6 Ma to present) glacial to interglacial climate variability evolved from dominantly 40 kyr cyclicity (Early Pleistocene) to 100 kyr cyclicity (Late Pleistocene to present). Three aspects of this period remain poorly understood: Why did the dominant frequency of climate oscillation change, given that no major changes in orbital forcing occurred? Why are the longer glacial cycles of the Late Pleistocene characterised by a more asymmetric form with abrupt terminations? And how can the Late Pleistocene climate be controlled by 100 kyr cyclicity when astronomical forcings of this frequency are so much weaker than those operating on shorter periods? Here we show that the decreasing frequency and increasing asymmetry that characterise Late Pleistocene ice age cycles both emerge naturally in dynamical systems in response to increasing system complexity, with collapse events (terminations) occuring only once a critical state has been reached. Using insights from network theory we propose that evolution to a state of criticality involves progressive coupling between climate system 'nodes', which ultimately allows any component of the climate system to trigger a globally synchronous termination. We propose that the climate state is synchronised at the 100 kyr frequency, rather than at shorter periods, because eccentricity-driven insolation variability controls mean temperature change globally, whereas shorter-period astronomical forcings only affect the spatial pattern of thermal forcing and thus do not favour global synchronisation. This dynamical systems framework extends and complements existing theories by accomodating the differing mechanistic interpretations of previous studies without conflict.</p>

Pleistocene Climate

Science ◽  
1981 ◽  
Vol 214 (4525) ◽  
pp. 1076-1076
Author(s):  
Madeleine Briskin
Keyword(s):  
Pleistocene Climate
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