Rb/Sr GEOCHEMISTRY OF LOESS DEPOSITS IN THE HORQIN DUNEFIELD, NORTHEASTERN CHINA, AND ITS IMPLICATIONS FOR CLIMATE CHANGE DURING LATE QUATERNARY

2014 ◽  
Vol 33 (2) ◽  
pp. 129-136 ◽  
Author(s):  
Shuangwen YI ◽  
Huayu LU ◽  
Yali ZHOU ◽  
Xianyan WANG ◽  
Quanyu LIU
Keyword(s):  
Climate Change ◽  
Late Quaternary ◽  
Northeastern China ◽  
Loess Deposits

Sensitivity of aboveground biomass and species composition to climate change in boreal forests of Northeastern China

2021 ◽  
Vol 445 ◽  
pp. 109472
Author(s):  
Chao Huang ◽  
Yu Liang ◽  
Hong S. He ◽  
Mia M. Wu ◽  
Bo Liu ◽  
...  
Keyword(s):  
Climate Change ◽  
Species Composition ◽  
Aboveground Biomass ◽  
Boreal Forests ◽  
Northeastern China

Quaternary Mammal Communities: Relevance of the Individualistic Response and Non-Analogue Faunas

2005 ◽  
Vol 11 ◽  
pp. 141-158 ◽  
Author(s):  
Russell W. Graham
Keyword(s):  
Climate Change ◽  
Global Climate Change ◽  
Natural Experiment ◽  
Late Quaternary ◽  
Global Climate ◽  
Land Use Management ◽  
Change Analysis ◽  
Climate Fluctuations ◽  
Core Species ◽  
Mammal Communities

Frequent and repeated climate fluctuations of the late Quaternary serve as a “natural experiment” for the response of species to environmental change. Analysis of the FAUNMAP database documents individualistic shifts in the geographic distributions for late Quaternary mammals. However, because the individualistic response is not necessarily random and because many species share similar niche parameters, it is possible that some species appear to form coherent groups of core species. In reality their dispersals are individualistic with regard to rate and timing. The individualistic response of mammals, as well as that of other organisms, has created late Quaternary communities without modern analogues. This concept has profound implications for the design of biological reserves and for land use management with respect to future global climate change. However, the relevance of non-analogue mammal communities has been challenged by Alroy (1999), who claims that non-analogue associations were not common in the Quaternary and that they appeared to occur in both the Pleistocene and Holocene. Reexamination of his analysis shows that he employed a different definition for non-analogue faunas and that his methods of analyses created artificially low counts of non-analogue communities and consequently an underestimate of their importance.

scholarly journals Late Quaternary climate change in the north-eastern highlands of Ethiopia: A high resolution 15,600 year diatom and pigment record from Lake Hayk

2018 ◽  
Vol 202 ◽  
pp. 166-181 ◽  
Author(s):  
Katie L. Loakes ◽  
David B. Ryves ◽  
Henry F. Lamb ◽  
Frank Schäbitz ◽  
Michael Dee ◽  
...  
Keyword(s):  
Climate Change ◽  
High Resolution ◽  
Late Quaternary ◽  
The North ◽  
Quaternary Climate ◽  
North Eastern ◽  
Eastern Highlands

scholarly journals Climate change in the recent geological past and the near future. Predicting its impacts: a Review

2019 ◽  
Vol 55 (1) ◽  
pp. 260
Author(s):  
Constantinos Perisoratis
Keyword(s):  
Climate Change ◽  
Sea Level Rise ◽  
Climatic Change ◽  
Sea Level ◽  
Scientific Community ◽  
Climate Changes ◽  
Late Quaternary ◽  
The Earth ◽  
Geological Past ◽  
Near Future

The climate changes are necessarily related to the increase of the Earth’s temperature, resulting in a sea level rise. Such continuous events, were taking place with minor and greater intensity, during the alternation of warm and cool periods in the Earth during the Late Quaternary and the Holocene periods. However, a particularly significant awareness has taken place in the scientific community, and consequently in the greater public, in the last decades: that a climatic change will take place soon, or it is on-going, and that therefore it is important to undertake drastic actions. However, such a climatic change has not been recorded yet, and hence the necessary actions are not required, for the time being.

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