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increase in atmospheric pCO2 Brian A. Schubert , A. Hope Jahren DOI : 10.1130 / G36467.1 Published on May 2015(passive) caused bythe Last Glacial Maximum
increase in atmospheric pCO2 Brian A. Schubert , University of Louisiana at Lafayette , Lafayette , Louisiana , USA(passive) caused bythe Last Glacial Maximum
increase in atmospheric pCO2 , " Geology , 43(5(passive) caused bythe Last Glacial Maximum
When South America became attached to North America creating the Isthmus of Panama , the Arctic region cooled due to the strengthening of the Humboldt and Gulf Stream currents[citation neededeventually leadingto the Last Glacial Maximum
increase in atmospheric pCO2Stomatal and(passive) caused bythe Last Glacial Maximum
increase in atmospheric pCO2Climate change(passive) caused bythe Last Glacial Maximum
increase in atmospheric pCO2 , https://doi.org/10.1130/G36467.1(passive) caused bythe Last Glacial Maximum
high - amplitude , rapid climatic oscillationsleadinginto the Last Glacial Maximum
increase in atmospheric pCO2 | Geology Skip to main content Global increase in plant carbon(passive) caused bythe Last Glacial Maximum
the time periodleadingup to the Last Glacial Maximum
the critical periodleadingto the Last Glacial Maximum
increase in atmospheric pCO2AbstractFulltextPDFA 17-My - old whale constrains onset of uplift and climate change in east AfricaAbstractFulltextPDFA synthesis of the theories and concepts of early human evolutionAbstractFulltextPDFWeb of Science(passive) caused bythe Last Glacial Maximum
the climatic declineleadingto the last glacial maximum
Ice Age Climate Puzzle SolvedCausedthe Last Glacial Maximum
From a loess - paleosol section in western Kentucky , stratigraphic changes in gastropod assemblages imply climatic cooling at 29 ka and again at 27 kaleadinginto the last glacial maximum
severe climatic stressleadingup to the Last Glacial Maximum
the growth phase of the Laurentide Ice Sheetleadinginto the Last Glacial Maximum
the ~15,000 yearsleadinginto the Last Glacial Maximum
the 15 kyrleadinginto the Last Glacial Maximum
the falling sea levelleadingup to the Last Glacial Maximum
the increased aridityleadingto the last glacial maximum
the last glacial cycleleadingup to the Last Glacial Maximum
that extinctions took placeleadingup the Last Glacial Maximum ( LGM
December 2007eventually leadingto the Last Glacial Maximum
a north - flowing West Australian Current(passive) caused bythe Last Glacial Maximum
Such eventsledto the Last Glacial Maximum
the temperature fluctuationsleadingup to the Last Glacial Maximum
the deteriorationwould resultin the Last Glacial Maximum
increasing aridityleadingup to the Last Glacial maximum
individuals recruited from multiple nesting beaches of Atlantic Ocean(passive) composed bythe Last Glacial Maximum
CO2 starvation(passive) are caused bylast glacial maximum
extreme aridityleadingup to the Last Glacial Maximum
The expansion of modern humans to the American continent afterledthe Last Glacial Maximum
two other reef - death events — one 17,000 years ago and another 13,000 years agotriggeredtwo other reef - death events — one 17,000 years ago and another 13,000 years ago
widespread depopulation of Northern Europe , the subsequent repopulation as the ice retreated marked the start of the Mesolithic eracausedwidespread depopulation of Northern Europe , the subsequent repopulation as the ice retreated marked the start of the Mesolithic era
to community - wide population expansion in a montane songbird radiation in highland Papua New Guinea Sustainability , Vol . 12 , Pages 5603ledto community - wide population expansion in a montane songbird radiation in highland Papua New Guinea Sustainability , Vol . 12 , Pages 5603
these early human groups to seek refuge at the southern margins of the continentpromptedthese early human groups to seek refuge at the southern margins of the continent
approximately 17,000 years agoresultedapproximately 17,000 years ago
to a 120 m rise in sea levelcontributedto a 120 m rise in sea level
in between 25,000 and 19,500 years agosetin between 25,000 and 19,500 years ago
greater mobility and more extended social networks than among previous hominin populationsmay have triggeredgreater mobility and more extended social networks than among previous hominin populations
to their eventual demiseledto their eventual demise
to its extinctionledto its extinction
in retreating knickpoints and where he is using cosmogenic isotopes to look at the erosion rates of bedrock rivers above and below the knickshas resultedin retreating knickpoints and where he is using cosmogenic isotopes to look at the erosion rates of bedrock rivers above and below the knicks
in lower levels of genetic diversity in temperate and polar regionshas resultedin lower levels of genetic diversity in temperate and polar regions
to greater deposition of loessledto greater deposition of loess
the temperature decrease(passive) caused bythe temperature decrease
to a massive retreat of tropical forests in Central Africaledto a massive retreat of tropical forests in Central Africa
population diminish lce sheetscreatespopulation diminish lce sheets
the arid phase(passive) caused bythe arid phase
the global carbon cycle through time Since the Last Glacial Maximum ( LGMinfluencedthe global carbon cycle through time Since the Last Glacial Maximum ( LGM
“ resource legacies ” seen today as gradients of biogeochemical properties in soils and lakeshave created“ resource legacies ” seen today as gradients of biogeochemical properties in soils and lakes
to the extensive spread of deserts and sand dunes in low latitudes ( Sarnthein , 1978leadingto the extensive spread of deserts and sand dunes in low latitudes ( Sarnthein , 1978
to current global patterns of specieshas contributedto current global patterns of species
a differential load across coastlines globallycreatea differential load across coastlines globally
from the deserts of eastern Asiaoriginatedfrom the deserts of eastern Asia
in a dramatic change in photic conditions from a completely dark cave environment to that of an epigean freshwater lake environment , in which K. crenarum , as an adaptation to the presence of light , may have regained some of its body pigmentationresultedin a dramatic change in photic conditions from a completely dark cave environment to that of an epigean freshwater lake environment , in which K. crenarum , as an adaptation to the presence of light , may have regained some of its body pigmentation
the archaeological clock ticking for Scotlandsetsthe archaeological clock ticking for Scotland
population bottleneckscausingpopulation bottlenecks
to a concentration of more people in less spaceledto a concentration of more people in less space
this region as a likely refugium , and bolsters the probability to the range expansion and secondary contact of haplotype of a refugium in the Tamaulipan region , thought to have lineageshas leadthis region as a likely refugium , and bolsters the probability to the range expansion and secondary contact of haplotype of a refugium in the Tamaulipan region , thought to have lineages
in much of southwest Africaresultedin much of southwest Africa
Pollen in small denominations(passive) is discoveredPollen in small denominations
in distributional gapsresultingin distributional gaps