Eurasia (Eurasia and Northern
Asia) lost 35% of its megafauna during the late Pleistocene, relatively fewer
than North America and Australia. Extinction patterns here differed from those
in North America; not all the extinctions occurred synchronously at the end of
the Pleistocene (Grayson 2007). For example, mammoths disappeared from many parts
of Eurasia at around 12,000 radiocarbon years ago, but lasted as late as 4,000
radiocarbon years ago on Wrangel Island. Similarly, giant deer disappeared from
Southwestern France between 12,000 and 11,000 radiocarbon years ago but not
from western Siberia until 7,000 years ago Stuart et al 2004).
The consensus is that Man was
unlikely to have caused megafauna extinction in Eurasia, as the first modern
humans (with sophisticated hunting tools) entered Eurasia around 50,000 radiocarbon
years ago, and there were no apparent extinctions then (Grayson 2007). However,
Stuart (1999) argues that the human role in Eurasia is not insignificant. For
example, according to radiocarbon-calibrated pollen profiles, vegetation able
to support mammoth was present more than 1,000 radiocarbon years after these
animals disappeared in the region, weakening the argument that environmental
change was the sole cause of extinction. Instead, he suggests that the
asynchronous nature of extinction in Eurasia could mean that extinctions only occurred
when animal populations were already undergoing significant stress from climate
change, and human hunting provided the last straw. This probably also explains
why there were 2 distinct waves of extinction in Eurasia which coincided with
periods of climate change (40,000 to 20,000 radiocarbon years before present
and 14,000 to 10,000 radiocarbon years before present), the latter of which is
the focus of this blog.
While Stuart’s argument is
convincing, I think an interesting counterargument can be found in Anthony Barnosky’s
1986 paper. He argues that Irish deer, which became extinct at around 10,000 to
12,000 radiocarbon years ago, before the arrival of humans in Ireland, were
wiped out not by Holocene warming but a brief cold spell just before warming.
This cold spell shortened feeding seasons for the Irish elk, which were also
unable to migrate to any refugia quickly enough as Ireland is an island. The
evidence is in lake sediment layers where pollen records suggest changes in
vegetation associated with colder weather and fewer elk bones, during a period
called the Nahanagan Stadial. He suggests that the accumulation of many local
causes of extinction could have led to the total extinction of megafauna. Nevertheless,
more work remains to be done on this fascinating hypothesis.
Figure 1: Irish Elk |
Finally, I return to a discussion
of the climate change that occurred during the late Pleistocene. In my previous
blog post ‘Humans in the Wild West’, I discussed research showing that the late
Pleistocene-Holocene glacial transition was unique in the Northern Hemisphere
compared to other previous interglacials, both in climate and biological terms.
This caused megafauna extinction due to climate unsuitability. Nogues-Bravo et
al (2008) constructed a model which shows this for one species – the woolly
mammoth in Europe.
Figure 2: Maps of Projected
Climatic Suitability for the Woolly Mammoths in the Late Pleistocene and
Holocene (Nogues-Bravo et al 2008)
The increasing intensities of red
show increasing suitability of mammoth habitat while increasing intensities of
green show decreasing suitability. Black dots show mammoth presence while black
lines show the northern limit of early humans. The figure shows that climate
and habitat suitability for mammoths decreased during the late Pleistocene.
Although humans did move Northwards, their presence did not seem to affect
mammoth presence as drastically as habitat suitability; even in areas untouched
by humans (north of black line), mammoth populations declined as habitat
suitability decreased.
The causes of megafauna
extinction in Europe are certainly extremely complex. Climate change appears to
be the main culprit, since human populations coexisted with megafauna for over
50,000 radiocarbon years while accelerated extinctions only occurred in 2
distinct phases which were periods of distinct climate change. Extinctions in
at least some specific geographical locations, such as the Irish elk in
Ireland, were certainly distinct from the role of humans.
References
Barnosky, A.
(1986) “Big game” extinction caused by late Pleistocene climatic change: Irish
elk (Megaloceros giganteus) in Ireland’, Quaternary
Research, Vol. 25, 1, pp. 128-135
Grayson, D.
K. (2007) ‘’Deciphering North American Pleistocene extinctions’’, Journal of Anthropological Research, Vol.
63, No. 2, pp. 185-213
Nogues-Bravo,
D. et al (2008) ‘’Climate change, humans and the extinction of the woolly
mammoth’’, PLOS Biology, 6(4), e79
Stuart, A. J. (1999). Late Pleistocene megafaunal extinctions
in MacPhee, R. D. E. (ed.) Extinctions in Near Time: Causes, Contexts, and
Consequences, New York: Plenum, pp. 257-269.
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