Although the authors of this journal are economists rather than paleo or megafauna experts, they do make an important point about considering the behavioural incentives facing early human hunters and not simply portraying them to be the mechanistic 'superpredators' of most overkill models.
Sunday, 28 October 2012
I came across an interesting journal article the other day about introducing a behavioural economics perspective to megafauna extinction. This journal is interesting not only to me as an Economics and Geography student, but also because it suggests the value of an inter-disciplinary perspective to environmental geography. In the 2005 paper ‘Megafauna Extinction: A Paleo-economic Theory of Human Overkill in the Pleistocene’, Bulte et al argue that previous scientific models of overkill concentrated only on megafauna as prey for humans, while ignoring the entire opportunity set facing the human hunters, which is the presence of substitute foods and behaviours. One of these is hunting small animals or minifauna.
Bulte et al have designed a model which suggests that counter intuitively, hunting minifauna was essential to the overkill hypothesis. Minifauna supported human populations and allowed humans to reach critical densities which were large enough to wipe out megafauna. Besides, hunting minifauna enabled more chance encounters with megafauna. Complementing last week’s post, they suggest that the harsh environmental conditions of the late Pleistocene may have triggered humans to engage in minifauna hunting rather than more benign activities like agriculture. Minifauna did not go extinct because they breed much more quickly than slow-breeding megafauna.
This echoes modern day poaching behaviour in Africa. Poachers often hunt both rhinos and elephants, and not only the more valuable rhino ivory alone, because the probability of encountering rhinos is much smaller, making sole rhino hunting a loss-making activity. Thus, poachers also hunt the relatively more abundant elephants, taking rhinos as a bonus. Thus, elephant hunting is what economists call a ‘complementary’ activity to rhino hunting, in the same way as hunting minifauna was complementary to hunting megafauna for early humans.
Saturday, 20 October 2012
The late Pleistocene extinction of megafauna in North America was a unique event as previously, species that became extinct were small mammals. In the Pleistocene interglacial, extinction was almost entirely confined to large mammals (>1,000 kg) and medium-large ones (100 – 1,000kg) (Stuart 1991). North America lost 35 out of 45 megafauna genera during the Pleistocene (Grayson 2007: See Table).
|Grayson (2007): Table of Extinct Megafauna of the Late Pleistocene|
|National Geographic (2011): CT scan showing cross-section of the broken tip of a spear embedded in a mastodon's rib (dated 13,800 years ago)|
Grayson and Meltzer (2002) argue against this generally accepted view of human predation driving megafauna extinction. They show that only 15 of the 35 genera that were supposedly killed by Clovis hunters actually survived to 11,000 radiocarbon years ago, which is when they would have encountered Clovis hunters. Besides, megafauna extinction in North America is by no means a unique phenomenon. The entire Northern Hemisphere experienced substantial species extinctions around 10,000 – 11,000 radiocarbon years ago. In Eurasia for example, many megafauna like reindeer, giant deer and mammoth also disappeared around the same time as those in North America did. Woodman et al (1997) support the view that humans cannot be blamed for giant deer extinction in Ireland as there were no people there during that time.
The reasons for why climate change has been rejected as a cause of megafauna extinction are encapsulated in Fiedel’s (2009:30) question: “if Holocene warming was so disastrous for megafauna, why wasn't there a wave of extinction around 125 ka in the last interglacial?” There are 2 arguments proponents of the climate change explanation use. The first is that the last interglacial was much warmer than previous interglacials and had fewer seasonal temperature variations, leading to mosaic vegetation types that supported a richer range of animal species (Graham and Lundelius 1984). When the open grasslands of the late Pleistocene gave way to thicker forests and vegetation which showed strong zoning according to climate during the Holocene, animal extinctions occurred as the less diverse vegetation could no longer support the previous level of biodiversity (Stuart 1991). Graham (1985) has also argued that the Pleistocene – Holocene transition was unique from previous transitions. Not only was Holocene climate and vegetation was very different from that of previous interglacial periods, but also unusually, the last interglacial was warmer, rather than cooler, than the Holocene in both North America and Europe.
The second is that the late Pleistocene was biotically unique. Scott (2010) argues that this assumes a static view of megafauna composition and hence, similar adaptations to climate change. He uses the example of bison becoming more widespread in North America. Guthrie (1980) proposed that since bison survived while other species perished during this period, this may suggest that competition from bison, along with failure to adapt to climate change, drove the megafaunal extinction event. Nevertheless, the key takeway from Scott’s paper is that ‘megafauna’ is not a static concept, and this has implications for evolutionary responses to climate change. This squares with Graham and Lundelius’ (1984) theory of ‘coevolutionary disequilibrium’ – species evolve individualistically and uniquely to climate change in ways that may become detrimental to other species.
Additionally, during 10,000 years of the Holocene very few land mammals became extinct, although human populations certainly increased dramatically (Stuart 1991).
Nevertheless, the extinctions in North America were definitely more sudden and severe than in Europe. The North American case supports the view of a greater, but not dominant, human role in extinction in relation to other regions. The arrival of Clovis hunters (not present in Europe) at a time of more profound climate change was probably the last straw for many species already suffering the stress from a changing environment.
|The Modern Elephant and its Prehistoric Cousins - A Similar Fate?|
Thursday, 11 October 2012
Woolly mammoths, sabre-toothed tigers and other Pleistocene megafauna roamed the Earth, forming a vital part of natural ecosystems. Today, they occupy no more than a CGI-manipulated place in the popular imagination, with appearances in natural history museums, animated movies and even in the hit TV series Game of Thrones as the dire wolf. How these mighty beasts have fallen!
Natural climate change was long thought to be behind their extinction, but recent studies have pointed to a new culprit: Man. Although Man cannot be solely held responsible, evidence suggests that early humans played a precipitating role in megafauna extinction which complemented the effects of climate change, at least in a fair number of continents like North America, Eurasia and Australia. Indeed, even in his less-than-glorious past, with his primitive weapons and small numbers, Man has managed to sound the death knell for these powerful creatures. With Man’s impact on biodiversity tremendously larger today, the prospects for today’s megafauna - elephants for example – are dire.
That said, important lessons abound for modern conservation from the unfortunate fate of these vanished giants. Human-induced climate change and human impacts on the natural environment are ever greater today, and the past has shown that these two factors have decimated two thirds of megafauna genera between 50,000 and 10,000 years ago – 40,000 years is merely the blink of an eye in geological time.
This blog explores the role of Man in Pleistocene megafauna extinctions and bridges the lessons of the past with the implications for contemporary conservation efforts.