Page 308 - Earth's Climate Past and Future
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284     PART V • Historical and Future Climate Change


        15-6 Did Humans Cause Megafaunal Extinctions?       south of the ice sheets by high summer insolation, reduc-
                                                            tion of habitat in the cooler north by the slow retreat of
        Populations of large mammals, called  megafauna,    the ice sheet, and unusual (no-analog) mixtures of vege-
        decreased drastically late in the most recent glacial oscil-  tation that developed as forests and grasslands shifted
        lation. Prior to 50,000 years ago, more than 150 genera  from their glacial positions to their modern locations.
        of mammals larger than 45 kg (~100 pounds) existed. By  Critics of this climatic hypothesis note that no
        10,000 years ago, 50 or fewer genera were left. This  comparable pulse of extinction occurred in any of the
        interval of extinctions was unprecedented compared to  50 or so earlier deglaciations. In fact, the number of
        millions of years of prior history.                 species that went extinct near 12,500 years ago exceeds
           During the most recent glaciation, near 50,000 years  the total during all of the previous 2.75 million years.
        ago (within the uncertainties of the dating methods),  The same basic combination of climatic conditions—
        many of the larger marsupials in Australia became   high summer insolation, rising CO levels, and rapidly
                                                                                          2
        extinct within a few millennia, including various kinds  melting ice sheets—had occurred during earlier deglacia-
        of kangaroos and wombats and a lion, as well as non-  tions without causing pulses of extinction. So the critics
        marsupials such as giant tortoises and flightless birds.  ask why the extinctions occurred only during this one
        Just before this time, humans had first entered Australia  deglaciation and not the others.
        from southeast Asia, helped by the exposure of land    Another vulnerability of the climatic hypothesis is
        masses by lowered sea level. These people, who used  the fact that so many mammals throughout the Ameri-
        “fire sticks” to burn grasslands and drive game, have  cas, living in environments that ranged from semiarid
        been proposed as the cause of these extinctions.    grasslands to rain forests, suffered the same fate. Because
           The megafaunal population of the Americas was    these different environments followed different climatic
        very diverse until the late stages of the most recent  paths during deglaciation, climate change cannot possi-
        deglaciation, with a rich array of mammals in North  bly explain all the extinctions.
        America (Figure 15–12). Then, within an interval of a  A second explanation, called the overkill hypothe-
        few thousand years centered on 12,500 years ago, over  sis, put forward by the paleoecologist Paul Martin, is
        half of the large mammal species living in both North  that human hunting caused this extinction pulse. The
        and South America became extinct. The list in North  immediate cause of the extinctions could have been
        America includes giant mammoths and mastodons       either the first arrival of humans in the Americas or the
        (larger than modern elephants), horses the size of mod-  first appearance of a new hunting technology or strat-
        ern Clydesdales, camels, giant ground sloths, saber-  egy among the people already present.
        toothed tigers, and beaver as large as modern bears.   Both the origin and time of arrival of the first
           One explanation for this rapid pulse of extinction is  humans in the Americas were once thought to have
        that major climate changes at the end of the glacial maxi-  been resolved. They supposedly came by land from Asia
        mum created new environmental combinations to which  near 12,500 years ago, during the late stages of the last
        many mammals were unable to adapt. These conditions  deglaciation. They crossed into Alaska over a land
        included strong summer warming and drying of the land  bridge in the Bering Strait exposed by the lower glacial













                                                                           FIGURE 15–12 Mammals of the glacial
                                                                           maximum A rich array of large mammals
                                                                           lived on the North American plains prior
                                                                           to the most recent deglaciation, including
                                                                           several forms that became extinct: woolly
                                                                           mammoths, saber-toothed tigers, and
                                                                           giant ground sloths. (Courtesy of
                                                                           Smithsonian Institution, Washington, DC;
                                                                           painted by Jay Matternes.)
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