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Evolution__3rd_Edition

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..<br />

Number of families<br />

Number of families<br />

(a)<br />

1,000<br />

800<br />

600<br />

400<br />

200<br />

Cm<br />

0<br />

V Ca O S D C P Tr J K T<br />

(b)<br />

1,200<br />

1,000<br />

800<br />

600<br />

400<br />

200<br />

0<br />

V Ca O S D C P Tr J K T<br />

Figure 23.15<br />

The history of global biological diversity. (a) Sepkoski<br />

originally found a logistic increase with a Paleozoic plateau,<br />

followed by a steady increase since the Permian mass<br />

extinction. He also recognized three distinct faunas:<br />

Cambrian (Cm), Paleozoic (Pz), and Modern (Md).<br />

(b) Benton compiled the data in a slightly different way,<br />

. . . or an exponential model ...<br />

Pz<br />

Md<br />

Number of genera<br />

250<br />

200<br />

150<br />

100<br />

50<br />

0<br />

(c)<br />

CHAPTER 23 / Extinction and Radiation 675<br />

Median<br />

95% CI<br />

Ca O S D C P Tr J K T<br />

550 450 350 250 150 50<br />

Time (Myr)<br />

and found a pattern that was indistinguishable from a steady<br />

exponential increase. (c) A new compilation aims to correct<br />

for stratigraphic incompleteness, and preliminary findings<br />

suggest no increase in diversity between the Ordovician<br />

and Tertiary. Redrawn, by permission of the publisher, from<br />

Miller (1998) and Alroy et al. (2002). © 1998 American<br />

Association for the Advancement of Science.<br />

The difference between the Paleozoic and Modern parts of Sepkoski’s graph suggest<br />

that the Permian mass extinction had a major creative influence for life on Earth today.<br />

In the absence of the Permian mass extinction, maybe the Paleozoic fauna would have<br />

continued to dominate life on Earth, and diversity might still be stuck at the Paleozoic<br />

plateau. The “Modern” fauna seems to have been able to diversify more than the<br />

Paleozoic fauna.<br />

A second model a the exponential model afor the history of diversity was proposed<br />

by Benton (1997). He used a different data compilation, including land organisms. He<br />

suspected that Sepkoski’s result, including the Paleozoic plateau, was peculiar to<br />

marine life. If all life is looked at together (Figure 23.15b), the full history of diversity<br />

could just as well be explained by a steady (if noisy) exponential increase. Two implications<br />

of Benton’s model are as follows. First, species have been persistently dividing and<br />

subdividing ecological niches into finer and finer units a if there is a limit on total

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