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Botkin Environmental Science Earth as Living Planet 8th txtbk

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106 CHAPTER 6 The Biogeochemical Cycles<br />

Oil and g<strong>as</strong> is transported<br />

below and on top of<br />

the water by ocean<br />

current and<br />

wind<br />

Wind and current<br />

Air<br />

Water<br />

Seabed<br />

Folded rock<br />

(anticline)<br />

(a)<br />

Deposition of oil<br />

on seabed is<br />

degraded by<br />

microbes<br />

Microbes consume oil and g<strong>as</strong><br />

in water column and oil on<br />

seabed (often in a mat)<br />

Fracture (fault) oil<br />

and g<strong>as</strong> (bubbles)<br />

move up<br />

(b)<br />

FIGURE 6.2 (a) Idealized diagram of physical, chemical, and biological processes with shallow methane<br />

and oil seeps; (b) small bubbles of methane (~1 cm) from a seep at Coal Oil Point on the seabed; and<br />

(c) methane bubbles (~1 cm) at the surface. (Photographs courtesy of David Valentine.)<br />

(c)<br />

6.1 <strong>Earth</strong> Is a Peculiar<br />

<strong>Planet</strong><br />

Our planet, <strong>Earth</strong>, is unique, at le<strong>as</strong>t to the extent that<br />

we have explored the cosmos. In our solar system, and<br />

in the Milky Way galaxy to the extent that we have<br />

observed it, <strong>Earth</strong> is the only body that h<strong>as</strong> the combination<br />

of four characteristics: liquid water; water at its<br />

triple point (g<strong>as</strong>, liquid, and solid ph<strong>as</strong>es at the same<br />

time); plate tectonics; and life (Figure 6.3). (Recent<br />

space probes to the moons of Jupiter and Saturn suggest<br />

that there may be liquid water on a few of these<br />

and perhaps also an equivalent of plate tectonics. And<br />

recent studies of Mars suggest that liquid water h<strong>as</strong><br />

broken through to the surface on occ<strong>as</strong>ion in the p<strong>as</strong>t,<br />

causing <strong>Earth</strong>like water erosion.)<br />

The above discussion leads to consideration of<br />

the history of <strong>Earth</strong> over billions of years. This h<strong>as</strong><br />

prompted some geologists to propose “big history”—<br />

to link contemporary history with geologic history,<br />

perhaps even going back all the way to the Big Bang

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