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Here Be Dragons

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GOING TO EXTREMES<br />

the bottom, that's heterotrophic bacteria, they feed off organic compounds<br />

produced in the upper layers. There's not much oxygen down<br />

there, so they're anaerobic. Instead of breathing oxygen they breathe<br />

sulfur, so to speak. They convert sulfate to sulfide, and that's what's<br />

black."<br />

Taking a few strides off the lake bed and across the highway, we<br />

stand under a rocky cliff, among a pile of rocks that have tumbled<br />

down from Dante's View. <strong>Here</strong> too, the first impression is of total<br />

sterility, but closer inspection reveals the presence of life. An occasional<br />

rock is encrusted with overlapping blotches of yellow or red or<br />

brown or with a branching tracery of black. "Lichen—they're fungi<br />

with algae inside," says McKay. "They can extract moisture from the<br />

air, when the humidity is seventy percent or more. The algae by themselves<br />

need a humidity of at least ninety percent, but the fungus has<br />

some kind of fancy membrane—like Gore-Tex—which lets water<br />

vapor in but doesn't let liquid water out. It's a matter of pore size."<br />

McKay has come to Badwater to install a high-precision thermometer,<br />

which is intended to send a continuous air-temperature reading<br />

back to his office at Ames. The idea is to monitor long-term processes<br />

such as global warming. Badwater held the world's high-temperature<br />

record, at i34°F, until 1922, when a site in the Libyan desert went two<br />

degrees higher. Possibly McKay hopes to wrest the world record back<br />

for the USA.<br />

While he and two junior colleagues attach the device to a post and<br />

program its microprocessor and transmitter, we go off in search of another<br />

ecological niche that McKay has described to us. We soon find<br />

what we're looking for on the pebbly ground north of the lake bed (see<br />

Color Plate i). A small piece of translucent white quartzite looks as<br />

sterile as its darker neighbors, but once flipped on its back, it reveals a<br />

green underbelly—cyanobacteria again. We bring our prize back for<br />

verification. "Yup, hypolith," says McKay. "The stone acts as a moisture<br />

trap. The light comes right through, allowing photosynthesis.<br />

Quartzite stones are a major habitat for life in dry environments all<br />

over the world. They're in the Negev, the Gobi, the Atacama, the outback<br />

of Australia, even Antarctica. If it gets too dry, they go into a dehydrated<br />

vegetative state, and wait it out."<br />

McKay is a biologist whose major interest is in identifying habitats<br />

for life on other planets, especially Mars. Until such time as his employers<br />

provide him with a ticket to the Red Planet, however, he<br />

spends much of his time investigating "extraterrestrial" habitats on<br />

41

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