In 1993, after three summers of trudging across the barren rust colored hills and deep sands of Mongolia's Gobi Desert, paleontologist Mike Novacek and a team of researchers from the American Museum of Natural History stumbled upon one of the richest fossil bed ever found. The site, known as Ukhaa Tolgod, produced countless skeletons of Velociraptors, several species of dinosaur embryo fossils, hard-to-find fossils of the bird-like Mononykus, and skulls of Mesozoic mammals.
 

New fossils are eroded out of the Gobi's sandstone every year. This scientist from the American Museum of Natural History stands in front of the type of rock formations which frequently contain fossils. (Courtesy American Museum of Natural History)

Since their big discovery, the researchers have traveled back to the Gobi every summer to locate additional sites and to work Ukhaa Tolgod. (see map.) Despite the scientists’ experience and their earlier success, locating potential fossil beds in the Gobi continues to be a difficult task. The desert is vast and inhospitable with few roads, harsh winds, and 100-degree (Fahrenheit) temperatures. Maps are often inaccurate and trails are unmarked. Traipsing about looking for these outcrops of reddish-brown sandstone where fossils are often found requires an enormous amount of time and money.

Recently, in an effort to improve their chances, the museum researchers have turned their attention to orbiting satellites. Using the images these satellites produce of the Earth, Novacek and his team have found a way to locate potential fossil beds before they even set foot in the desert. Already their efforts uncovered one site last year that produced several good specimens. In the future they hope the images will not only cut down on the time they spend trekking around the desert, but will also ensure that they never stop retrieving remarkable specimens from the reddish-brown sandstone of the Gobi.

 A Layered Past

The data used in this study are available in one or more of NASA's Earth Science Data Centers.

Mongolia lies between eastern Russia and China. The Gobi Desert covers the southern half of the country and parts of northern China. (map detail) (Map by Robert Simmon)

Most of the fossils found in southern Mongolia represent animals that lived some 80 million years ago in the late Cretaceous Period. This was some 15 million years before the dinosaurs became extinct and when the Velociraptor and the shield-headed Protoceratops roamed the Earth. Paleontologists believe that the area now known as the Gobi Desert, though primarily arid, also contained marshy areas and ponds created by water run-off from the surrounding mountains. Enough vegetation grew then to support a wide variety of dinosaurs, lizards, and mammals (Loope et al., 1998).

These animals were trapped and buried in sediments in a number of different ways during the late Cretaceous Period. Some were taken by flash floods and were buried in flood plains. Some drowned in lakes and were covered by silt. Still others were swallowed by sandstorms. However, Novacek explains, the best-preserved fossils from Ukhaa Tolgod came about as a result of collapsing sand dunes. Stable, non-drifting sand dunes formed at and around the marshlands and small ponds back then. "The dinosaurs would hunker down in these dune fields and make their nests," said Novacek. Sometimes the dunes, which were often many stories high, would become unstable. During a heavy rain, the top layers of sand on the dune would slide down its sides like an avalanche, catching dinosaurs unaware below and covering them instantly as they were nesting, fighting, or collecting food (Loope et al., 1998).
 

This paleontologist is excavating a dinosaur fossil in Mongolia. The fossil may have been created when the dinosaur's corpse was covered by drifting sand, or the dinosaur may have ben buried alive by a collapsing sand dune. (Courtesy American Museum of Natural History)

Over time, layers upon layers of sediments built up on top of these dunes. Under the intense pressure of these additional strata, the sand dunes turned to red sandstone and the bones within fossilized. Millions of years later, continental uplift and erosion from water and wind brought the fossils back to the surface. The climate in this region became even more arid and sparsely vegetated, making the fossils easy to find.
 

Throughout the twentieth century, the red sandstone fossil beds yielded the finest specimens of both late Cretaceous dinosaur and mammal fossils in the world. In the 1920s while searching for human fossil remains, Roy Andrews, a paleontologist at the American Museum of Natural History, made the first big Gobi fossil discovery at a locality known as the Flaming Cliffs. Here he found a fossilized dinosaur nest as well as the first known skeletons of the infamous Velociraptor. For the 60 years that followed, during the time that Mongolia was under communist rule, researchers from Poland and Mongolia trekked further into the desert, turning up, among other things, a fossil of an Oviraptor in a fight to the death with a Protoceratops (Webster, 1996).

The museum resumed its campaigns shortly after the Soviet Union break up. Under the direction of Novacek, paleontologists uncovered the greatest Gobi fossil beds to date around an area known as Ukhaa Tolgod. "In this four-square-kilometer area we've found probably as many specimens as have been found in the rest of the Gobi combined," says Novacek. He explains this site has not only given them great specimens of fossils, but insights into the evolution of mammals and how dinosaurs raised their young. An Oviraptor skeleton they retrieved, for instance, shows that dinosaurs took care of their eggs in much the same way that birds do today (Norell et al., 1995). Well-preserved mammal skeletons dug up at the site have helped scientists fill in branches of the evolutionary tree that perhaps led to our existence.

 Using Satellites to Unearth Fossils
 Finding Fossils from Space

The protoceratops was one of the first dinosaurs discovered in the Gobi, by Roy Andrews. [(Negative #312326)/(Julius Kirschner)/Courtesy Dept. of Library Services, American Museum of Natural History]

Each year the winds and harsh winters of the Gobi peel away additional layers of the red sandstone at Ukhaa Tolgod, exposing more fossils. Every summer since 1993 researchers from the museum have traveled back to the site, and they've continued to find remarkable specimens. Despite their success, the paleontologists still believe that there may be undiscovered sites just as good or even better in other parts of the desert. So when Novacek and his team make their yearly pilgrimage, they also take time to search for new fossil beds.
 

In general, the fossil-bearing red sandstone can be found in bluffs and outcrops of eroded sedimentary rock. After the scientists locate a potential site either by chance, by map, or by word of mouth, they go to the area and poke around until they see enough evidence of good fossils to start digging. "But locating these sites is often very difficult," says Novacek. They are dispersed across the vast desert and topographic and geologic maps of the Gobi aren't always accurate. Novacek explains that driving around the Gobi looking for sites that may or may not be there isn’t always the best idea. Hundred-degree temperatures and sandstorms are common in the Gobi. There are no gas stations or super markets along the way, so the scientists have to bring large, unwieldy supply and gas trucks with them. Once, while heading for a site they knew existed in the western Gobi, the team had to go off road. They got mired in a large expanse of sand and had to dig out the supply trucks and gas tanker twenty-one times in one day. "I want to know exactly where we are going before I take a column down there," said Novacek.
 

In order to find new sites and pinpoint ones they know exist, Novacek and the other fossil hunters at the American Museum of Natural History started using images of the Gobi Desert retrieved from the Landsat 5 satellite. This satellite, launched by NASA in 1984, moves in a near-circular orbit very nearly from pole-to-pole around the Earth and scans strip after strip of our spinning planet. A sensor array onboard known as the Thematic Mapper has seven different types of detectors, which acquire images of different wavelengths of reflected sunlight or emitted thermal radiation from the surface of the Earth. One light detector records only the blue light coming off the Earth (band 1), another observes all the yellow-green light (band 2), and still another picks up on thermal radiation (band 7). These data are then beamed back to the planet's surface where they can be made into detailed images of the Earth's surface. Scientists can mix and match the various bands into a single image to highlight various aspects of a section of land. For instance, vegetation in a region can be highlighted by combining the blue, near-infrared, and red bands of the Thematic Mapper data. (View a comparison between true color and infrared false color Landsat data.)
 

This true color Landsat 5 image of the Gobi desert covers an area between Ukhaa Tolgod and the Flaming Cliffs, two of Mongolia's most famous fossil sites. Landsat data are more accurate than existing maps of the region, so they are extremely helpful in the search for fossils.

Unfortunately, there is no simple combination of bands that will immediately pinpoint the fossil sites in the Gobi. Novacek explains that the best they can do is combine blue, near-infrared, and thermal radiation bands on the images of the desert. Together these bands show the rock formations of the Gobi in the most detail. "We then look for the outcrops with the right features and contours," he says. After years of dealing with the geology of the Gobi, Novacek and his team have developed a sense for what types of rock formations will yield fossils and how to spot them on an image. Though there are no hard and fast rules for identifying fossil-bearing outcrops, he explains they are usually found at the base of the larger mountains that run through the Gobi. These outcrops also contain layers of sedimentary rock, and they are well-weathered, low-lying, and sparsely vegetated. All of these aspects can be detected in the satellite images.

So far, Novacek says they have had some success using these Landsat images. Last year, in fact, they tracked down one such site northeast of Ukhaa Tolgod and visited it on their yearly campaign. While it was nothing like Ukhaa Tolgod, he says they did find a few well-preserved, fossilized mammal skulls as well as some partial fossils of dinosaurs. The find gives him confidence that in the future the maps will be useful in tracking down both new sites as well as confirming sites shown on the questionable older maps of the Gobi. "And more than anything they will save us many days of driving across the desert," he says.

References
Loope, D. B., L. Dingus, C. C. Swisher, and C. Minjin, 1998: Life and death in a late Cretaceous dune field, Nemegt Basin, Mongolia, Geology, 26(1), pp. 27-30.

Norell, M. A., J. M. Clark, L. M. Chiappe, and D. Dashzeveg, 1995: A Nesting Dinosaur, Nature, 378, 21/28 December, pp. 774-776.

Webster, D., 1997: Dinosaurs of the Gobi: Unearthing a fossil trove, National Geographic, July 1996, pp. 73-89.

Links
The American Museum of Natural History

 A Layered Past

This image uses Landsat band 7 (shortwave infrared) for red, band 4 (near infrared) for green, and band 1 (blue) for blue. Vegetation and different types of rock and soil stand out much more clearly in this image, enabling fossil hunters to find likely fossil sites. (View a comparison between true color and infrared false color Landsat data.) (Images by Barbara Summey, NASA GSFC Visualization Analysis Lab, based on Landsat 5 data provided by the Laboratory for Terrestrial Physics)