Showing posts with label Gomphotherium. Show all posts
Showing posts with label Gomphotherium. Show all posts
Friday, February 27, 2015
Barren Cliffs Reveal a Rich and Violent Past: Red Rock Canyon State Park
Deserts have such a fearsome reputation around the world, but deserts can be both beautiful and at certain times of the year a pleasant place to visit. The dry lands of the American Southwest are no exception. For geologists, the treat is made better by the marvelous exposures of barren rock that tell stories of the past when the landscape was very different. This is one of those places: Red Rock Canyon State Park in California. We paid a visit on our way to Death Valley a few weeks ago.
The Garlock fault cuts across the boundary between the Basin and Range province and the Mojave Desert, forming a high linear ridge called the El Paso Mountains. Erosion has stripped away the alluvial cover, exposing the underlying continental sedimentary rocks. The rocks, candy-striped in tones of red, pink and white, formed in a deep basin between 12.5 to 7.5 million years ago, accumulating to a depth of more than a mile. The sediments include arkosic sandstone, siltstone, shale, along with volcanic ash and lava flows recorded several dozen eruptive events. The environment was perhaps semiarid, but certainly wetter than the current day. The fossil record suggests an Upper Sonoran paleobotanical zone, with Black Locust, Mexican pinyon pine, cypress, California live oak, red-root, acacia, desert thorn and palm. Similar plants are found today in the high mountain ridges between San Jacinto and Santa Rosa Peaks in southern California (a region I explored often in my youth).
The steep cliffs have attracted filmmakers for decades, making appearances in all manner of movies, including a lot of westerns, and one of my favorites, the opening scenes of "Jurassic Park". But instead of dinosaurs, paleontologists have discovered a treasure trove of late Cenozoic mammals, reptiles, amphibians, and birds. More than 100 species have been found thus far.
What kinds of animals lived in the western North America around 10 million years ago? It was a diverse ecosystem with many unexpected species for those who think that deer, antelope and buffalo cover all the bases. Thanks to David Whistler, we have a rather comprehensive list of the animals who lived here.
On the open plains, one would have seen two different rhino species, ten species of horse, four kinds of camels, three antelope species, two elephant-like gomphotheres, vultures, two large land tortoises, pika, two ground squirrel species, deer mice, and rabbits.
In the brush covered woodlands, one would have found two oreodonts (extinct sheep-like animals), peccary, three-toed browsing horse, short-legged camel, ringtailed cat, skunk, two weasel-like animals, wolverine, four distinctly different spiny lizards, night lizard, rosy boa, racer snakes, hedgehog, chipmunk, two gopher-like rodents, two different pocket mice, a bat, three small perching birds, mole, four different shrews, a small, rear-fanged snake, and two alligator lizard species.
This rich selection of plant eating animals represented a huge source of walking protein, so there were predators, lots of them. There were six different species of canids (ancestors to the wolves, foxes, and coyotes), a very large bear-like animal, and three large ancestors to the cats including a an early form of sabertooth.
We spent our time learning the basics of stratigraphy, practiced a rudimentary form of geologic mapping, and interpreted the environment of deposition from the nature of the sediments exposed in the cliff. I wandered between groups of working students, answering questions, but my eyes kept ranging across the cliffs, thinking how incredible it is that we live in a time when we can discern the past history of our planet, and in so doing, understanding how we came to be. We are both a part of the Earth's ecosystem, and yet exist outside that ecosystem (for better or worse).
This rich variety of animals in Miocene time occurred because the climate provided rich sources of food, and diversity of the ecosystem was the result. Today, if a climate is not to our liking, we alter the ecosystem to our own ends. We build our shelters, we travel in little cocoons with air-conditioning and stereophonic sound, and we import vast amounts of resources and fuels to maintain our chosen lifestyle. We tend to ignore the other elements of the ecosystem where we live and visit. We don't embrace our environment, we cut ourselves off from it. It's when I'm in a place like Red Rock that I am reminded of where we come from, our ultimate heritage. We are children of the Earth. And there are limits.
Thursday, December 31, 2009
The Other California: Prairies Past and Some Nice Folding
Visitors at Calico Ghost Town in the Mojave Desert geomorphic province are treated to an authentic old mining town complete with bars, melodrama theatres, staged gunfights, and portraits in oldtime clothing. They may even learn a bit of genuine history of the old silver mining district from the occasional sign. Calico is California's Official Silver Rush Ghost Town (discussed in a previous post), and is definitely worth a stop, but not necessarily for the reason envisioned by those who run the park. The parking lot sits in the gulch below the town, and exposes some of the finest folds to be seen anywhere. They have appeared in many geology textbooks ("textbook examples" of anticlines, the upward pointing folds, and synclines, the downward pointing folds).
The origin of these folds has been the subject of much discussion, but their proximity to an active transverse fault (the Calico fault) suggests they developed as a result of transpressional stress. Place a sheet of paper flat on a table, and put your palms on each end. Moving one hand towards you and the other away from you will cause crumpling across the middle. Those crumples are transpressional folds.A bit farther to the west, the Barstow Formation is exposed at Rainbow Basin Natural Area, administered by the Bureau of Land Management. An upside-down rainbow, the Barstow Syncline, is one of the most striking features. I talked about the area in a previous post.
In a marked contrast to the volcanic rocks that make up the core of the Calico Mountains, the Barstow layers are sedimentary rocks. Sedimentary structures such as mudcracks (below) and ripplemarks indicate that the sediments accumulated in a faulted basin in a moderately tropical and occasionally arid environment, essentially similar to the African Savannah of today's world. It was a world of grasslands and palm trees that existed between 13 and 19 million years ago, based on radiometric dates of volcanic ash layers that bracket the sedimentary strata.
An African savannah. Visions of elephants, giraffes, zebras, and rhinos. But not in America, right? Well, time for a new vision. The most stunning aspect of the Barstow Formation is the diversity of fossil species found in its layers. Numerous species of ancestral horses and camels, a rhino ancestor (Aphelops), and an early elephant called a gomphotherium (similar to those big elephants in the Lord of the Rings movie, only much smaller) are among the discoveries. Feeding on these planteaters were one of the earliest cats (Pseudaelurus), an ancestor to the coyotes (Tomarctus), and a probable forebear to the bears and dogs called an Amphicyon (pictured below).The extreme diversity of the fossil assemblage, and the fact that the formation is well-dated led to the establishment of a portion of the geologic time scale called the Barstovian stage of the Miocene epoch, referring to the time period from 16.3 to 13.6 million years ago.
One further aspect of the fossil record in the Barstow Formation are calcareous nodules that contain nicely fossilized insects. Insects are rarely preserved as fossils, but the bugs in the lake sediments were replaced by silica and were supremely preserved, to the extent that even leg hairs are visible.
A technical article from the GSA Bulletin on the Barstow Formation (abstract; full article requires fee or GSA membership)
A nice slideshow about the Barstow Formation and the fossils it contains, from the San Bernardino County Museum.
A nice slideshow about the Barstow Formation and the fossils it contains, from the San Bernardino County Museum.
This has been an entry in the series on the Other California.
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