A Famous Visitor Teresamanera in 1832 Charles Darwin Came Here to Lessed with Fertile Soil and Known to Us Only by Their Fossils
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Volume 29, Number 2 Center for the Study of the First Americans Department of Anthropology April, 2014 Texas A&M University, 4352 TAMU, College Station, TX 77843-4352 ISSN 8755-6898 World Wide Web site http://centerfirstamericans.org and http://anthropology.tamu.edu 6&7 Ancient DNA from bone proves ancestry of First Americans and Native Americans Child burials discovered decades ago on two continents had to wait for genome analysis to unlock their secrets. 16 Dating the earliest petroglyphs in North America in the Nevada desert Tufa deposits from Pyramid Lake and dry Winnemucca Lake give geochemist Benson and anthro- pologist Hattori a gauge for measuring the age of striking “pit and groove” rock carvings. these footprints adds a note of ur- gency to this story. Tracks of birds and footprints of Megatherium at the Pehuen Co site. A famous visitor TERESAMANERA In 1832 Charles Darwin came here to LESSED WITH FERTILE SOIL and known to us only by their fossils. At the investigate the legendary Monte Her- lush grasses, the Pampas of Argen- southern extremity of the Argentinean moso cliffs, whose sediments con- tina is perhaps best known for its Pampas plain lies a 30-km sector of the tain fossil remains of autochthonous cattle that supply beef to markets all over Atlantic coast whose soils have yielded South American fauna. His visit is re- the globe. The Pampas grasslands roll an extraordinary assemblage of fossils called by Teresa Manera, professor at southward from the Rio de la Plata to the that give us a snapshot of the changing the National University of the South banks of the Rio Negro, westward toward paleoenvironment at four significant mo- in Bahía Blanca and honorary direc- the Andes, and northward to the southern ments over the past 5 million years, from tor of the Charles Darwin Municipal parts of Córdoba and Santa Fe provinces, the upper Tertiary through the arrival of Natural Science Museum. “Darwin embracing the entire Buenos Aires and the first humans. went to Monte Hermoso with Cap- La Pampa provinces. For many millennia And not only the skeletal remains of tain Robert FitzRoy to survey the before man and cattle arrived, the Pampas extinct fauna are present. We also have area,” Dr. Manera tells us. “There, was the habitat for myriad herbivores great their footprints, fossilized and safe from he found some rodent bones that and small, most of them now extinct and harm . until now. The rush to preserve were important in the development 2 Volume 29 n Number 2 of his thought on the evolution of life.” ments accumulated, and with them the mammals with exotic names—Borhy- The bones, fossil remains of an extinct remains of creatures then extant. At the aenids, Hegetotheridae, Mesotheriidae, member of the cavy family, gave Darwin Farola Monte Hermoso site, entombed in Protherotheriidae, Macraucheniidae. So tangible evidence of an extinct ancestor marine cliffs 12 m high that stretch for rich and varied is the paleontological re- of a species living today. Here we witness 3 km are members of every significant cord, in fact, that the locale has given its the first stirrings of his volcanic theory family of animals from the Pliocene into name to a specific evolutionary age, the of evolution. “After Darwin,” Manera the Pleistocene, some that appear in Montehermosan Stage. continues, “many scientists performed popular literature—armadillos, glypto- At the beginning of the upper Pleis- research at Monte Hermoso cliffs—ar- dons, ground sloths, and fish, amphib- tocene eolian deposits consolidated into chaeologists, paleontologists, and geolo- ians, and reptiles—and now-vanished sandstone that capped the Monte Her- gists, which eventually led to an outcrop of sediments spanning from the Pliocene to Holocene,” says Manera. As a geologist working in paleon- tology, Manera studies vertebrate ta- phonomy at the Monte Hermoso site. Working with a Ph.D. student, she has found Pliocene vertebrate bones (fishes, amphibians, reptiles, birds, and mam- mals) and some sloth footprints. “This work was important because it allowed us to define in a better way the stratig- The Mammoth Trumpet (ISSN 8755-6898) is published quarterly by the Center for the Study of the First Americans, Department of Anthropology, Texas A&M University, raphy of the Pliocene formation (Monte College Station, TX 77843-4352. Phone (979) 845-4046; fax (979) 845-4070; e-mail Hermoso Formation), which was very [email protected]. Periodical postage paid at College Station, TX 77843-4352 and at ad- controversial.” ditional mailing offices. POSTMASTER: Send address changes to: A wealth of material for paleon- Mammoth Trumpet tologists Department of Anthropology, Texas A&M University You would be hard pressed to name an- 4352 TAMU other area anywhere in the world so rich College Station, TX 77843-4352 in evidence of past life as Monte Hermoso Copyright © 2014 Center for the Study of the First Americans. Permission is hereby and other sites in the vicinity of Bahía given to any non-profit or educational organization or institution toreproduce without cost any materials from the Mammoth Trumpet so long as they are then distributed at Blanca. Just to the north within a radius no more than actual cost. The Center further requests that notification of reproduction of 300 km lie such archaeological sites of materials under these conditions be sent to the Center. Address correspondence to the as Arroyo Seco, El Guanaco, Paso Otero, editor of Mammoth Trumpet, 2122 Scout Road, Lenoir, NC 28645. Cerro La China, Cerro El Sombrero, Michael R. Waters Director and General Editor sites that today are creating immense e-mail: [email protected] excitement—and great controversy—by Ted Goebel Associate Director demonstrating that humans occupied e-mail: [email protected] the South American continent far earlier James M. Chandler Editor, Mammoth Trumpet than was previously thought (MT 25-4, e-mail: [email protected] “Paleo South America: Long Time, No Christel Cooper Office Manager e-mail: [email protected] See”). C & C Wordsmiths Layout and Design Clustered in the immediate vicinity of AlphaGraphics Printing and mailing Bahía Blanca are a suite of sites that span Web site: www.alphagraphics.com many geological ages. Cristina Bayón, to- World Wide Web site http://centerfirstamericans.com gether with Silvia Aramayo, Manera, and The Center for the Study of the First Americans is a non-profit organization. Subscrip- Gustavo Politis, professor of archaeology tion to the Mammoth Trumpet is by membership in the Center. at the Universidad Nacional del Centro in Buenos Aires, describes how stratified Mammoth Trumpet, Statement of Our Policy sediments formed the sites. The setting Many years may pass between the time an important discovery is made and the acceptance of research results by the scientific community. To facilitate communication among all parties interested in staying originated, they explain, as a plain lying abreast of breaking news in First Americans studies, the Mammoth Trumpet, a science news magazine, between the hills of the Ventania range provides a forum for reporting and discussing new and potentially controversial information important to and the sea. Fine sediments were laid understanding the peopling of the Americas. We encourage submission of articles to the Managing Editor down in a fluvial environment by mean- and letters to the Editor. Views published in the Mammoth Trumpet are the views of contributors, and do not reflect the views of the editor or Center personnel. dering rivers laden with silt. Over many –Michael R. Waters, Director millennia meter upon meter of sedi- April n 2014 3 moso Formation. “On the shores of these temporary ponds of the Pampean Late This mantle, called Pleistocene,” say Bayón et al., “an exceptional record of ani- the Puerto Belgrano mal footprints and tracks crops out on platforms along 5,000 Formation, was itself meters of the modern coast. The process was repeated quite overlain with fluvial regularly, each after deposits that eventu- SIERRA DE LA a short period of time, ally formed the Sauce VENTANIA generating overlap- Grande River, which ini- ping layers.” tially flowed into the Atlan- More than a hun- S tic near the Monte Hermoso a dred trackways and u c cliffs. By the time of the e hundreds of random G late Pleistocene the ever- Bahía Blanca ra footprints record nd shifting terrain had altered e R. the passage of the the course of the river 11 most notable South km to the east, where the Monte Hermoso1– American Pleisto- Playa del Barco site today lies. Its sediments La Olla cene fauna. From the 050 Pehuen Co contain the remains of fauna of a later evolutionary km Playa del Barco tracks Manera, Ara- stage than those of the Farola Monte Hermosa site. Farola Monte Hermoso mayo, and other sci- Some are descendants of the same groups present in entists have identified the Montehermosan Stage, now evolved into different genera— Megatheridae, Mylodontidae, Glyptodontidae, Macrauchenia, giant ground sloths, and glyptodons and their close relatives, the Paleolama, Lama, Equidae, Stegomastodon, Carnivora (Ursi- Dasypodidade. Making their first appearance are also animals dae, Canidae, Felidae), and Caviidae. of North American origin, including camelids, pro- A lifetime of caring boscideans, cervids, and Manera has a deep attachment to carnivores. Preying on the the Pehuen Co site, which is evi- late-Pleistocene megaher- dent in the 2004 Rolex Award for bivores of the Pampas was Enterprise she received for her Smilodon, the saber-tooth work there. (To view an excellent tiger of Rancho la Brea reprise of her work, log on to http:// fame. www.rolexawards.com/gallery/vid- eos/2004.) When she was growing Setting the stage for up, her parents had a weekend house recording footprints in Pehuen Co.