54. Possible Relatives in the Americas

Jaguay and Tacahuay sites (Arequipa and Tacna, Peru)

by George Weber


 

 

 

Location of Tacahuay andJaguay sites on the coast of southern Peru. The two sites represent the oldest known adaption of early humans in the Americas to a coastal way of life.

Sources for Jaguay:
-- Tanner B. R. 2001. Lithic Analysis of Chipped Stone Artifacts recovered from Quebrada Jaguay, Peru, thesis, Graduate School, The University of Maine

Sources for Tacahuay:--
-- deFrance S. D. and Álvarez A. U.. 2004. "Quebrada Tacahuay: un sitio maritimo del Pleistoceno tardio en loa costa Sur del Peru.". Chungara, Revista de Antropología Chilena, vol. 36:257-278.
-- Wilford J.N., 1998, "In Peru: Evidence of an Early Human Maritime Culture - the Discovery of Ancient Camps in Peru and Chile." New York Times, 22 September 1998 

        

 

The traditional picture of the first inhabitants of the Americas is one of big-game hunters who made their living heroically from large, now-extinct mammals such as mastodons and mammoths. Only after about 10,000 years ago, as the large mammals disappeared, did these people turn to other, more diverse sources of food. The Tacahuay and Jaguay sites shatter this picture.

It is also usually assumed that the first humans in the Americans (whenever the arrived and from wherever they came) spread over the Americas mostly on foot and this may indeed have been largely true in the conquest of the continental interiors. On the other hand, the Jaguay and Tacahuay sites provide strong evidence that the earliest major human population movements of which we have archaeological evidence were much more likely to have been along the coasts - by boat.

Early coastal archaeological sites such as Tacahuay and Jaguay show that their people had remarkably advanced technologies adapted to a coastal way of life from moment they appear on the archaeological radar. The existence of sophisticated and highly efficient fishing nets - unlikely to have been be invented "on the spot" at Jaguay and Tacahuay, for example - speak for a long preceding period of coastal living.

If the earliest human arrivals in the Americas moved south over many generations by boat along the western coast from Alaska to Tierre del Fuego, it would also explain why some dates from South America are at least as early as any North American dates - and why the spread of the first humans into the Americas was so astonishingly rapid.

Why have there not been more coastal sites found? With the climate-warming after the end of the pleistocene ice age (very roughly 10,000 years ago) sea levels rose quickly and by as much as 100 m. Most pleistocene coastal sites must now be deep under water and so be very difficult to find and only sitess on steep coasts still are above modern sea levels. There is a strong probability that there were people in the Americas still earlier than those of Jaguay and Tacahuay - and that their sites simply have not been found yet because most a5re under water.

 

The Jaguay site

The Jaguay site (often called "Quebrada Jaguay" for the gulch or ravine it is located in) was excavated by D.H. Sandweiss, University of Main, USA, in the 1990s. The site is located near the bed of a seasonal stream flowing out of the highlands into the coastal desert. People occupied the site for a time 13,000 to 11,000 years ago (calibrated C14 years). They seem to have lived from clams they gathered and by catching small fish with sophisticated tools and methods.

 

The local environment of the Jaguay site (adapted from Tanner B.R., 2001).

The red arrow points in the general direction from where the earliest the Jaguay people already procured high-quality obsidian (a very hard volcanic glass used for making tools).

The locations where obsidian is found are between 150 and 200 km to the North and Northwest of Jaguay in the High Andes. These places can be reached from the coast only over extremely difficult and mountainous terrain. It is not known whether the earliest inhabitants of the Jaguay site went on obsidian-collecting expeditions into uninhabited territory or whether they traded for the material with people already living there. Knowledge of sources in such remote and inhospitable areas 13,000 years ago certainly indicates that humans had moved around and explored there there for some time before they appear in the archaeological record.

The connection between the Jaguay and the Alca obsidian sources is the only definitively proven material link between coastal and highland locales in all of South America. Obsidian can be traced to its origin because of its characteristic chemical signatures and it has been possible to pinpoint the source ofJaguay's obsidian and to study areas near the Alca obsidian source in order to find additional early highland archaeological sites. A 2005 expedition to the Alca obsidian source and nearby Nevado Firura ice cap discovered numerous early sites possibly contemporary with the early Jaguay site. This early occupation is noteworthy because they are the world's most elevated late pleistocene sites.

 

 

Excavation work in progress on the Jaguay site in 1996.

From the start of human settlement of South America people built houses (among the earliest known in the New World) and carried out domestic activities such as cooking and finishing chipped stone tools. During the first occupation, dating to around 13,000-11,000 years ago, obsidian from the highland Alca source 130 km distant indicates contact with the mountainous interior. Very likely these people moved seasonally between the coast and the Andes. Later, during the early Holocene, obsidian is much rarer and many sites suddenly appear in the surrounding countryside. By this time, some people may have lived year-round on the coast, moving seasonally from the quebrada bank where water flows in the summer to the foothills where dense fog provides water and vegetation in the winter. The site and region seem to have been abandoned after 8000 years ago, when many records suggest an extended dry period that lasted for about 4000 years. Though the Quebrada Jaguay site was never reoccupied, other sites in the region date to about 4000 years ago, but their contents suggest a different way of life than that of the earlier settlements.

 

 

Postholes from a late Pleistocene house at the Jaguaysite. The blue balloons in the post holes that predate an indurated layer indicate the earliest known human construction on the site.

 

An example of archaeological strata at the Jaguay site
(adapted from Tanner B.R., 2001).

Archaeologicval strata marked in yellow in the graphic date to the terminal Pleistocene (i.e. older than very roughly 10,000 years ago) while grey strata represent early Holocene human occupation of the site and are less than very roughly 10,000 years ago.

      

 

Uniface tools from the Jaguay site's oldest (terminal pleistocene) levels.
(adapted from Tanner B.R., 2001).

 

Biface tools from the Jaguay site's oldest (terminal pleistocene) levels.
(adapted from Tanner B.R., 2001).

 

The Tacahuay site

 

 

 

About 10,700 years ago, a series of catastrophic flooding events (El Nino events) covered and sealed the accumulated signs of previous human activity (stratum 8) at the Tacahuay site by massive amounts of debris washed down by torrential rains from the mountains (stratum 7).

Before the late 1990s it had been thought that El Nino was a relatively recent phenomenon - but Dr. James B. Richardson in 1965 he discovered the 8,000 year old Siches site near Talara, Peru where he found evidence of dramatic climate change over a 4,000 year period. After extensive archaeological research on the coast of Peru, this led him and his colleague Dr. Daniel H. Sandweiss of the University of Maine, to propose in 1986 that El Nino was only 5,000 years old. They met considerable scepticism. But in 1996,with the discovery of no less than 19 El Nino flood deposits at the site of Tacahuay proved that El Nino events merely ceased (or were substantially reduced) between 9,000 to 5,000 years ago.

 

 

The Tacahuay excavation site of 2001 (map adapted from deFrance et al, 2004)

 

The stratification of block 2 of the Tacahuay sit (depth shown: 3 m). The dates shown are unclibrated. The oldest calibrated dates from the site (from block 1) come from charceal from a hearth and range from 12,390 to 13,030 years before present (adapted from deFrance et al, 2004).

Map of the ancient river bed
in strata 8/9).

 

 

The arrows point at stone flakes still in situ (block 3).
(from deFrance et al, 2004).

 

Stone tools from stratum 8 of block 3.
(adapted from deFrance et al, 2004)

 

A stone toolf from stratum 8.
(adapted from Wilford 1998)

 

 

A worked rib of a marine mammal - a mesh gauge for fishing nets?

 

(from deFrance et al, 2004)

Although no direct evidence of early net fishing has been found at Tacahuay (apart perhaps from the possible mesh gauge shown above), another very early coastal site, Jaguay (near Camana and ca. 350 miles as the crow flies NW from Tacahuay) has yielded bits of knotted cordage that could well be the remains of fishing nets. At Tacahuay, the bones of numerous small fish (mostly anchovy) were found. The small size of these fish argue for the use of nets rather than hook-and-line, let alone harpoons.

 

A clay ball, an artefact of unknown purpose:
(from deFrance et al, 2004)

 

 

A bird bone showing multiple cuts from stone tools, indicating that it had been butchered by humans. Many other bones showing similar cut marks have been found at Tacahuay.
(from deFrance et al, 2004)

  

 Among web-sites with further information are:

- http://www.scielo.cl/scielo.php?pid=S0717-73562004000200002&script=sci_arttext

- http://www.unl.edu/rhames/monte_verde/peru_clovis.htm

- http://www.carnegiemnh.org/news/06-apr-jun/051006richardson.htm

- http://www.pnas.org/cgi/reprint/0509279102v1.pdf

- http://www.library.umaine.edu/theses/pdf/TannerBR2001.pdf

- http://www.climatechange.umaine.edu/Research/Contrib/pdf/pdfFiles/contribution05.pdf

 

 

[ Go to HOME ]

[ Go to CONTENTS OF OUT-OF-AFRICA CHAPTERS ]

[ Go to CONTENTS OF AMERICA CHAPTERS ]

Last change 20 July 2007