Science1 publisher3 min readPublished
A capybara tooth from coastal Chile puts standing water in the Atacama 9 million years ago
Priscilla Martinez's team pulled the tooth from a marine deposit at El Morro in northern Chile. Freshwater fish, gavials and palm phytoliths from the same beds carry more of the argument than the tooth does.
The Scientist · Science desk

What happened
- A fossilized tooth from a capybara that lived almost 9 million years ago in what is now the Atacama Desert is the first and oldest record of the rodent in coastal Chile, where none live today.
- The tooth came from sediments deposited in a shallow marine environment between 10 million and 7 million years ago at El Morro, part of northern Chile's fossil-rich Bahia Inglesa Formation.
- The same deposits yielded fossils of freshwater fishes and gavials, freshwater crocodiles, which the authors read as independent signs of persistently wet conditions at the site.
- The paper, in Scientific Reports, questions the textbook account of the Atacama as one of Earth's oldest continuously dry regions, an estimate that runs back some 40 million years.
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Why it matters
- constraint A continuity claim breaks on its wettest documented gap, and this one is dated to about 9 million years ago, which leaves the older 31 million years of the record untested by the fossil either way.
- capability Obligate semiaquatic animals plus phytoliths give aridity work a local water-presence check that does not depend on isotopes or sediment chemistry, and it can be applied wherever such fossils are preserved.
- decision Anyone extending El Morro's wet signal to the desert as a whole now has to argue the step explicitly, because the deposit that produced the tooth is a coastal marine one.
- constraint With a single specimen and no other capybara material from that stretch of coast, the strength of the reconstruction sits with the associated freshwater fossils and plants, not with the rodent.
What makes the tooth a climate claim is what a capybara needs to stay alive. Rodent specialists call them obligate semiaquatic herbivores that indicate persistent riparian ecosystems [6]. They are the largest living rodents, native to South America, and today they live east of the Andes in low-elevation wetlands, their core range roughly outlining the Amazon basin [7]. Their way of life ties them to standing surface water, wetland vegetation and movement along creeks and rivers [8].
The tooth itself came out of the wrong rock for that habitat. The beds at El Morro were deposited in a shallow marine environment between 10 million and 7 million years ago [4], so where the animal was buried is not where it lived. Fresh water comes in with the rest of the assemblage. "We have multiple lines of evidence indicative of really wet conditions that are typically associated with capybaras today," said Mark Clementz of the University of Wyoming, a co-author. "The same deposits contain fossils of freshwater fishes and gavials (freshwater crocodiles)" [14]. The team also recovered phytoliths, the silica bodies that form inside plant cells as roots take up dissolved silica from groundwater, and co-author Caroline Strömberg of the University of Washington matched them to palms and other flowering plants, including dicots, nothing that grows in the Atacama now [15][16]. "Think sunny Southern California full of palm trees," Martinez said [17].
The 40-million-year figure and the fossil do not sit at the same scale. If the region's dryness began 40 million years ago and the tooth dates to about 9 million, then 31 million years of that record run before the wet interval and are untouched by it [18]. The tooth's age is bracketed rather than measured directly, inside a three-million-year depositional window [19].
The animals also had to get there. Geologists estimate the Andes rose to about 18,000 feet, roughly 5,500 metres, before capybaras appeared, walling the Atacama off from the eastern lowlands that hold the animal's range today [11][20]. "Not only are the plateau lands of the Central Andes very tall, they're also extremely arid," Martinez said. "So, if capybaras originated east of the Andes in this foreland region, how in the world could these short-legged rodents make it across?" [12] The authors propose they went around, counterclockwise through low-elevation wetlands from today's Venezuela into Colombia, Ecuador and Peru, then into northern Chile [13].
The record rests on one tooth. "We don't have any other evidence of capybaras in that part of coastal Chile," said co-author Barbara Carrapa, Martinez's doctoral adviser at the University of Arizona [10]. The published account does not say how long the wet conditions lasted or how far inland they extended [21]. I would put weight on the wet coastal setting at El Morro, which three independent fossil lines support, and much less on the 40-million-year continuity figure being wrong, because that case needs deposits of the same age from inland sites and the paper describes a coastal one [4][2].
What to watch
- Deposits of the same 10-to-7-million-year window from inland Atacama sites, with or without freshwater fossils, would test whether the wet interval was regional or coastal.
- A second capybara specimen from El Morro or elsewhere on the Chilean coast would turn one stray animal into evidence of a resident population.
- Whether aridity reconstructions revise the 40-million-year continuity estimate or restrict it to parts of the desert the fossil does not sample.