[Aztlan] Jaguars in Formative Valley of Mexico
Bruce Rogers
bwrogers at dslextreme.com
Sun Jul 27 19:29:46 CDT 2008
Listeros,
Travis Doering asked if the jaguar (Pantera onca, Linnaeus, 1785)
was indigenous to the Valley of Mexico during Formative time and if
so, what were the ecological constraints on its range.
From my limited knowledge and reference searching (remember: I'm a
geologist, not a mammologist...), it appears that historically the
jaguar was present in the Valley of Mexico during Formative times.
Although the jaguar prefers a fairly dense rain forest and adjacent
open water such as rivers and such, it was/is known from semi-arid
scrub forest. It prefers lower elevations below about 1000 m, but
current sightings have been recorded up to 3,800 m.
The paleontological record has shown that jaguars evolved from
leopards, a genus that itself apparently evolved in India some 5
million years ago, or at least that's what the current fossil record
tells us. Panthera gombaszoegensis evolved in Eurasia shortly there
after. Panthera agusta was the first "grandaddy" jaguar to migrate
to the New World from Siberia somewhere between 3 and 1.5 million
years ago; the fossil record is spotty and open to debate at this
point. Evolving during the latest Pliocene and following Pleistocene
Epochs, fossil remains of jaguars as a distinct species have been
found that are as old as 40,000 years ago in the latest Pleistocene
Epoch. The Missouri fossil "population" was much heavier and more
robust than present species and dated to between less than 40,000 and
10,500 years old. Another 14 inch-long skull and long bones of a
jaguar (exact species unidentified-it's still under study) was found
in 1995 at Oregon Cave National Monument in southwestern Oregon near
the California border. This is the northernmost occurrence of fossil
jaguars known in the New World and dates to about the latest
Pleistocene Epoch, some 38,000 years ago.
New World fossil jaguars, in general, evolved in North America during
the latest Pliocene Epoch, then spread south, crossing North America
towards South America about 2 million years ago after the Isthmus of
Panama finally connected the two continents some 3.1 million years
ago (a milestone in New World tectonics). The oldest fossil big cats
in South America found so far date to the end of the Pleistocene
Epoch, just under 2 million years old.
It appears that availability of prey, dense vegetative cover, and
availability of water (a habitat preferred much like its solitary
cousin the tiger, P. tigris) are key elements in its ecological niche.
With the tremendous changes in the Valley of Mexico (clearing of
vegetation, draining of Lake Texcoco, and intense urbanization) this
part of the big cat's range has become untenable. Indeed, current
range maps indicate the species has been largely extirpated in the
northern part of Mexico and adjacent southwestern USA (although
reliable observations exist for solitary animals from as recent as
2004) and its longitudinal range now limited to the Sierra Madre
Occidental and areas to the west.
In particular, Lake Texcoco (site of the modern Mexico City) has
existed for about 100,000 years, was possibly fairly deep with
extensive surrounding marshland fed by bordering springs emanating
from the porous volcanic rock and alluvial soils. By about 10,000
years ago, the lake fauna was replaced by shallow water, marshy
fauna, most probably caused as the lake started shrinking due to the
end of the Pleistocene Ice Ages. The marshy lake margins supporting
dense vegetation would have been prime habitat for the jaguars over
the last several hundred millennia.
What a loss . . . .
Cheers,
Bruce Rogers, earth scientist (& part time naturalist) on a good day
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