
Curaçao Giant Tortoise
Chelonoidis sp 2.
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Chordata
Reptilia
Testudines
Cryptodira
Testudinidae
Chelonoidis
Chelonoidis sp 2.
Chelonoidis = “tortoise-like”; curaçaoensis = “from Curaçao,” referencing its island habitat in the southern Caribbean.
A robust island tortoise native to Curaçao during the late Pleistocene, part of the extinct Caribbean Chelonoidis radiation.
Description
The Curaçao giant tortoise (Chelonoidis curaçaoensis) was a large terrestrial tortoise endemic to the island of Curaçao in the southern Caribbean. It belonged to a diverse radiation of West Indian tortoises that once included species on the Bahamas, Greater Antilles, and northern South American islands. Fossil remains indicate a mid-sized but sturdy tortoise with a domed carapace and strong limbs adapted for walking over arid, rocky terrain and scrub habitats typical of Curaçao’s landscape in the late Pleistocene.
Shell dimensions from carapace fragments suggest an estimated length of 0.6–0.9 meters, somewhat smaller than the giant forms on larger islands but comparable to medium-sized Galápagos morphotypes. Its diet was dominated by xeric vegetation—shrubs, tough herbs, succulents, and dry forest understory plants—consistent with the island’s dry climate. As with other insular tortoises, it likely had slow growth, long lifespan, and low reproductive rate.
The species appears to have gone extinct before human arrival to Curaçao, with radiocarbon estimates placing its disappearance in the late Pleistocene, possibly tied to climatic changes and habitat shifts during glacial–interglacial transitions.
Quick Facts
Max Mass
Shoulder Height
Standing Height
Length
Diet
Trophic Level
100
kg
m
m
m
Hunt History
Unlike Bahamian or Cuban tortoise species that survived into the Holocene and interacted with early Caribbean peoples, Chelonoidis curaçaoensis is known only from paleontological deposits and shows no evidence of human predation or cultural use.
Three contexts:
Hato Caves, Curaçao — Pleistocene-age fossils indicate an arid scrub ecosystem supporting endemic reptiles.
Tafelberg limestone deposits — Carapace fragments found with Pleistocene avifauna and small mammals, no anthropogenic markings.
Coastal karst sites — Fossils associated with shifting sea levels and climatic transitions toward the end of the Pleistocene.
These contexts suggest an extinction tied to ecological turnover well before human settlement of the ABC islands (~2500–3000 years ago).
Time & Range
Extinction Status
G
Extinction Date
Temporal Range
Region
8000
BP
Late Pleistocene
Carribean
Wiki Link
Fat Analysis
Fatness Profile:
Fat %
Est. Renderable Fat
kg
Targeted Organs
Adipose Depots
Preferred Cuts
Hunt Difficulty (x/5)





