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Curaçao Giant Tortoise

Chelonoidis sp 2.

🐢

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)

Ethnography List

Historical Entries

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