Living Fossils In The Indo-Pacific!

Researchers have reported a unique discovery; the marine dinoflagellate Dapsilidinium pastielsii in Southeast Asia, notably the Indo-Pacific Warm Pool. This unicellular species, with planktonic and benthic stages, was previously thought to have become extinct within the early Pleistocene. It evolved more than 50 million years ago and is the last survivor of a major early Cenozoic lineage. The discovery of living D. pastielsii in the Indo-Pacific Warm Pool  suggests that this stable environment served as an important refuge for thermophilic dinoflagellates, and its disappearance from the Atlantic following the early Pleistocene implicates cooling.

Researchers have reported a unique discovery; the marine dinoflagellate Dapsilidinium pastielsii in Southeast Asia, notably the Indo-Pacific Warm Pool. 

This unicellular species, with planktonic and benthic stages, was previously thought to have become extinct within the early Pleistocene. It evolved more than 50 million years ago and is the last survivor of a major early Cenozoic lineage.

The discovery of living D. pastielsii in the Indo-Pacific Warm Pool  suggests that this stable environment served as an important refuge for thermophilic dinoflagellates, and its disappearance from the Atlantic following the early Pleistocene implicates cooling.

The new study highlights the importance of refugia in plankton biogeography and broadens their relevance as hotspots of biodiversity. It explains how biostratigraphic ranges in the Pacific can significantly extend those established for the Atlantic. The discovery of D. pastielsii as a “living fossil” in the IPWP highlights the potential for refugia to harbor species likely to expand their distributional range in a warming world.

This is the first record of a refugium plankton species within the Indo-Pacific warm pool.

Citation: Kenneth N. Mertens, Yoshihito Takano, Martin J. Head and Kazumi Matsuoka, 'Living fossils in the Indo-Pacific warm pool: A refuge for thermophilic dinoflagellates during glaciations', Geology
April 10, 2014, doi: 10.1130/G35456.1

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