4.5 Article

Ostracods had colonized estuaries by the late Silurian

Journal

BIOLOGY LETTERS
Volume 17, Issue 12, Pages -

Publisher

ROYAL SOC
DOI: 10.1098/rsbl.2021.0403

Keywords

Silurian; ostracods; pioneer; colonizers; estuary

Funding

  1. Natural Environment Research Council [NE/S007350/1]
  2. Central England NERC Training Alliance (CENTA)
  3. Vietnamese project `Stratigraphical research for the Devonian sedimentary rocks in the north-northwest of the Song Hien structure' [TNMT.2018.03.05]
  4. Vietnamese project 'Phanerozoic stratigraphy in the eastern Viet Bac (including Ha Giang, Cao Bang, Bac Ka. n, Thai Nguyen and La. ng Son provinces) and related mineral resources' [NVTX.2021.03.03]
  5. Japan Society for the Promotion of Science [16K05593, 19K04059, 18H02495]
  6. Leverhulme Research Fellowship ('The early Palaeozoic evolution of Vietnam') [RF-2018-275/4]
  7. Grants-in-Aid for Scientific Research [19K04059, 18H02495] Funding Source: KAKEN
  8. NERC [NE/S007350/1] Funding Source: UKRI

Ask authors/readers for more resources

Ostracod crustaceans began occupying marginal marine and estuarine environments early on, acting as a significant component in the transition from marine to non-marine environments.
The fossil record of terrestrialization documents notable shifts in the environmental and physiological tolerances of many animal and plant groups. However, for certain significant components of modern freshwater and terrestrial environments, the transition out of marine settings remains largely unconstrained. Ostracod crustaceans occupy an exceptional range of modern aquatic environments and are invaluable palaeoenvironmental indicators in the fossil record. However, pre-Carboniferous records of supposed non-marine and marginal marine ostracods are sparse, and the timing of their marine to non-marine transition has proven elusive. Here, we reassess the early environmental history of ostracods in light of new assemblages from the late Silurian of Vietnam. Two, low diversity but distinct ostracod assemblages are associated with estuarine deposits. This occurrence is consistent with previous incidental reports of ostracods occupying marginal and brackish settings through the late Silurian and Devonian. Therefore, ostracods were pioneering the occupation of marginal marine and estuarine settings 60 Myr before the Carboniferous and they were a component of the early phase of transition from marine to non-marine environments.

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