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The history of life at hydrothermal vents

Journal

EARTH-SCIENCE REVIEWS
Volume 217, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.earscirev.2021.103602

Keywords

Evolution; Chemosynthesis; Deep sea; Pyrite preservation; Cold seep; Volcanogenic massive sulfide

Funding

  1. United Kingdom Natural Environment Research Council [NE/R000670/1]
  2. South Urals Federal Research Center of Mineralogy and Geoecology UB RAS [AAAA-A19-119061790049-3]
  3. NERC [NE/R000670/1] Funding Source: UKRI

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Hydrothermal vents, supporting highly productive communities of specially-adapted fauna, have been a feature of Earth since its early history, intricately woven into the history of life on the planet. Fossils and molecular data provide valuable insights into the evolution and adaptation of life at vents, showing a transition in community composition over Earth's history. Targeting ancient vent deposits with low diagenetic changes can provide further insights and fill gaps in knowledge about vent fossils.
Hydrothermal vents are among the most fascinating environments that exist within the modern oceans, being home to highly productive communities of specially-adapted fauna, supported by chemical energy emanating from the Earth's subsurface. As hydrothermal vents have been a feature our planet since the Hadean, their history is intricately weaved into that of life on Earth. Despite an overall scant fossil record due to the improbabilities of preservation of vent deposits and organisms, recent fossil findings from ancient vent environments, accompanied by molecular data as well as fossils from ecologically-similar environments, have yielded invaluable new insights into the history of life at hydrothermal vents. Fossils from hydrothermal vents are among the earliest contenders for direct evidence of life on Earth, while a range of additional fossil finds indicate that vent habitats were readily exploited by microbes during the Precambrian. The first metazoans possibly appeared within vents during the Cambrian, and by the Ordovician-Silurian, hydrothermal vents in the deep ocean were colonised by mollusc, brachiopod and tubeworm taxa whose large abundances and sizes suggest these early animals were well-adapted to this setting. A transition in vent community composition occurred during the Mesozoic, as modern vent faunas began to occupy these environments and replace Paleozoic taxa. Molecular evidence indicates that many additional taxa radiated within vents during the Cenozoic, demonstrating that throughout Earth history, organisms were repeatedly able to overcome the challenges of adapting to the harsh conditions at vents to exploit their productivity. Targeting ancient vent deposits that have undergone low degrees of diagenetic or metamorphic change during mining-related exposure has great potential to provide further insights into the vent fossil record and fill existing gaps in knowledge.

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