ArticleCommunications biology2021
Fossil evidence for vampire squid inhabiting oxygen-depleted ocean zones since at least the Oligocene.
Article in Communications biology, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
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Who cites it
6 citing papers in PubMed.
- Giant genome of the vampire squid reveals the derived state of modern octopod karyotypes.iScience · 2025Article
- Article
- Probability-based preservational variations within the early Cambrian Chengjiang biota (China).PeerJ · 2022Article
- The significance of cephalopod beaks as a research tool: An update.Frontiers in physiology · 2022Review
- Fossil evidence for vampire squid inhabiting oxygen-depleted ocean zones since at least the Oligocene.Communications biology · 2021Article
- Distraction sinking and fossilized coleoid predatory behaviour from the German Early Jurassic.Swiss journal of palaeontology · 2021Article
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Authors and funding
11 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
A marked 120 My gap in the fossil record of vampire squids separates the only extant species (Vampyroteuthis infernalis) from its Early Cretaceous, morphologically-similar ancestors. While the extant species possesses unique physiological adaptations to bathyal environments with low oxygen concentrations, Mesozoic vampyromorphs inhabited epicontinental shelves. However, the timing of their retreat towards bathyal and oxygen-depleted habitats is poorly documented. Here, we document a first record of a post-Mesozoic vampire squid from the Oligocene of the Central Paratethys represented by a vampyromorph gladius. We assign Necroteuthis hungarica to the family Vampyroteuthidae that links Mesozoic loligosepiids with Recent Vampyroteuthis. Micropalaeontological, palaeoecological, and geochemical analyses demonstrate that Necroteuthis hungarica inhabited bathyal environments with bottom-water anoxia and high primary productivity in salinity-stratified Central Paratethys basins. Vampire squids were thus adapted to bathyal, oxygen-depleted habitats at least since the Oligocene. We suggest that the Cretaceous and the early Cenozoic OMZs triggered their deep-sea specialization.
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