Jump to content

Nidophis

From Wikipedia, the free encyclopedia

Nidophis
Temporal range: Maastrichtian
Nidophis insularis vertebrae (scale bar 1 mm)
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Order: Squamata
Family: Madtsoiidae
Genus: Nidophis
Species:
N. insularis
Binomial name
Nidophis insularis
Vasile et al., 2013

Nidophis is an extinct genus of madtsoiid snake that inhabited on Hațeg island in what is now Romania. The type and only known species of the genus is N. insularis. The holotype was closely associated with the dinosaur egg nest,[1] though it may not have been a nest raider.[2]

Discovery and naming

[edit]

The holotype of Nidophis insularis is a well-preserved mid-trunk vertebra, with only the posterolateral margins of the left postzygapophysis broken off. The genus name Nidophis is a portmanteau of the Latin word nidus ("nest"), referring to its discovery associated with a dinosaur nest, and the Ancient Greek word ὄφις (ophis, "serpent"). The specific name insularis is a Latin word alluding to the probable island occurrence of this taxon.[1]

Paleoenvironment

[edit]

The holotype of Nidophis insularis is found in the uppermost Cretaceous (Maastrichtian) continental deposits of the Hațeg Basin, western Romania.[1] Today Haţeg is a landlocked town in Romania, but 70 million years ago during the late Cretaceous it was an island within a shallow sea that covered much of today's southern Europe.[3]

Based upon the study of paleosols (fossilised soils) the climate is thought to have been sub-tropical with distinct wet and dry seasons,[4] carbon isotopes indicate "dry woodland" conditions,[5] and oxygen isotopes suggests a mean annual temperature of about 20-25 °C. Rainfall estimates differ according to whether they are based upon plant fossils or palaeosols. Palaeosols indicate that the climate had seasonal precipitation of less than 1000 mm/year, with greater evapotranspiration than precipitation and a fluctuating water table.[6]

References

[edit]
  1. ^ a b c Ştefan Vasile; Zoltán Csiki-Sava; Márton Venczel (September 2013). "A new madtsoiid snake from the Upper Cretaceous of the Haţeg Basin, western Romania". Journal of Vertebrate Paleontology. 33 (5): 1100–1119. doi:10.1080/02724634.2013.764882. ISSN 0272-4634. Wikidata Q29997837.
  2. ^ Venczel, Márton; Vasile, Ştefan; Csiki-Sava, Zoltán (2015). "A Late Cretaceous madtsoiid snake from Romania associated with a megaloolithid egg nest – Paleoecological inferences". Cretaceous Research. 55: 152–163. doi:10.1016/j.cretres.2015.02.009.
  3. ^ Weishampel, D. B.; Jianu, C.-M. (1996-07-31). "New Theropod Dinosaur Material from the Haţeg Basin (Late Cretaceous, Western Romania)". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 200 (3): 387–404. doi:10.1127/njgpa/200/1996/387. ISSN 0077-7749.
  4. ^ Van Itterbeeck, J., Sasaran, E., Codrea, V., Sasaran, L., and Bultynck, P. 2004. Sedimentology of the Upper Cretaceous mammal- and dinosaur-bearing sites along the Râul Mare and Bãrbat rivers, Haþeg Basin, Romania. Cretaceous Research 25, 517-530.
  5. ^ Bojar, A.V., Grigorescu, D., Ottner, F., and Csiki, Z. 2005. Palaeoenvironmental interpretation of dinosaur- and mammal-bearing continental Maastrichtian deposits, Haţeg basin, Romania. Geological Quarterly 49, 205-222.
  6. ^ Therrien, F. 2005. Paleoenvironments of the latest Cretaceous (Maastrichtian) dinosaurs of Romania: insights from fluvial deposits and paleosols of the Transylvanian and Haþeg basins. Palaeogeography, Palaeoclimatology, Palaeoecology 218, 15-56.