Parasilvia ("near forest") is a genus of anomodont therapsid (extinct mammal-line synapsid related to dicynodonts) known from rocks assigned to the Late Permian aged Chroniosaurus levis Tetrapod Zone (Podlesnyi locality) in Orenburg, Russia. The genus contains the type and only species, Parasilvia alexandrae, known from various fragmentary and disarticulated bones of the skull and jaw. Parasilvia closely resembles other Russian anomodonts, namely Suminia and Parasuminia, and the three were classified as 'dromasaurs' together in their own family by its describers with the South African Galechirus in Galechiridae. Parasilvia appears relatively primitive (basal) compared to Suminia and Parasuminia, in some ways more closely resembling Galechirus and other Russian anomodonts (e.g. Venyukovia and Ulemica, i.e. Venyukovioidea). In phylogenetic systematics, all the other Russian anomodonts are conventionally classified together under Venyukovioidea while 'dromasaurs' are regarded as an artificial grouping (polyphyletic) of unrelated South African taxa (including Galechirus). This reflects the different approaches to anomodont taxonomy. Regardless, Parasilvia is the youngest known early anomodont from Russia, despite being considered relatively primitive compared to its older close relatives.
History of discovery Fossils of Parasilvia were first discovered in 2024 in a quarry on the northeast outskirts of the village of Podlesnyi in the Grachevsky District of Orenburg, Russia. The fossil locality in the quarry was newly discovered that year by F. F. Shaymardanov and M. L. Papernyi, and the first anomodont fossils from the quarry (teeth and a lower jaw) were reported at conferences in 2024 by Shaymardanov and Papernyi with V. V. Bulanov. Subsequent excavations in 2025 by the Borissiak Paleontological Institute of the Russian Academy of Sciences (PIN RAS) and the Samara Paleontological Society discovered additional partial remains of the snout and palate, which together were enough to identify the Podlesnyi anomodont as a new taxon. The fossils of Parasilvia alexendrae were described and named as a new genus and species by Bulanov, Shaymardanov and Papernyi in 2026. Bulanov and colleagues described the etymology of the genus name as being derived from Latin and as a combination of para (to mean "beside") and silva ("forest"), which itself comes from a near-literal translation of "Podlesnyi". The species name P. alexandrae is named after Alexandra Papernaya, the wife of M . L. Papernaya. The holotype specimen of Parasilvia (PIN, no. 5936/5) is a skull fragment comprising most of the right maxilla (the largest upper jaw bone) with fragmentary portions of the attached jugal and lacrimal bones, as well as portions of the right palatal bones (palatine, pterygoid and ectopterygoid). Additional specimens include an isolated left premaxilla (PIN, no. 5936/4) and a partial lower jaw (PIN, no. 5936/1), as well as several isolated teeth. These fossils were CT-scanned at PIN RAS and reconstructed digitally in 3D. The Podlesnyi locality has not been dated absolutely, but biostratigraphic correlations imply it belongs to the Chroniosaurus levis Tetrapod Zone (a biozone) of Russian regional stratigraphy), and potentially directly correlative to the better studied Mutovino locality of the Kichuga Member in the Poldarsa Formation. This locality is roughly dated to the end of the Severodvinian stage in regional stratigraphy. This stage corresponds to the end of the Capitanian and into the early Wuchiapingian on the global International Stratigraphic Scale of the Middle and Late Permian respectively, and so correlation with Mutovino suggests the Podlesnyi locality dates to the Wuchiapingian, no more than 259.857 million years ago (Ma). The fossiliferous rocks of the quarry consist of layers of fine-grained sandstone approximately 8.5 metres (28 ft) thick representing fluvial deposits, interbedded with pebbles and gravels.
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