Triturus
Triturus is a genus of newts comprising the crested and the marbled newts, which are found from Great Britain through most of continental Europe to westernmost Siberia, Anatolia, and the Caspian Sea region. Their English names refer to their appearance: marbled newts have a green–black colour pattern, while the males of crested newts, which are dark brown with a yellow or orange underside, develop a conspicuous jagged seam on their back and tail during their breeding phase.
Eduard Solà · CC BY-SA 3.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- SalamandridaePBDB
- Diet
- carnivorePBDB, for Temnospondyli
- Life habit
- amphibiousPBDB, for Temnospondyli
- Motility
- actively mobilePBDB, for Temnospondyli
- Environment
- brackish,freshwater,terrestrialPBDB, for Tetrapoda
Time the record covers
At least 48 million years on record.
The record covers at least 48.07 Mya to 11.7 ka. No occurrence read is dated outside 56 Mya to 0 Mya.
77 occurrences of Triturus on record, most of them in the Pleistocene. The Paleobiology Database records this as a living group. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
77 occurrencesThese are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
6 formations
- Upper Freshwater Molasse Formation · Molasse Group4
- Cromer Forest Bed Formation3
- Sajovolgyi Formation3
- Borgloon Formation · Tongeren Group2
- Unterer Travertin Formation2
- Gaverdovsky Formation2
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The named rock units Triturus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 61 occurrences have no formation on record, which is common for older literature.
Triturus and its relatives
PleistoceneWhere Triturus and its relatives were recorded in the Pleistocene.
Found in the same rock
843 taxa- Rana29 sites
- Lacerta25 sites
- Bufo bufo19 sites
- Anguis fragilis17 sites
- Bufo13 sites
- Lacertidae13 sites
- Natrix12 sites
- Natrix natrix12 sites
- Pelobates12 sites
- Rana temporaria11 sites
- Bufo viridis10 sites
- Hyla arborea10 sites
- Ophisaurus10 sites
- Pelophylax10 sites
- Colubrinae9 sites
- Latonia gigantea9 sites
- Microtus9 sites
- Vipera9 sites
- Chelotriton8 sites
- Hyla8 sites
- Anguis7 sites
- Anura7 sites
- Coluber7 sites
- Equus7 sites
The Paleobiology Database records 47 sites for Triturus, and this reads all of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
28 references- Pleistocene Amphibians and Reptiles in Britain and Europe33
- Terrestrial and marine faunas from the Miocene deposits of the Mokra Plateau (Drahany Upland, Czech Republic) - impact on palaeogeography5
- Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)3
- Amphibians and squamate reptiles from the late early Miocene (MN 4) of Béon 1 (Montréal-du-Gers, southwestern France)3
- The Herpetofauna (Amphibia: Caudata, Anura; Reptilia: Sclerogiossa) of the Upper Miocene Locality Kohfidisch (Burgenland, Austria)3
- Középs & #337;-miocén & #337;smaradványok, a Mátrasz & #337;l & #337;s , Rákóczi-kápolna alatti útbevágásból. I. A Mátrasz & #337;l & #337;s 1. lel & #337;hely [Middle miocene fossils from the road cut below the Rákóczi chapel at Mátrasz & #337;l & #337;s. I. The site Mátrasz & #337;l & #337;s 1]3
- Ectothermic vertebrates (Actinopterygii, Allocaudata, Urodela, Anura, Crocodylia, Squamata) from the Miocene of Sandelzhausen (Germany, Bavaria) and their implications for environment reconstruction and palaeoclimate2
- Biostratigraphy and palaeoecology of a Middle Miocene (Karpathian, MN 5) fauna from the northern margin of the North Alpine Foreland Basin (Oggenhausen 2, SW' Germany)2
- Ectothermic vertebrates (Teleostei, Allocaudata, Urodela, Anura, Testudines, Choristodera, Crocodylia, Squamata) from the Upper Oligocene of Oberleichtersbach (Northern Bavaria, Germany)2
- Les vertébrés terrestres de l’Oligocène inférieur de Belgique (Formation de Borgloon, MP 21): inventaire et interprétation des données actuelles2
- Pleistocene vertebrate faunas of Hungary2
- Fossil amphibians and reptiles from Tegelen (Province of Limburg) and the early Pleistocene palaeoclimate of The Netherlands1
Each of the 77 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. 16 further references are not listed. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content2
Picture of Triturus
- Source
- Wikipedia/Commons
- Credit
- Eduard Solà
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
CT scan
- Source
- MorphoSource
- Licence
- In Copyright
- Commercial use
- cannot be read from the licence given — check the record
- Specimen
- Triturus cristatus · FMNH:Amphibians and Reptiles:84926
Smithsonian Open Access was not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Source
- Wikipedia, “Triturus”
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itSalamandridae through timeFormations of the PleistoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Rafinesque 1815