Palaeobatrachus
Palaeobatrachus is an extinct genus of frogs from Europe that existed from the middle Eocene to the middle Pleistocene, spanning almost 50 million years. They were obligately aquatic, and would have not spent much time on dry land. They are one of two genera and by far the largest genus in the family Palaeobatrachidae, which are considered to be members of Pipimorpha, related to the South American-African family Pipidae, which includes the African clawed frog and Surinam toad.

Kozuch · 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
- PalaeobatrachidaePBDB
- 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 63 million years on record.
The record covers at least 66 Mya to 2.58 Mya. No occurrence read is dated outside 72.2 Mya to 774 ka.
30 occurrences of Palaeobatrachus on record, most of them in the Miocene. 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
30 occurrences- Late Cretaceous13%
- Paleocene3%
- Oligocene33%
- Miocene43%
- Pliocene3%
- Pleistocene3%
These 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
9 formations
- Lance Formation3
- Sajovolgyi Formation3
- Borgloon Formation · Tongeren Group2
- Gaverdovsky Formation2
- Conglomérat de Cernay Formation1
- Agenais Limestone Formation1
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The named rock units Palaeobatrachus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 15 occurrences have no formation on record, which is common for older literature.
Palaeobatrachus and its relatives
MioceneWhere Palaeobatrachus and its relatives were recorded in the Miocene.
Found in the same rock
609 taxa- Pelobates12 sites
- Rana10 sites
- Lacerta8 sites
- Latonia gigantea8 sites
- Anguis7 sites
- Pelophylax7 sites
- Hyla6 sites
- Lacertidae6 sites
- Triturus6 sites
- Chelotriton paradoxus5 sites
- Colubrinae5 sites
- Lissotriton5 sites
- Pseudopus5 sites
- Vipera5 sites
- Blackia miocaenica4 sites
- Coluber4 sites
- Elaphe4 sites
- Eopelobates4 sites
- Eopelobates bayeri4 sites
- Hyla arborea4 sites
- Mioproteus caucasicus4 sites
- Natrix4 sites
- Ophisaurus4 sites
- Salamandra4 sites
The Paleobiology Database records 26 sites for Palaeobatrachus, 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
20 references- Ectothermic vertebrates (Teleostei, Allocaudata, Urodela, Anura, Testudines, Choristodera, Crocodylia, Squamata) from the Upper Oligocene of Oberleichtersbach (Northern Bavaria, Germany)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
- New discoglossid and palaeobatrachid frogs from the Late Cretaceous of Wyoming and Montana, and a review of other frogs from the Lance and Hell Creek Formations3
- Palaeobatrachid frog from the late Miocene of Northern Caucasus, Russia2
- Amphibians and Squamates from the Miocene of Felsőtárkány Basin, N-Hungary2
- Les vertébrés terrestres de l’Oligocène inférieur de Belgique (Formation de Borgloon, MP 21): inventaire et interprétation des données actuelles2
- Biostratigraphy and paleoecology of continental Tertiary vertebrate faunas in the Lower Rhine Embayment (NW-Germany)2
- Amphibians and squamate reptiles from the late Miocene of Fălciu (Eastern Romania)1
- Amphibian and reptilian fauna from the early Miocene of Echzell, Germany1
- Plio-Pleistocene amphibians and reptiles from Central Turkey: new faunas and faunal records with comments on their biochronological position based on small mammals1
- Reassessing the earliest Oligocene vertebrate assemblage of Monteviale (Vicenza, Italy)1
- Palaeobatrachus eurydices, sp. nov. (Amphibia, Anura), the last Western European palaeobatrachid1
Each of the 30 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. 8 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 content1
Picture of Palaeobatrachus
- Source
- Wikipedia/Commons
- Credit
- Kozuch
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
No 3D scan of Palaeobatrachus was found in Sketchfab.
Smithsonian Open Access and MorphoSource were not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- 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 itPalaeobatrachidae through timeFormations of the MioceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Tschudi 1839