Khurendukhosaurus is a genus of choristodere, a type of amphibious reptile. It is known from Lower Cretaceous rocks of Mongolia and Russia. Two species have been named. The type species, K. orlovi, was named in 1984 by Sigogneau–Russell and Efimov for the fragmentary postcranial skeleton PIN 3386/3. This specimen was discovered in the Albian-age Lower Cretaceous Khuren Dukh Formation Formation at Hüren Dukh, central Mongolia. The lake deposits at this site also contain fossils of the choristoderes Irenosaurus and Tchoiria. Other postcranial bones of K. orlovi have been found at this site as well.
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| - Khurendukhosaurus (fr)
- Khurendukhosaurus (en)
- 후렌덕호사우루스 (ko)
- 呼伦杜赫龙属 (zh)
|
| rdfs:comment
| - Khurendukhosaurus est un genre éteint et fossile de choristodères, un type de « reptiles » amphibies. Il est connu dans les sédiments du Crétacé inférieur de Mongolie et de Russie. (fr)
- 후렌덕호사우루스(학명:Khurendukhosaurus orlovi Sigogneau–Russell & Efimov)는 도마뱀아목에 이케초사우루스과에 속하는 도마뱀이다. 지금은 멸종한 종으로 몸길이가 1m인 중형급의 도마뱀에 속한다. (ko)
- Khurendukhosaurus is a genus of choristodere, a type of amphibious reptile. It is known from Lower Cretaceous rocks of Mongolia and Russia. Two species have been named. The type species, K. orlovi, was named in 1984 by Sigogneau–Russell and Efimov for the fragmentary postcranial skeleton PIN 3386/3. This specimen was discovered in the Albian-age Lower Cretaceous Khuren Dukh Formation Formation at Hüren Dukh, central Mongolia. The lake deposits at this site also contain fossils of the choristoderes Irenosaurus and Tchoiria. Other postcranial bones of K. orlovi have been found at this site as well. (en)
- 呼伦杜赫龙属（学名：Khurendukhosaurus）是离龙目下的一个属，它被发现于蒙古和俄罗斯的下白垩纪岩石。该属目前有两个物种被命名，模式种K.orlovi的化石标本在1984年被Sigogneau-Russell和Efimov命名为颅后骨骼碎片针3386/3。这一标本发现于蒙古中部的阿普第阶下白垩统Hühteeg-Svita组。该地的湖泊沉积物中还发现了伊克昭龙属和Tchoiria的化石以及K.orlovi的其他颅后骨骼。 第二个物种K.bajkalensis的标本于1996年被Efimov命名为PIN 2234/201，由一个肩胛骨和一根肋骨组成。这些骨骼发现于俄罗斯布里亚特省Gusinoye湖的下白垩世Murtoi地层。第一种俄罗斯离龙目由Efimov和Storrs在2000年发现，由于化石稀少，很难与K.orlovi区分开，因为材料数量。Skutschas（2008）的报告支持在俄罗斯发现的离龙目化石在呼伦杜赫龙属中的位置的额外材料，但发现K.bajkalensis在该属中的分类是可疑的。从Batylykh地层中发现了一个不确定的物种。 (zh)
|
| foaf:depiction
| |
| dcterms:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| sameAs
| |
| dbp:wikiPageUsesTemplate
| |
| thumbnail
| |
| authority
| - Sigogneau–Russell & Efimov, 1984 (en)
|
| display parents
| |
| fossil range
| |
| image caption
| - Specimen MPC-MX 1/107, Khurendukhosaurus .sp (en)
|
| subdivision
| - *K. orlovi (Sigogneau–Russell & Efimov, 1984 )
*K. bajkalensis (Efimov, 1986) (en)
|
| taxon
| |
| has abstract
| - Khurendukhosaurus is a genus of choristodere, a type of amphibious reptile. It is known from Lower Cretaceous rocks of Mongolia and Russia. Two species have been named. The type species, K. orlovi, was named in 1984 by Sigogneau–Russell and Efimov for the fragmentary postcranial skeleton PIN 3386/3. This specimen was discovered in the Albian-age Lower Cretaceous Khuren Dukh Formation Formation at Hüren Dukh, central Mongolia. The lake deposits at this site also contain fossils of the choristoderes Irenosaurus and Tchoiria. Other postcranial bones of K. orlovi have been found at this site as well. Second species K. bajkalensis was named by Efimov in 1996 for PIN 2234/201, consisting of a scapulocoracoid and a rib. These bones were found in the Lower Cretaceous Murtoi Formation at Lake Gusinoye, Buryatia, Russia. The first Russian choristodere, Efimov and Storrs (2000) found it difficult to distinguish from K. orlovi based on the small amount of material. Skutschas (2008) reported on additional material which supported the placement of the Russian taxon within Khurendukhosaurus, but found the species K. bajkalensis to be dubious within the genus. An indeterminate species is known from the Batylykh Formation. Khurendukhosaurus was a small choristodere, approximately 1 metre (3.3 ft) long at most. Efimov and Storrs regarded it as a basal member of Choristodera, but Skutschas was unable to confirm this in a phylogenetic analysis. It may have been related to the hyphalosaurids, a group of long–necked choristoderes. The neural spines of the tail are elongate, suggesting that it swam by using a tall tail. In 2019, another partial skeleton (MPC-MX 1/107) of the taxon was described from the Khuren Dukh Formation, confirming the presence of a long neck with at least 13 cervical vertebrae. A phylogenetic analysis found it to be the most basal hyphalosaurid. Phylogeny from the analysis of Dong and colleagues (2020): (en)
- Khurendukhosaurus est un genre éteint et fossile de choristodères, un type de « reptiles » amphibies. Il est connu dans les sédiments du Crétacé inférieur de Mongolie et de Russie. (fr)
- 후렌덕호사우루스(학명:Khurendukhosaurus orlovi Sigogneau–Russell & Efimov)는 도마뱀아목에 이케초사우루스과에 속하는 도마뱀이다. 지금은 멸종한 종으로 몸길이가 1m인 중형급의 도마뱀에 속한다. (ko)
- 呼伦杜赫龙属（学名：Khurendukhosaurus）是离龙目下的一个属，它被发现于蒙古和俄罗斯的下白垩纪岩石。该属目前有两个物种被命名，模式种K.orlovi的化石标本在1984年被Sigogneau-Russell和Efimov命名为颅后骨骼碎片针3386/3。这一标本发现于蒙古中部的阿普第阶下白垩统Hühteeg-Svita组。该地的湖泊沉积物中还发现了伊克昭龙属和Tchoiria的化石以及K.orlovi的其他颅后骨骼。 第二个物种K.bajkalensis的标本于1996年被Efimov命名为PIN 2234/201，由一个肩胛骨和一根肋骨组成。这些骨骼发现于俄罗斯布里亚特省Gusinoye湖的下白垩世Murtoi地层。第一种俄罗斯离龙目由Efimov和Storrs在2000年发现，由于化石稀少，很难与K.orlovi区分开，因为材料数量。Skutschas（2008）的报告支持在俄罗斯发现的离龙目化石在呼伦杜赫龙属中的位置的额外材料，但发现K.bajkalensis在该属中的分类是可疑的。从Batylykh地层中发现了一个不确定的物种。 呼伦杜赫龙属是一类小型的离龙目，长约1米（3.3英尺）。Efimov和Storrs认为它是离龙目的基干种类，但Skutschas在系统发育分析中无法证实这一点。它可能与有关，这是一类有着长脖子的离龙目。呼伦杜赫龙属的尾部神经棘是拉长的，表明它是用一条长尾巴游泳的。 (zh)
|
| gold:hypernym
| |
| prov:wasDerivedFrom
| |
| page length (characters) of wiki page
| |
| foaf:isPrimaryTopicOf
| |
| is Link from a Wikipage to another Wikipage
of | |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)
