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来自新西兰渐新世晚期的一种新的克肯齿鲸科属种,并对鲸类牙齿移位的演化进行评论。

A new genus and species of kekenodontid from the late Oligocene of New Zealand with comments on the evolution of tooth displacement in Cetacea.

作者信息

Corrie Joshua E, Fordyce R Ewan

机构信息

Department of Biology, San Diego State University, San Diego, CA, USA.

Department of Geology, University of Otago, Dunedin, New Zealand.

出版信息

J R Soc N Z. 2024 Jan 31;54(5):722-737. doi: 10.1080/03036758.2023.2297696. eCollection 2024.

Abstract

The Kekenodontidae are late-surviving archaeocetes from the Late Oligocene of Southwest Pacific that includes a single-named species, . is a new genus and species of small body-sized kekenodontid from the upper Oligocene (Chattian) Kokoamu Greensand of Otago, South Island, New Zealand. Phylogenetic analyses recover . within a monophyletic Kekenodontidae, forming a clade with an unnamed provisional kekenodontid, OU 22023. Kekenodontids are recovered crownward to basilosaurids and stemward to a paraphyletic group of toothed 'mysticetes' that are excluded from Neoceti. The analyses confirm the identification of kekenodontids as the latest-diverging archaeocetes that persisted into the Late Oligocene. The holotype OU 22394 is a juvenile individual preserving several isolated heterodont teeth with characteristics of deciduous teeth, including unmineralized pulp cavities and cheek teeth with lower-lying triangular crowns that are different from all known kekenodontids. Diphyodonty is known from Eocene archaeocetes but is unknown from geologically younger toothed cetaceans, with monophyodonty being hypothesised for all Neoceti. Inferences of diphyodonty in . would be the first instance in Cetacea from rocks geologically younger than the Eocene and would indicate diphyodonty persisted in some Late Oligocene archaeocetes.

摘要

肯氏鲸科是来自西南太平洋晚渐新世的晚期残存古鲸类,包含一个单型种。 是来自新西兰南岛奥塔哥渐新世晚期(查特阶)科科阿穆绿砂层的一个新的小型肯氏鲸科属种。系统发育分析将 归入单系的肯氏鲸科,与一个未命名的暂定肯氏鲸科OU 22023形成一个分支。肯氏鲸科在系统发育树上位于龙王鲸科上方,下方是一个被排除在新鲸类之外的并系有齿“须鲸类”群。分析证实肯氏鲸科是最晚分化的古鲸类,一直存活到晚渐新世。正模标本OU 22394是一个幼年个体,保存了几颗孤立的异型齿,具有乳牙的特征,包括未矿化的牙髓腔和冠部较低的三角形颊齿,这与所有已知的肯氏鲸科不同。双套牙在始新世古鲸类中已知,但在地质年代更晚的有齿鲸类中未知,所有新鲸类都被假设为单套牙。 在 中推断出双套牙将是鲸目动物中首次在地质年代比始新世更晚的岩石中出现,这将表明双套牙在一些晚渐新世古鲸类中仍然存在。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e503/11459822/c14a93f851b8/TNZR_A_2297696_F0001_OC.jpg

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