Biology:Pantodonta
Pantodonta | |
---|---|
Barylambda | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Mammalia |
Clade: | Paraxonia |
Order: | †Pantodonta Cope 1873 |
Subgroups | |
|
Pantodonta is an extinct suborder (or, according to some, an order) of eutherian mammals. These herbivorous mammals were one of the first groups of large mammals to evolve (around 66 million years ago) after the end of the Cretaceous. The last pantodonts died out at the end of the Eocene (around 34 million years ago).
Pantodonta include some of the largest mammals of their time, but were a diversified group, with some primitive members weighing less than 10 kg (22 lb) and the largest more than 500 kg (1,100 lb).[1]
The earliest and most primitive pantodonts, Bemalambda (with a 20 cm (7.9 in) skull probably the size of a dog) and Hypsilolambda, appear in the early Paleocene Shanghuan Formation in China. All more derived families are collectively classified as Eupantodonta. The pantodonts appear in North America in the middle Paleocene, where Coryphodon survived into the middle Eocene. Pantodont teeth have been found in South America (Alcidedorbignya) and Antarctica,[2] and footprints in a coal mine on Svalbard.[3]
Description
The pantodonts varied considerably in size: the small Archaeolambda, of which there is a complete skeleton from the Late Palaeocene of China, was probably arboreal, while the North American, ground sloth-like Barylambda was massive, slow-moving ("graviportal") and probably browsed on high vegetation.[2]
Dentition
The pantodonts have a primitive dental formula (3.1.4.33.1.4.3) with little or no diastemata. Their most important synapomorphy are the zalambdodont (V-shaped ectoloph opening towards lip) P3–4 and (except in the most primitive families) dilambdodont (W-shaped ectoloph) upper molars. Most pantodonts lacked a hypocone (fourth cusp) and had small conules (additional small cusps). The incisors are small but the canines large, occasionally sabertooth-like. On P3-M3 there is normally an ectoflexus (indentation on the outer side). Asian families can typically be distinguished from the American because their paracone and metacone (bottom of W on side of tongue) tend to be closer together.[1]
The cheek teeth in the lower jaw are also dilambdodont, with broad, high metalophids (posterior crest) and tall metaconid (posterior-interior cusp) with much lower paracristids and small paraconids.[1]
Postcranial skeleton
Pantodonts have plesiomorphic (unaltered) and robust postcranial skeletons. Their five-toed feet are often hoofed with the tarsals similar to those of ungulates, which feature had led to previously suggested ties to arctocyonid "condylarths", but this similarity is now considered primitive.[1]
Classification
The pantodonts were previously grouped with the ungulates as amblypods, paenungulates, or arctocyonids, but since McKenna & Bell 1997 they have been allied with the tillodonts and considered to be derived from the cimolestids. The interrelationship within Pantodonta is controversial,[2] but, following McKenna & Bell 1997, it contains about two dozen genera in ten families. Most of the families are known from the Paleocene of either Asia or North America. The pantolambdodontids and coryphodontids survived into the Eocene and the latter are known from across the northern hemisphere.[1] Some dental features can possibly link the most primitive pantodonts to the palaeoryctids, a group of small and insectivorous mammals that evolved during the Cretaceous.[2] Recently a close relationship with Periptychidae has been suggested.[4] This would make pantodonts crown-group ungulate placentals and not related to cimolestids at all.
Genera from North America tended to be large and robust, starting with Pantolambda and Caenolambda in the Middle Paleocene epoch, and later in the epoch started to get larger, with Barylambda as the largest Paleocene form of pantodont. However, Asian forms, such as Archaeolambda, tended to be thinner and less robust, around the size of a medium-sized dog. Only later in the Eocene, with Hypercoryphodon, did Asian pantodonts get large and robust.
Timeline of genera
<timeline> ImageSize = width:850px height:auto barincrement:15px PlotArea = left:10px bottom:50px top:10px right:10px
Period = from:-66 till:-23.03 TimeAxis = orientation:horizontal ScaleMajor = unit:year increment:10 start:-60 ScaleMinor = unit:year increment:1 start:-66 TimeAxis = orientation:hor AlignBars = justify
Colors =
#legends id:CAR value:claret id:ANK value:rgb(0.4,0.3,0.196) id:HER value:teal id:HAD value:green id:OMN value:blue id:black value:black id:white value:white id:paleogene value:rgb(0.99,0.6,0.32) id:paleocene value:rgb(0.99,0.65,0.37) id:eocene value:rgb(0.99,0.71,0.42) id:oligocene value:rgb(0.99,0.75,0.48)
BarData=
bar:eratop bar:space bar:periodtop bar:space bar:NAM1 bar:NAM2 bar:NAM3 bar:NAM4 bar:NAM5 bar:NAM6 bar:space bar:period bar:space bar:era
PlotData=
align:center textcolor:black fontsize:M mark:(line,black) width:25 shift:(7,-4)
bar:periodtop from: -66 till: -56 color:paleocene text:Paleocene from: -56 till: -33.9 color:eocene text:Eocene from: -33.9 till: -23.03 color:oligocene text:Oligocene
bar:eratop from: -66 till: -23.03 color:paleogene text:Paleogene
PlotData=
align:left fontsize:M mark:(line,white) width:5 anchor:till align:left color:paleocene bar:NAM1 from:-64 till:-61 text: Alcidedorbignya color:paleocene bar:NAM2 from:-63 till:-57 text: Pantolambda color:paleocene bar:NAM3 from:-60 till:-50 text: Barylambda color:paleocene bar:NAM4 from:-59 till:-56 text: Titanoides color:paleocene bar:NAM5 from:-57 till:-46 text: Coryphodon color:eocene bar:NAM6 from:-37 till:-34 text: Hypercoryphodon
PlotData=
align:center textcolor:black fontsize:M mark:(line,black) width:25
bar:period from: -66 till: -56 color:paleocene text:Paleocene from: -56 till: -33.9 color:eocene text:Eocene from: -33.9 till: -23.03 color:oligocene text:Oligocene
bar:era from: -66 till: -23.03 color:paleogene text:Paleogene
</timeline>
References
- "On the short footed Ungulata of the Eocene of Wyoming". Proceedings of the American Philosophical Society 13: 38–74. 1873. https://archive.org/stream/proceedingsofame13amer#page/38/mode/2up. Retrieved 1 July 2013.
- Kemp, Tom S. (2005). The Origin and Evolution of Mammals. Oxford University Press. ISBN 978-0198507611. OCLC 56652579.
- Classification of Mammals Above the Species Level. New York: Columbia University Press. 1997. ISBN 978-0231110136. OCLC 37345734.
- Rose, Kenneth David (2006). The beginning of the age of mammals. Baltimore: JHU Press. ISBN 978-0801884726. https://books.google.com/books?id=3bs0D5ix4VAC.
- "†PANTODONTA - pantodonts". After McKenna & Bell (1997), and Alroy (2002). http://www.helsinki.fi/~mhaaramo/metazoa/deuterostoma/chordata/synapsida/eutheria/cimolesta/pantodonta.html.
Footnotes
- ↑ 1.0 1.1 1.2 1.3 1.4 Rose 2006, p. 114
- ↑ 2.0 2.1 2.2 2.3 Kemp 2005, pp. 238–40
- ↑ "Fossil Arctic animal tracks point to climate risks". Reuters. April 25, 2007. https://www.reuters.com/article/scienceNews/idUSL2441335120070425?src=042507_0835_ARTICLE_PROMO_also_on_reuters.
- ↑ Halliday, Thomas J.D.; Upchurch, Paul; Goswami, Anjali (February 2017). "Resolving the relationships of Paleocene placental mammals". Biological Reviews 92 (1): 521–55–. doi:10.1111/brv.12242. PMID 28075073. PMC 6849585. http://discovery.ucl.ac.uk/1473028/1/Halliday_et_al-Biological_Reviews.pdf.
External links
Wikidata ☰ Q132156 entry
Original source: https://en.wikipedia.org/wiki/Pantodonta.
Read more |