Biology:Protostega

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Short description: Genus of reptiles

Protostega
Temporal range: Late Cretaceous, 83.5 Ma
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Protostega Gigas.jpg
Mounted skeleton
Scientific classification e
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Order: Testudines
Suborder: Cryptodira
Family: †Protostegidae
Genus: †Protostega
Cope, 1872
Type species
†Protostega gigas
Cope, 1872

Protostega ('first roof')[1] is an extinct genus of sea turtle containing a single species, Protostega gigas. Its fossil remains have been found in the Smoky Hill Chalk formation of western Kansas (Hesperornis zone, dated to 83.5 million years ago[2]), time-equivalent beds of the Mooreville Chalk Formation of Alabama[3] and Campanian beds of the Rybushka Formation (Saratov Oblast, Russia ).[4] Fossil specimens of this species were first collected in 1871, and named by Edward Drinker Cope in 1872.[5] With a total length of 3.9 metres (13 ft), it is the second-largest sea turtle that ever lived, second only to the giant Archelon,[6] and one of the three largest turtle of all time along Archelon and Gigantatypus.[7]

Protostega skeletal reconstruction in the Rocky Mountain Dinosaur Resource Center, Woodland Park, Colorado

Discovery and history

The first known Protostega specimen (YPM 1408) was collected on July 4 by the 1871 Yale College Scientific Expedition, close to Fort Wallace and about 5 months before Cope arrived in Kansas. However the fossil that they found was never described or named.[8] It wasn't until E. D. Cope found and collected the first specimen of Protostega gigas in the Kansas chalk in 1871. A variety of bones were found in yellow cretaceous chalk from a bluff near Butte Creek.[9][10]

Paleoenvironment

The Late Cretaceous was marked by high temperatures, with large epicontinental seaways.[11] During the Mid-to Late Cretaceous period the Western Interior Seaway covered the majority of North America and would connect to the Boreal and Tethyan oceans at times.[12][13] Within these regions are where the fossil of Protostega gigas have been found.[14][15]

Life restoration

Description

Protostega is known to have reached up to 3–3.9 m (9.8–12.8 ft) in length.[2][6][4] A specimen from the upper Taylor Marl is even larger, at 2 m (6.6 ft) in carapace length and 4.2 m (14 ft) in total length.[16][6] Despite lacking its head and three limbs, it is well-preserved.[16] Cope's Protostega gigas discovery reveled that their shell had a reduction of ossification that helped these huge animals with streamlining in the water and weight reduction.[17] The carapace was greatly reduced and the disk only extending less than half way towards the distal ends of the ribs. Cope described other greatly modified bones in his specimen including an extremely long coracoid process that reached all the way to the pelvis and a humerus that resembled a Dermochelys.[18] Creating better movement of their limbs.

Body structure of fossilized Protostega

Skull Structure: Edward Cope described the uniqued Protostega gigas to have a large jugal that reached to the quadrate along with a thickened pterygoid that reached to the mandibular articulating surface of the quadrate.[1] The fossil featured a reduction in the posterior portion of the vomer where the palatines meet medially.[1] Another fossilized specimen showed a bony extension, that would have been viewed as a beak, was lacking in the Protostega genus.[8] The premaxillary beak was very shorter than that of Archelon.[18] In front of the orbital region was elongated with broadly roofed temporal region. The jaws of the fossil showed a large crushing -surfaces.[18] The quadrato-jugal was triangular with a posterior edge that was concave and the entire bone was convex from distal view. The squamosal appeared to have a concave formation on the surface at the upper end of the quadrate. In Cope's fossil the mandible was preserved almost perfectly and from this he recorded that the jaw was very similar to the Cheloniidae and the dentary had a broad for above downward with a concave surface, marked by deep pits in the dentary.[19] Cope concluded that these animals were most likely omnivores and consumed a diet of hard shelled crustacean creatures, due to the long symphysis of its lower jaw.[18] Along with probably consisted of seaweed and jellyfish or scavenged on floating carcasses as well, like modern turtles.[6]

Classification

The classification of Protostega was complicated at best. The specimen that Cope discovered in Kansas was hard to evaluate with the preservation condition. The fossil shared many characteristics with two other recorded genus named Dermochelys and Cheloniidae. Cope wrote about the characteristics that distinctly separated this particular species from the two controversial groups. The differences he described were that the fossil had a reduced or lacking amount of dermal ossification on the back, the articulation of the pterygoid and quadrates, presplenial bone in the jaw was present, no articular process on the back side of the nuchal, simple formation of the radial process on the humerus and a peculiar bent formation of the xiphiplastra. He concluded that genus Protostega and species Protostega gigas was an intermediate form of the two groups Dermochelys and Cheloniidae.[19]

Paleobiology

Examining the bone tissue microstructure (osteohistology) of the Protostega revealed growth patterns similar to modern leatherback sea turtles with rapid growth to large body size. Leatherbacks don't have a typical reptile metabolism, since they have high resting metabolic rates and can hold a body temperature higher than their surroundings. If Protostega had similar bone growth patterns to leatherbacks, it is hypothesized that they both had a similar metabolism. This rapid growth to adult body size in sea turtles would also indicate rapid growth to reproductive maturity, which would have been a great advantage in their survival. However, comparing Protostega to its more basal relative Desmatochelys shows that not all protostegids had the same growth patterns. This indicates that rapid growth to large size evolved late within the lineage, perhaps in response to the evolution of large mosasaurs like Tylosaurus. Given uncertainties in the phylogenetic placement of protostegids relative to living sea turtles, it is unclear if the evolution of rapid growth rates and possible elevated metabolism were convergent with modern leatherbacks or if the two were more closely related.[20]

See also

References

  1. ↑ 1.0 1.1 1.2 Hirayama, Ren (1994). "Phylogenetic systematics of chelonioid sea turtles" (in en). Island Arc 3 (4): 270–284. doi:10.1111/j.1440-1738.1994.tb00116.x. ISSN 1440-1738. 
  2. ↑ 2.0 2.1 Carpenter, K. (2003). "Vertebrate Biostratigraphy of the Smoky Hill Chalk (Niobrara Formation) and the Sharon Springs Member (Pierre Shale)." High-Resolution Approaches in Stratigraphic Paleontology, 21: 421-437. doi:10.1007/978-1-4020-9053-0
  3. ↑ Kiernan, Caitlin R. (2002). "Stratigraphic distribution and habitat segregation of mosasaurs in the Upper Cretaceous of western and central Alabama, with an historical review of Alabama mosasaur discoveries". Journal of Vertebrate Paleontology 22 (1): 91–103. doi:10.1671/0272-4634(2002)022[0091:SDAHSO2.0.CO;2]. 
  4. ↑ 4.0 4.1 Danilov, I. G.; Obraztsova, E. M.; Arkhangelsky, M. S.; Ivanov, A. V.; Averianov, A. O. (2022). "Protostega gigas and other sea turtles from the Campanian of Eastern Europe, Russia". Cretaceous Research 135: Article 105196. doi:10.1016/j.cretres.2022.105196. https://www.researchgate.net/publication/359189888. 
  5. ↑ Cope, Edward Drinker (1872). "A description of the genus Protostega". Proceedings of the Academy of Natural Sciences of Philadelphia: 422–433. 
  6. ↑ 6.0 6.1 6.2 6.3 Mike Everhart. "Marine turtles from the Western Interior Sea". http://oceansofkansas.com/turtles.html. 
  7. ↑ H. F. Kaddumi (2006). "A new genus and species of gigantic marine turtles (Chelonioidea: Cheloniidae) from the Maastrichtian of the Harrana Fauna-Jordan". PalArch's Journal of Vertebrate Palaeontology 3 (1): 1–14. http://www.palarch.nl/wp-content/kaddumi_hf_a_new_genus_and_species_of_gigantic_marine_turtles_chelonioidea_cheloniidae_from_the_maastrichtian_of_the_harrana_fauna_jordan_palarchs_journal_of_vertebrate_palaeontology_3_1_20061.pdf. Retrieved 2010-02-04. 
  8. ↑ 8.0 8.1 "Protostega_dig-2011". http://oceansofkansas.com/ProtostegaDig.html. 
  9. ↑ Cope, Edward (1871). "A Description of the Genus Protostega, a Form of Extinct Testudinata". Proceedings of the American Philosophical Society 12 (86): 422–433. https://duwamish.lib.washington.edu/uwnetid/illiad.dll?Action=10&Form=75&Value=1861494. 
  10. ↑ Wiffen, J. (1981-03-01). "The first Late Cretaceous turtles from New Zealand". New Zealand Journal of Geology and Geophysics 24 (2): 293–299. doi:10.1080/00288306.1981.10422718. ISSN 0028-8306. 
  11. ↑ Dennis, K. J.; Cochran, J. K.; Landman, N. H.; Schrag, D. P. (2013-01-15). "The climate of the Late Cretaceous: New insights from the application of the carbonate clumped isotope thermometer to Western Interior Seaway macrofossil" (in en). Earth and Planetary Science Letters 362: 51–65. doi:10.1016/j.epsl.2012.11.036. ISSN 0012-821X. Bibcode: 2013E&PSL.362...51D. 
  12. ↑ Schröder-Adams, Claudia J.; Cumbaa, Stephen L.; Bloch, John; Leckie, Dale A.; Craig, Jim; Seif El-Dein, Safaa A.; Simons, Dirk-Jan H. A. E.; Kenig, Fabien (2001-06-15). "Late Cretaceous (Cenomanian to Campanian) paleoenvironmental history of the Eastern Canadian margin of the Western Interior Seaway: bonebeds and anoxic events" (in en). Palaeogeography, Palaeoclimatology, Palaeoecology 170 (3): 261–289. doi:10.1016/S0031-0182(01)00259-0. ISSN 0031-0182. Bibcode: 2001PPP...170..261S. 
  13. ↑ Petersen, Sierra V.; Tabor, Clay R.; Lohmann, Kyger C.; Poulsen, Christopher J.; Meyer, Kyle W.; Carpenter, Scott J.; Erickson, J. Mark; Matsunaga, Kelly K. S. et al. (2016-11-01). "Temperature and salinity of the Late Cretaceous Western Interior Seaway" (in en). Geology 44 (11): 903–906. doi:10.1130/G38311.1. ISSN 0091-7613. Bibcode: 2016Geo....44..903P. 
  14. ↑ "Mooreville Chalk" (in en), Wikipedia, 2019-12-16, https://en.wikipedia.org/w/index.php?title=Mooreville_Chalk&oldid=931029488, retrieved 2020-03-04 
  15. ↑ Lutz, Peter L.; Musick, John A. (1996). The Biology of Sea Turtles. CRC Press. p. 10. ISBN 978-0-8493-8422-6. https://books.google.com/books?id=fhm2yGTBiN8C&q=Protostega&pg=PA10. 
  16. ↑ 16.0 16.1 Derstler, K.; Leitch, A. D.; Larson, P. L.; Finsley, C.; Hill, L. (1993). "The World's Largest Turtles - The Vienna Archelon (4.6 m) and the Dallas Protostega (4.2 m), Upper Cretaceous of South Dakota and Texas". Journal of Vertebrate Paleontology 13 (suppl. to no. 3) (33A). https://www.academia.edu/2394297. 
  17. ↑ "Protostega gigas by Triebold Paleontology, Inc.". http://trieboldpaleontology.com/protostega.html. 
  18. ↑ 18.0 18.1 18.2 18.3 Carnegie Institution of Washington (1908). Carnegie Institution of Washington publication. MBLWHOI Library. Washington, Carnegie Institution of Washington. https://archive.org/details/carnegieinstitut75carn. 
  19. ↑ 19.0 19.1 Case, Ermine Cowles (1897) (in en). On the Osteology and Relationships of Protostega. Ginn. https://books.google.com/books?id=icrRAAAAMAAJ&q=protostega+classification&pg=PA21. 
  20. ↑ Wilson, Laura E. (2023). "Rapid growth in Late Cretaceous sea turtles reveals life history strategies similar to extant leatherbacks". PeerJ 11: e14864. doi:10.7717/peerj.14864. PMID 36793890. 

Wikidata ☰ Q1051251 entry



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