Information about Hesperornis

Hesperornis
Fossil range: Late Cretaceous (Coniacian -? Maastrichtian)

Hesperornis regalis
Conservation status
Extinct (fossil)
Scientific classification
Kingdom:Animalia
Phylum:Chordata
Class:Aves
Subclass:Hesperornithes
Order:Hesperornithiformes
Family:Hesperornithidae
Genus:Hesperornis
Marsh, 1872
Species
  • H. bairdi
  • H. chowi
  • H. crassipes
  • H. gracilis
  • H. macdonaldi
  • H. mengeli
  • H. regalis
  • H. rossicus (formerly rossica)


Hesperornis is an extinct genus of flightless aquatic birds that lived during the Coniacian to Maastrichtian sub-epochs of the Late Cretaceous (89-65 mya). One of the lesser known discoveries of Marsh in the late 19th century Bone Wars, it was an important early find in the history of avian paleontology. Famous locations for Hesperornis are the Late Cretaceous marine limestones from Kansas and the marine shales from Canada, but the genus had probably a Holarctic distribution.

Description

Hesperornis were very large birds, reaching up to 2 meters (6.5 feet) in length. They had virtually no wings, swimming with powerful hind legs. Their toes were probably lobed rather than being webbed, as in today's grebes; like in these, the toes could rotate well, which is necessary to decrease drag in lobed feet but not in webbed ones such as in loons, where the toes are simply folded together.

Like many other Mesozoic birds such as Ichthyornis, Hesperornis had teeth in its beak which were used to hold prey (most likely fish). In the hesperornithiform lineage they were of a different arrangement than in any other known bird (or in non-avian theropod dinosaurs), with the teeth sitting in a longitudinal groove rather than in individual sockets[1].

Of the many species traditionally placed in this genus - such as the famous H. regalis, the small H. gracilis or the huge H. rossicus -, not all may be valid. Some, such as H. macdonaldi, are known from very few or even a single bone and cannot be properly compared against the more plentiful (but also incomplete) remains of other similar-sized and contemporary taxa. Coniornis altus (which includes H. montana) may also belong into this genus. In addition, there are some unassigned remains, such as SGU 3442 Ve02 and LO 9067t and bones of an undetermined species from Tzimlyanskoe Reservoir near Rostov[2].

Paleobiology

Enlarge picture
Skeleton of Hesperornis regalis.
Hesperornis hunted in the waters of such contemporary shelf seas as the North American Inland Sea, the Turgai Strait and the prehistoric North Sea[3], which then were subtropical to tropical waters, much warmer than today. They probably fed mainly on fish, maybe also crustaceans, cephalopods and mollusks as do the diving seabirds of today. Their teeth were helpful in dealing with slippery or hard-shelled prey.

On land, Hesperornis may or may not have been able to walk. They certainly were not able to stand upright as in the early reconstructions as the legs attached far at the back and sideways, with even the lower leg being tightly attached to the body (see photo of skeleton). Thus, they were limited to a clumsy hobble at best on land and would indeed have been more nimble if they moved by sliding on their belly or galumphing. Indeed, the leg skeleton of the hesperornithids was so much adapted to diving that their mode of locomotion while ashore, as well as where it laid its eggs and how it cared for its young is a matter of much speculation.

Some have even pointed out that it cannot be completely ruled out that these birds were ovoviviparous instead of incubating their eggs. In any case, young Hesperornis grew fairly quickly and continuously to adulthood, as is the case in modern birds, but not Enantiornithes[4]. More young birds are known from the fossil record of the more northernly sites than from locations further south. This suggests that at least some species were migratory like today's penguins which swim polewards in the summer.

Hesperornis were preyed upon by large marine carnivores. Tylosaurus proriger specimen SDSMT 10439 contains the bones of a Hesperornis in its gut, for example.

In popular culture

Enlarge picture
Primeval's Hesperornis.
Hesperornis appeared in the third episode of the Science Fiction show Primeval. In Episode three, a housewife in west London finds, water spreading through the basement. She then calls a plumber. When he comes, the plumber is then killed by a frightened Hesperornis. Later a flock of Hesperornis where shown swimming around in a tropical sea and a Hesperornis rookery was shown amongst the rocky shoreline. Here Hesperornis was deplicted as having scales when in real life, Hesperornis was likely covered in feathers.

Hesperornis was also shown in the last episode of the Walking with... series spin-off Sea Monsters, being frequently attacked and devoured by larger predators such as Xiphactinus and Halisaurus

Footnotes

1. ^ Discussed in detail by Marsh (1880) and Gregory (1952).
2. ^ The former two bones are probably H. rossicus; some remains assigned to that species in turn seem to belong to the latter undetermined taxon (Rees & Lindgren 2005).
3. ^ Hills et al. (1999), Rees & Lindgren (2005).
4. ^ Chinsamy et al. (1998)

References

  • Chinsamy A, Martin, Larry D. & Dobson, P. (1998): Bone microstructure of the diving Hesperornis and the volant Ichthyornis from the Niobrara Chalk of western Kansas. Cretaceous Research 19(2): 225-235. doi:10.1006/cres.1997.0102 (HTML abstract)
  • Everhart, Mike (2007): Oceans of Kansas: Hesperornis regalis Marsh 1872 - Toothed marine birds of the Late Cretaceous seas. Version of 2006-DEC-12. Retrieved 2007-AUG-23.
  • Gregory, Joseph T. (1952): The Jaws of the Cretaceous Toothed Birds, Ichthyornis and Hesperornis. Condor 54(2): 73-88. PDF fulltext
  • Hills, L. V.; Nicholls, E. L.; Núñez-Betelu, L. "Koldo" M. & McIntyre, D. J. (1999): Hesperornis (Aves) from Ellesmere Island and palynological correlation of known Canadian localities. Canadian Journal of Earth Sciences 36(9): 1583-1588. HTML abstract
  • Marsh, Othniel Charles (1880): Odontornithes, a Monograph on the Extinct Toothed Birds of North America. Government Printing Office, Washington DC.
  • Rees, Jan & Lindgren, Johan (2005): Aquatic birds from the Upper Cretaceous (Lower Campanian) of Sweden and the biology and distribution of hesperornithiforms. Palaeontology 48(6): 1321–1329. doi:10.1111/j.1475-4983.2005.00507.x (HTML abstract)
Late Cretaceous (100mya - 65mya) refers to the second half of the Cretaceous Period, named after the famous white chalk cliffs of southern England, which date from this time. Rocks deposited during the Late Cretaceous Period are referred to as the Upper Cretaceous Series.
..... Click the link for more information.
The Coniacian is a stage of the Late Cretaceous Epoch. It spans the time between 89.3 ± 1 Ma and 85.8 ± 0.7 Ma (million years ago).

References

  • GeoWhen Database - Coniacian

Cretaceous period
Lower/Early Cretaceous Upper/Late Cretaceous
..... Click the link for more information.
The Maastrichtian is the last stage of the Cretaceous period, and therefore of the Mesozoic era. It spanned from 70.6 ± 0.6 Ma to 65.5 ± 0.3 Ma (million years ago).
..... Click the link for more information.
conservation status of a species is an indicator of the likelihood of that species continuing to survive either in the present day or the future. Many factors are taken into account when assessing the conservation status of a species: not simply the number remaining, but the
..... Click the link for more information.
For other uses of the term, see Fossil (disambiguation)


FOSSIL is a standard for allowing serial communication for telecommunications programs under the DOS operating system.
..... Click the link for more information.
Scientific classification or biological classification is a method by which biologists group and categorize species of organisms. Scientific classification also can be called scientific taxonomy, but should be distinguished from folk taxonomy, which lacks scientific basis.
..... Click the link for more information.
Editing of this page by unregistered or newly registered users is currently disabled until (UTC) due to vandalism.
If you are prevented from editing this page, and you wish to make a change, please discuss changes on the talk page, request unprotection, log in, or
..... Click the link for more information.
Chordata
Bateson, 1885

Typical Classes

See below

Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
..... Click the link for more information.
Aves
Linnaeus, 1758

Orders

About two dozen - see section below

Birds (class Aves) are bipedal, warm-blooded, egg-laying vertebrate animals.
..... Click the link for more information.
Hesperornithes
Fürbringer, 1888

Order: Hesperornithiformes
Sharpe 1899

Families

Enaliornithidae
Baptornithidae
Hesperornithidae
Synonyms

Odontornithes Marsh, 1873 (partim)
..... Click the link for more information.
Hesperornithes
Fürbringer, 1888

Order: Hesperornithiformes
Sharpe 1899

Families

Enaliornithidae
Baptornithidae
Hesperornithidae
Synonyms

Odontornithes Marsh, 1873 (partim)
..... Click the link for more information.
Othniel Charles Marsh (October 29, 1831 - March 18, 1899) was one of the pre-eminent paleontologists of the 19th century, who discovered and named many fossils found in the American West.

Marsh was born in Lockport, New York.
..... Click the link for more information.
18th century - 19th century - 20th century
1840s  1850s  1860s  - 1870s -  1880s  1890s  1900s
1869 1870 1871 - 1872 - 1873 1874 1875

:
Subjects:     Archaeology - Architecture -
..... Click the link for more information.
species is one of the basic units of biological classification. A species is often defined as a group of organisms capable of interbreeding and producing fertile offspring.
..... Click the link for more information.
genus (plural: genera) is part of the Latinized name for an organism. It is a name which reflects the classification of the organism by grouping it with other closely similar organisms.
..... Click the link for more information.
Aves
Linnaeus, 1758

Orders

About two dozen - see section below

Birds (class Aves) are bipedal, warm-blooded, egg-laying vertebrate animals.
..... Click the link for more information.
The Coniacian is a stage of the Late Cretaceous Epoch. It spans the time between 89.3 ± 1 Ma and 85.8 ± 0.7 Ma (million years ago).

References

  • GeoWhen Database - Coniacian

Cretaceous period
Lower/Early Cretaceous Upper/Late Cretaceous
..... Click the link for more information.
The Maastrichtian is the last stage of the Cretaceous period, and therefore of the Mesozoic era. It spanned from 70.6 ± 0.6 Ma to 65.5 ± 0.3 Ma (million years ago).
..... Click the link for more information.
Late Cretaceous (100mya - 65mya) refers to the second half of the Cretaceous Period, named after the famous white chalk cliffs of southern England, which date from this time. Rocks deposited during the Late Cretaceous Period are referred to as the Upper Cretaceous Series.
..... Click the link for more information.
mya or "m.y.a." is an abbreviation for million years ago. This abbreviation is commonly used as a unit of time to denote length of time before the present or "B.P." (before AD 1950). Specifically, one mya is equal to 106 years ago.
..... Click the link for more information.
Othniel Charles Marsh (October 29, 1831 - March 18, 1899) was one of the pre-eminent paleontologists of the 19th century, who discovered and named many fossils found in the American West.

Marsh was born in Lockport, New York.
..... Click the link for more information.
The Bone Wars were an infamous period in the history of paleontology when the two pre-eminent paleontologists of the time, Edward Drinker Cope and Othniel Charles Marsh, competed to see who could find the most, and more sensational, new species of dinosaur.
..... Click the link for more information.
Limestone is a sedimentary rock composed largely of the mineral calcite (calcium carbonate: CaCO3). Limestone often contains variable amounts of silica in the form of chert or flint, as well as varying amounts of clay, silt and sand as disseminations, nodules, or layers
..... Click the link for more information.
State of Kansas

Flag of Kansas Seal
Nickname(s): The Sunflower State
Motto(s): Ad astra per aspera

Official language(s) English[1]

Capital Topeka
Largest city Wichita
..... Click the link for more information.
This page is currently protected from editing until disputes have been resolved.
Protection is not an endorsement of the current [ version] ([ protection log]).
..... Click the link for more information.
The Holarctic is a term used by zoologists to define the ecozone covering much of Eurasia and North America, which have often been connected by the Bering land bridge. The two regions have very similar mammal and bird fauna, with many Eurasian species having moved into North
..... Click the link for more information.
WING

City of license Dayton, Ohio
Broadcast area Dayton
Branding "ESPN 1410"
Slogan Same as branding
First air date 1921
Frequency 1410 KHZ
Format Sports Talk
ERP 5,000 watts-D/N
..... Click the link for more information.

..... Click the link for more information.

..... Click the link for more information.
The Mesozoic Era is one of three geologic eras of the Phanerozoic eon. The division of time into eras dates back to Giovanni Arduino, in the 18th century, although his original name for the era now called the 'Mesozoic' was 'Secondary' (making the modern era the 'Tertiary').
..... Click the link for more information.


This article is copied from an article on Wikipedia.org - the free encyclopedia created and edited by online user community. The text was not checked or edited by anyone on our staff. Although the vast majority of the wikipedia encyclopedia articles provide accurate and timely information please do not assume the accuracy of any particular article. This article is distributed under the terms of GNU Free Documentation License.
Herod_Archelaus


page counter