Astoria Formation | |
---|---|
Stratigraphic range: Miocene | |
Type | Geological formation |
Sub-units | From top to bottom: [1]
|
Underlies | Montesano Formation [2] |
Overlies | Lincoln Creek Formation [2] |
Location | |
Region | Washington (state) Oregon |
Country | United States |
The Astoria Formation (formerly known as the Astoria shales) is a geologic formation in Washington state & Oregon. It preserves fossils dating back to the early to middle Miocene (but was formerly thought to date to the Oligocene). [1]
The Astoria Formation is a thick marine formation representing a near shore, relatively shallow-water shelf deposit. [2] The formation spans a considerable amount of time, with its base considered to be lower boundary of Newportian Stage (late Early Miocene) & its top to be upper boundary of Newportian Stage (middle Middle Miocene). [1]
This article is missing information about invertebrate, microorganisum, and plant taxa.(February 2023) |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Genus | Species | Stratigraphy | Material | Notes | Images |
---|---|---|---|---|---|
Desmatophoca | D. brachycephala | East of Knappton, Washington. [3] | Skull elements. [3] | A desmatophocid. | |
D. oregonensis | Iron Mountain Bed & an unspecified horizon. [3] [4] | Multiple specimens. [3] [4] | A desmatophocid. | ||
Enaliarctos | E. emlongi | South of Big Creek, Lincoln County, Oregon. [5] | USNM 250345. [5] | A pinnipedimorph, may instead be from the Nye Mudstone.[ citation needed ] | |
E. sp. | Iron Mountain bed, Lincoln County, Oregon. [6] | Partial skeleton (UWBM 89114). [6] | A pinnipedimorph. | ||
Eodesmus | E. condoni | Iron Mountain Bed, Oregon. [7] | A nearly complete cranium. [7] | A desmatophocid. | |
Pacificotaria | P. hadromma | Iron Mountain bed, Lincoln County, Oregon. [8] | Complete cranium (LACM 127973). [8] | A pinnipedimorph. | |
Proneotherium | P. repenningi | Lincoln County, Oregon. [9] | Remains of multiple individuals. [9] | An odobenid. | |
Pteronarctos | P. goedertae | Lincoln County, Oregon. [10] | Skulls. [10] | A pinnipedimorph. |
Genus | Species | Presence | Material | Notes | Images |
---|---|---|---|---|---|
Cophocetus | C. oregonensis | North of Yaquina Bay. [4] | Associated skull, jaws & skeletal elements. [4] | A baleen whale. | |
Dilophodelphis | D. fordycei | Nye Beach, Oregon. [11] | USNM 214911. [11] | A platanistid. | |
Wimahl | W. chinookensis | Washington State [12] | A kentriodontid. | ||
Zarhinocetus | Z. donnamatsonae | Near Elma, Washington. [2] | UCMP 86139. [2] | An allodelphinid. | |
Genus | Species | Presence | Material | Notes | Images |
---|---|---|---|---|---|
Aphelops | A. sp. | Fragment of skull (USNM 187123). [4] | A rhinoceros. | ||
Tylocephalonyx | T. sp. | Iron Mountain Bed, Lincoln County, Oregon. [13] | A skull (NMNH 187129). [13] | A chalicothere. | |
Genus | Species | Presence | Material | Notes | Images |
---|---|---|---|---|---|
Diomedeidae | Gen. et. sp. indet. | East of Knappton, Washington. [14] | Partial skeleton (SMF Av 644). [14] | An albatross. | |
Genus | Species | Presence | Material | Notes | Images |
---|---|---|---|---|---|
Carcharodon | C. megalodon | North of Newport, Oregon. [15] | Species reassigned to the genus Otodus . | ||
Cetorhinus | C. piersoni | North of Newport, Oregon. [16] | Teeth. [16] | A basking shark. | |
Cosmopolitodus | C. hastalis | Coos Bay, Oregon. [15] | A tooth. [15] | A lamnid shark. | |
C. planus? | North of Newport, Oregon. [15] | A lamnid shark. | |||
Galeocerdo | G. cf. aduncus | North of Newport, Oregon. [15] | A requiem shark. | ||
Hexanchus | North of Newport, Oregon. [15] | A cow shark. | |||
Isurus | I. hastalis | Coos Bay, Oregon. [15] | A tooth. [15] | Species reassigned to Cosmopolitodus . | |
I. planus? | North of Newport, Oregon. [15] | Species reassigned to Cosmopolitodus . | |||
Myliobatis | North of Newport, Oregon. [15] | An eagle ray. | |||
Otodus | O. megalodon | North of Newport, Oregon. [15] | Originally reported as Carcharodon megalodon. | ||
Cetotherium is an extinct genus of baleen whales from the family Cetotheriidae.
Enaliarctos is an extinct genus of pinnipedimorph, and may represent the ancestor to all pinnipeds. Prior to the discovery of Puijila, the five species in the genus Enaliarctos represented the oldest known pinnipedimorph fossils, having been recovered from late Oligocene and early Miocene strata of California and Oregon.
Desmatophoca is an extinct genus of early pinniped that lived during the Miocene, and is named from the Greek "phoca", meaning seal. A taxon of the family Desmatophocidae, it shares some morphological similarities with modern true seals. Two species are recognized: Desmatophoca oregonensis and Desmatophoca brachycephala. Little information exists regarding Desmatophoca, due to the small number of fossil samples obtained and identified.
Cramauchenia is an extinct genus of litoptern South American ungulate. Cramauchenia was named by Florentino Ameghino. The name has no literal translation. Instead, it is an anagram of the name of a related genus Macrauchenia. This genus was initially discovered in the Sarmiento Formation in the Chubut Province, in Argentina, and later it was found in the Chichinales Formation in the Río Negro Province and the Cerro Bandera Formation in Neuquén, also in Argentina, in sediments assigned to the SALMA Colhuehuapian, as well as the Agua de la Piedra Formation in Mendoza, in sediments dated to the Deseadan. In 1981 Soria made C. insolita a junior synonym of C. normalis. A specimen of C. normalis was described in 2010 from Cabeza Blanca in the Sarmiento Formation, in sediments assigned to the Deseadan SALMA.
The John Day Formation is a series of rock strata exposed in the Picture Gorge district of the John Day River basin and elsewhere in north-central Oregon in the United States. The Picture Gorge exposure lies east of the Blue Mountain uplift, which cuts southwest–northeast through the Horse Heaven mining district northeast of Madras. Aside from the Picture Gorge district, which defines the type, the formation is visible on the surface in two other areas: another exposure is in the Warm Springs district west of the uplift, between it and the Cascade Range, and the third is along the south side of the Ochoco Mountains. All three exposures, consisting mainly of tuffaceous sediments and pyroclastic rock rich in silica, lie unconformably between the older rocks of the Clarno Formation below and Columbia River basalts above.
Ursoidea is a superfamily of arctoid carnivoran mammals that includes the families Subparictidae, Amphicynodontidae, and Ursidae which the last family includes the extant lineages of bears as well the extinct Hemicyoninae and Ursavinae. The interrelationships of ursoids has had slight arrangements. In the past it was thought the extinct Amphicyonidae were stem-bears based on morphological analysis of the ear region, though the most recent publications on early amphicyonids suggests they were basal caniforms. The amphicynodontids are sometimes classified as either a subfamily of bears, a paraphyletic assemblage of early bears, or even stem-pinnipeds. The subparictids were previously classified as amphicynodontine/ids. The hemicyonines have been occasionally reclassified as a separate family.
Australodelphis mirus is an extinct Pliocene dolphin. A. mirus is known from fossils found in the Sørsdal Formation, Mule Peninsula, Vestfold Hills, East Antarctica. The genus has been described as an example of convergent evolution with beaked whales.
Kentriodontidae is an extinct family of odontocete whales related to modern dolphins. The Kentriodontidae lived from the Oligocene to the Pliocene before going extinct.
The St. Marys Formation is a geologic formation in Maryland and Virginia, United States. It preserves fossils dating back to the Miocene Epoch of the Neogene period. It is the youngest Miocene formation present in the Calvert Cliffs and is part of the Chesapeake Group.
The Ashley Formation is a geologic formation in South Carolina. It preserves fossils dating back to the Paleogene period.
The Chandler Bridge Formation is a geologic formation in South Carolina. It preserves fossils dating back to the Chattian of the Paleogene period, corresponding to the Arikareean in the NALMA classification. The formation overlies the Ashley Formation and is overlain by the Edisto Formation.
The Sharps Formation is a geologic formation in South Dakota. It preserves fossils dating back to the Paleogene.
The Yaquina Formation is a geologic formation in Oregon. It preserves fossils dating back to the Paleogene period.
Pontolis is an extinct genus of large walrus. It contained three species, P. magnus, P. barroni, and P. kohnoi. Like all pinnipeds, Pontolis was a heavily built amphibious carnivore. Pontolis lived along the Pacific coast of North America along what is now the western coasts of California and Oregon between 11.608 and 5.332 million years ago, during the Miocene and Pliocene.
Annalisa Berta is an American paleontologist and professor emerita in the Department of Biology at San Diego State University.
Proneotherium is an extinct genus of pinniped that lived approximately 20.43 to 15.97 mya during the Early Miocene in what is now Oregon, U.S. It belonged to the family Odobenidae, the only extant species of which is the walrus.
Eopachyrucos is an extinct genus of interatheriid notoungulates that lived from the Middle Eocene to the Late Oligocene of Argentina and Uruguay. Fossils of this genus have been found in the Sarmiento Formation of Argentina and the Fray Bentos Formation of Uruguay.
Moqueguahippus is an extinct genus of notohippid notoungulates that lived during the Late Oligocene of what is now Peru. Fossils of this genus have been found in the Moquegua Formation of Peru, which it was named after.
{{cite book}}
: Missing or empty |title=
(help){{cite journal}}
: Cite journal requires |journal=
(help)