Fossil Frogs of the Late Clarendonian (Late Miocene) Pratt Slide Local Fauna of Nebraska, with the Description of a New Genus

2015 ◽  
Vol 49 (1) ◽  
pp. 143-149 ◽  
Author(s):  
Dennis Parmley ◽  
Robert Chandler ◽  
Linda Chandler
Keyword(s):  
Late Miocene ◽  
New Genus ◽  
Local Fauna

The Diet of Pliohippus potosinus [Equidae, Mammalia] from the Late Miocene Paso del Águila Local Fauna, San Luis Potosí, México

2021 ◽  
Vol 55 (8) ◽  
pp. 923-929
Author(s):  
V. A. Pérez-Crespo ◽  
I. Ferrusquía-Villafranca ◽  
J. E. Ruiz-González ◽  
J. R. Torres-Hernández ◽  
E. Cienfuegos-Alvarado ◽  
...  
Keyword(s):  
Late Miocene ◽  
Local Fauna ◽  
San Luis ◽  
San Luis Potosi ◽  
San Luis Potosí

A new genus and species of Sieblosiidae from the Middle Miocene of Germany (Odonata: Epiproctophora)

Zootaxa ◽  
2012 ◽  
Vol 3582 (1) ◽  
pp. 64
Author(s):  
ANDRÉ NEL ◽  
GUNTHER FLECK
Keyword(s):  
Late Miocene ◽  
Middle Miocene ◽  
New Genus ◽  
New Genus And Species ◽  
The Third

Germanostenolestes lutzi, new genus and species of Sieblosiidae is described from the Middle Miocene of Öhningen (Germany). It probably belongs to the clade (Paraoligolestes + (Parastenolestes (Germanolestes + Stenolestes))) sensu Nel et al. (2005). It is the third representative of the Sieblosiidae described from this outcrop, showing that this family was still quite diverse in the Middle-Late Miocene.

First mammals from the Paleocene Porcupine Hills Formation of southwestern Alberta, Canada

2013 ◽  
Vol 50 (3) ◽  
pp. 355-378 ◽  
Author(s):  
Craig S. Scott ◽  
Daniel N. Spivak ◽  
Arthur R. Sweet
Keyword(s):  
New Species ◽  
New Genus ◽  
Western Canada ◽  
New Genus And Species ◽  
Local Fauna ◽  
Arid Conditions ◽  
First Occurrence ◽  
The City ◽  
Semi Arid ◽  
Lithological Unit

Although mammals of Paleocene age are well known from Alberta, their record is largely restricted to one lithological unit, the Paskapoo Formation (a record that includes mammals from the Cochrane area erroneously attributed to the Porcupine Hills Formation). We report here the first occurrence of Paleocene mammals from the Porcupine Hills Formation at exposures near the western edge of the city of Calgary. The assemblage, termed the Bearspaw local fauna, documents a diversity of multituberculate and eutherian mammals, including new species of the pentacodontid Aphronorus bearspawensis sp. nov., the mixodectid Eudaemonema bohachae sp. nov., the hyopsodontid Promioclaenus thnetus sp. nov., and a new genus and species of multituberculate (Alopocosmodon hadrus gen. et sp. nov.) tentatively referred to the Microcosmodontidae. The Bearspaw local fauna also details the first Canadian occurrences of several taxa, including Ptilodus wyomingensis, Aphronorus fraudator, Bryanictis microlestes, Elpidophorus minor, and possibly Goniacodon. Preliminary biostratigraphic analyses suggest that the Bearspaw local fauna is middle Torrejonian (To2) in age, correlating most closely with near-coeval Gidley Quarry of Montana and Rock Bench Quarry of Wyoming. In addition to improving the depauperate record of Torrejonian mammals in western Canada, the new fauna is important in documenting a mammal assemblage from a lithological unit that is thought to have been deposited in semi-arid conditions, rather than the wetter and more humid conditions of the Paskapoo Formation. Further, the Bearspaw localities, along with several other recently discovered localities in the Calgary and Cochrane areas, closely bracket the 27n–26r chron boundary and as such will be important in detailing the Torrejonian–Tiffanian transition in western Canada.

scholarly journals A new enigmatic Late Miocene mylodontoid sloth from northern South America

2015 ◽  
Vol 2 (2) ◽  
pp. 140256 ◽  
Author(s):  
Ascanio D. Rincón ◽  
H. Gregory McDonald ◽  
Andrés Solórzano ◽  
Mónica Núñez Flores ◽  
Damián Ruiz-Ramoni
Keyword(s):  
South America ◽  
Late Miocene ◽  
Preliminary Analysis ◽  
New Genus ◽  
New Taxon ◽  
New Genus And Species ◽  
Consensus Tree ◽  
Discriminate Analysis ◽  
Northern South America ◽  
Phylogenetic Affinities

A new genus and species of sloth ( Eionaletherium tanycnemius gen. et sp. nov.) recently collected from the Late Miocene Urumaco Formation, Venezuela (northern South America) is herein described based on a partial skeleton including associated femora and tibiae. In order to make a preliminary analysis of the phylogenetic affinities of this new sloth we performed a discriminate analysis based on several characters of the femur and tibia of selected Mylodontoidea and Megatherioidea sloths. The consensus tree produced indicates that the new sloth, E. tanycnemius , is a member of the Mylodontoidea. Surprisingly, the new taxon shows some enigmatic features among Neogene mylodontoid sloths, e.g. femur with a robust lesser trochanter that projects medially and the straight distinctly elongated tibia. The discovery of E. tanycnemius increases the diversity of sloths present in the Urumaco sequence to ten taxa. This taxon supports previous studies of the sloth assemblage from the Urumaco sequence as it further indicates that there are several sloth lineages present that are unknown from the better sampled areas of southern South America.

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