Epstein Files Full PDF

CLICK HERE
Technopedia Center
PMB University Brochure
Faculty of Engineering and Computer Science
S1 Informatics S1 Information Systems S1 Information Technology S1 Computer Engineering S1 Electrical Engineering S1 Civil Engineering

faculty of Economics and Business
S1 Management S1 Accountancy

Faculty of Letters and Educational Sciences
S1 English literature S1 English language education S1 Mathematics education S1 Sports Education
teknopedia

  • Registerasi
  • Brosur UTI
  • Kip Scholarship Information
  • Performance
Flag Counter
  1. World Encyclopedia
  2. Fort Union Formation
Fort Union Formation
Coordinates: 47°00′N 104°36′W / 47.0°N 104.6°W / 47.0; -104.6
From Wikipedia, the free encyclopedia
Geologic formation in the northwestern United States
Fort Union Formation
Stratigraphic range: Maastrichtian-Selandian (Lancian-Clarkforkian)
~66–58 Ma
PreꞒ
Ꞓ
O
S
D
C
P
T
J
K
Pg
N
Browniea serrata from the Fort Union Formation
TypeGeological formation
Sub-unitsAtwell Gulch, China Butte, Ekalaka, Lebo, lower Ludlow, Overland, Rock Bench Quarry, Sentinel Butte, Shotgun, Somber beds, Tongue River, Tullock, upper Ludlow, Polecat Bench Formation
UnderliesWasatch Formation
OverliesHell Creek Formation, Lance Formation
Lithology
PrimarySandstone, shale
OtherCoal
Location
Coordinates47°00′N 104°36′W / 47.0°N 104.6°W / 47.0; -104.6
Approximate paleocoordinates52°48′N 80°06′W / 52.8°N 80.1°W / 52.8; -80.1
RegionMontana, North Dakota
Wyoming, Colorado
CountryUnited States
ExtentPowder River Basin

The Fort Union Formation is a geologic unit containing sandstones, shales, and coal beds in Wyoming, Montana, and parts of adjacent states. In the Powder River Basin, it contains important economic deposits of coal, uranium, and coalbed methane.[1]

Description

[edit]

The Fort Union is mostly of Paleocene age and represents a time of extensive swamps as well as fluvial and lacustrine conditions. The rocks are more sandy in southwestern Wyoming and more coal-bearing in northeast Wyoming and southeast Montana, reflecting a general change from rivers and lakes in the west to swamps in the east, but all three environments were present at various times in most locations.[2]

Coal in the Fort Union in the Powder River Basin occurs mainly in the Tongue River Member, where as many as 32 coal seams total more than 300 feet in thickness.[1] One such bed, the Wyodak Coal near Gillette, Wyoming, is as much as 110 feet (34 m) thick. Most of the coals in the Fort Union Formation are ranked subbituminous.[3]

Fort Union Formation - stratigraphy

Fossil content

[edit]
Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Mammals

[edit]

Cimolestans

[edit]
Cimolestans reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Crustulus C. fontanus Northeastern Montana.[4] Tullock Member.[4] An isolated upper molar.[4] A pantodont.

Leptictids

[edit]
Leptictids reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Prodiacodon P. crustulum Garfield & McCone counties, Montana.[5] Tullock Member.[5] Fragmentary dentary & isolated teeth.[5] A leptictid.

Marsupials

[edit]
Marsupials reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Peradectes P. sp. Swain Quarry, Wyoming.[6] Upper & lower molars.[6] Reassigned to Swaindelphys.
Swaindelphys S. cifellii Swain Quarry, Wyoming.[6] Upper & lower molars.[6] An opossum.

Primatomorphs

[edit]
Primatomorphs reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Carpodaptes C. sp. Wind River Basin, Wyoming.[7] Shotgun Member.[7] 2 isolated fourth lower premolars.[7] A carpolestid.
Chiromyoides C. caesor Hell's Half Acre (UCM locality 78009), Mesa County, Colorado.[8] A single upper incisor (UCM 53515).[8] A plesiadapid.
C. gigas Piceance Creek Basin, Colorado.[8] Multiple teeth.[8] A plesiadapid.
C. sp. UCM locality 78060, Colorado.[8] A left molar (UCM 41606).[8] A plesiadapid.
Elphidotarsius E. shotgunensis Wind River Basin, Wyoming.[7] Shotgun Member.[7] Right ramus of mandible & isolated teeth.[7] A carpolestid.
Nannodectes N. gazini Fremont County, Colorado.[8] A right maxilla (USGS 16872).[8] A plesiadapid.
Palaechthon P., near P. alticuspis Wind River Basin, Wyoming.[7] Shotgun Member.[7] 3 upper molars & 4 lower molars.[7] A plesiadapiform.
P. woodi Wind River Basin, Wyoming.[7] Shotgun Member.[7] A lower jaw & 13 isolated teeth.[7] A plesiadapiform.
Palenochtha P. cf. minor Wind River Basin, Wyoming.[7] Shotgun Member.[7] 5 lower teeth.[7] A plesiadapiform.
Paromomys P., near P. depressidens Wind River Basin, Wyoming.[7] Shotgun Member.[7] Approximately 12 upper teeth, 8 isolated lower teeth & a jaw fragment.[7] A paromomyid.
Phenacolemur P. fremontensis Wind River Basin, Wyoming.[7] Shotgun Member.[7] A lower jaw & isolated teeth.[7] A paromomyid.
P. cf. frugivorus Wind River Basin, Wyoming.[7] Shotgun Member.[7] 2 upper molars & 8 isolated lower molars.[7] A paromomyid.
Plesiadapis P. dubius Piceance Creek Basin, Colorado.[8] Jaw elements & teeth.[8] A plesiadapid.
P. fodinatus Piceance Creek Basin, Colorado.[8] Jaw elements & teeth.[8] A plesiadapid.
P. sp. Wind River Basin, Wyoming.[7] Shotgun Member.[7] 5 lower molars, 3 anterior upper molars & a premolar.[7] A plesiadapid.
Plesiolestes P. cf. problematicus Wind River Basin, Wyoming.[7] Shotgun Member.[7] Approximately 45 isolated teeth.[7] A plesiadapiform.
Pronothodectes P. intermedius Wind River Basin, Wyoming.[7] Shotgun Member.[7] Jaw elements & teeth.[7] A plesiadapid.
Purgatorius P. janisae 'Harley's Point' UCMP locality V77087, Garfield County, Montana.[9] Tullock Member.[9] UCMP 150018 (right m1), and UCMP 192398 (left m3).[9] A purgatoriid.
P. mckeeveri Garfield County, Montana.[9] Tullock Member.[9] Dentary remains & teeth.[9] A purgatoriid.
P. cf. P. mckeeveri Harley's Point' UCMP locality V77087, Garfield County, Montana.[9] Tullock Member.[9] UCMP 150019 (right M2), and UCMP 150020 (right M2).[9] A purgatoriid.
Torrejonia Cf. T. wilsoni Wind River Basin, Wyoming.[7] Shotgun Member.[7] About 14 lower teeth & possibly 3 upper molars.[7] A plesiadapiform.
Zanycteris Z. honeyi UMC locality number 92177, Colorado.[10] Atwell Gulch Member.[10] Right maxilla (UCM 87378).[10] A plesiadapiform.

Ungulates

[edit]
Ungulates reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Dissacus D. argenteus Princeton Quarry, Park County, Wyoming.[11] Upper part of the formation.[11] Jaw elements & teeth.[11] A mesonychid.
D. cf. navajovius Princeton Quarry, Park County, Wyoming.[11] Upper part of the formation.[11] Jaw elements & teeth.[11] Specimens reassigned to D. argenteus.
D. praenuntius Park County, Wyoming.[11] Upper part of the formation.[11] Mandible (YPM-PU 16159).[11] A mesonychid also known from the Willwood Formation.
Ectocion E. mediotuber Princeton Quarry, Wyoming.[12] Dentary.[12] A phenacodontid.
Periptychus P. carinidens Makoshika State Park, Montana.[13] A periptychid also found in the Nacimiento, North Horn, Black Peaks & Animas formations.
Sigynorum S. magnadivisus Great Divide Basin, southern Wyoming.[14] China Butte Member.[14] An arctocyonid.

Reptiles

[edit]

Birds

[edit]

A partial ornithurine coracoid bone found in this formation is identical to others found in the older Hell Creek Formation. At present, this unnamed species is the only known individual bird species that have survived the Cretaceous–Paleogene extinction event.[15]

Birds reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Lithornis L. celetius Bangtail Quarry, Sedan Quadrangle, Park County, Montana.[16] A lithornithid.

Crocodilians

[edit]
Crocodilians reported from the Fort Union Formation
Genus Species Location Stratigraphic member Material Notes Images
Allognathosuchus A. sp. Princeton Quarry, Park County, Wyoming.[17] Anterior end of left dentary (PU 16988).[17] A crocodilian.

Squamates

[edit]
Squamates reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Anguidae Genus & species indeterminate Swain Quarry, Carbon County, Wyoming.[18] Fragmentary jaw elements.[18] An anguid lizard.
cf. Anguidae Swain Quarry, Carbon County, Wyoming.[18] 6 partial dentaries.[18] Provisionally referred to anguid lizards based on size & shape.
Contogenys cf. C. sloani Swain Quarry, Carbon County, Wyoming.[18] Posterior part of a right maxilla (AMNH 12069).[18] A skink.
Exostinus E. cf. E. lancensis Swain Quarry, Carbon County, Wyoming.[18] 4 partial dentaries.[18] A xenosaurid lizard.
E. rugosus Princeton & Schaff quarries, Park County, Wyoming.[17] Multiple specimens.[17] A xenosaurid lizard.
Glyptosaurinae Genus & species indeterminate Swain Quarry, Carbon County, Wyoming.[18] Several jaw remains.[18] A glyptosaurine lizard.
Glyptosaurinae or Odaxosaurinae Genus & species indeterminate Swain Quarry, Carbon County, Wyoming.[18] Fragmentary jaw elements & osteoderms.[18] Indeterminate lizard remains.
Machaerosaurus M. torrejonensis Swain Quarry, Carbon County, Wyoming.[18] Numerous jaw elements.[18] An anguid lizard also known from the Nacimiento Formation.
Odaxosaurus O. piger Swain Quarry, Carbon County, Wyoming.[18] Many fragmentary jaw remains.[18] An anguid lizard.
Oligodontosaurus O. wyomingensis Park County, Wyoming.[17] A left mandible (PU 14246).[17] An amphisbaenian.
Palaeosaniwa cf. P. canadensis Swain Quarry, Carbon County, Wyoming.[18] Medial part of left dentary (AMNH 15957).[18] A large anguimorph lizard.
Palaeoxantusia P. fera Swain Quarry, Carbon County, Wyoming.[18] Numerous jaw elements.[18] A night lizard.
Pancelosaurus P. piger Princeton, Fritz & Schaff quarries, Park County, Wyoming.[17] Multiple skull elements.[17] An anguid lizard.
Provaranosaurus P. acutus Princeton Quarry, Park County, Wyoming.[17] PU 14243 (left maxilla), 14561 (anterior portion of left dentary) & 17145 ( fragment of left maxilla).[17] A palaeovaranid lizard.
cf. P. sp. Swain Quarry, Carbon County, Wyoming.[18] 3 partial dentaries (AMNH 14306, 14307 & 14309).[18] A palaeovaranid lizard.
Rhineuridae Unidentified genus & species Fritz Quarry, Park County, Wyoming.[17] An almost complete right dentary & a broken vertebra (PU 18627).[17] An amphisbaenian.
Saniwa cf. S. sp. Swain Quarry, Carbon County, Wyoming.[18] 2 trunk vertebrae (AMNH 15960 & 16003).[18] A varanid.
Swainiguanoides S. milleri Swain Quarry, Carbon County, Wyoming.[18] Jaw elements.[18] An iguanid.

Testudines

[edit]
Testudines reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Atoposemys A. entopteros Montana.[19] Tullock Member.[19] A softshell turtle.
Axestemys A. montinsana PTRM Site V02017, Slope County, North Dakota.[20] Numerous skull, limb & shell fragments.[20] A softshell turtle also found in the Melville & Denver formations.
Cardiochelyon C. rogerwoodi Reis Quarry, Park County, Wyoming.[21] Partial skeleton (YPM PU14671).[21] A kinosternoid formerly thought to be a platysternid.
Cedrobaena C. putorius Cedar Point Quarry, Wyoming.[22] Shell & skull elements.[22] A baenid turtle also found in the Hell Creek Formation.
Hutchemys H. arctochelys Burns Mine, Washoe Area, Carbon County, Montana.[23] Tongue River Member.[23] Multiple shell elements.[23] A softshell turtle.
H. rememdium Fallon County, Montana.[23] Ekalaka Member.[23] A near complete postcranial skeleton (YPM PU 16795) & shell elements.[23] A softshell turtle.
H. sp. Duffy's Ranch, Sweet Grass County, Montana.[23] YPM PU 11566.[23] A softshell turtle.
Ptychogaster P. sp. Princeton Quarry & Reiss Locality, Park County, Wyoming.[17] PU 17794 (fragments of the skull & shell), 14671 & 16443 (shells).[17] A turtle.
Tullochelys T. montanus Montana.[19] Tullock Member.[19] A chelydrid turtle also known from the Hell Creek Formation.

Amphibians

[edit]
Amphibians reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Amphiuma A. jepseni Park County, Wyoming.[17] PU 14666 (partial vertebral column), 14668 (partial skull) & 16788 (dislocated vertebrae).[17] An aquatic salamander.
Anura Incertae sedis Park County, Wyoming.[17] PU 14662 (distal end of right radioulna), 14663 (proximal end of left radioulna), 14669 (phalanx), 13372 (right maxilla).[17] A frog.
Discoglossidae Undescribed genus & species Park County, Wyoming.[17] Distal end of right humerus (PU 14670).[17] A frog similar to undescribed discoglossid remains from the Hell Creek Formation.[17]
Eorhinophrynus E. sp. Princeton & Fritz quarries, Park County, Wyoming.[17] Humeri & vertebrae.[17] A burrowing toad.
Opisthotriton O. kayi Princeton Quarry, Park County, Wyoming.[17] Multiple specimens.[17] A salamander.
Scapherpeton S. tectum Princeton & Schaff quarries, Park County, Wyoming.[17] PU 20583 (3 broken vertebrae, an atlas, an ilium & a rib) & PU 19500 (a humerus).[17] A salamander.

Fish

[edit]
Fish reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Acipenseridae Morphotype A Eagle Mine near Bear Creek, Carbon County, Montana.[24] A complete lateral scute (YPM VPPU 17066).[24] A large sturgeon.
Morphotype B Highway Blowout Site, Fallon County, Montana.[24] Tongue River Member.[24] A complete lateral scute (YPM VPPU 16646).[24] A large sturgeon.
Amia A. basiloides Burns Mine and Eagle Mine near Bear Creek, Carbon County, Montana[25] A near complete skull and partial skeleton, isolated vertebra[25] A large bowfin.
Atractosteus A. grandei Bowman County, North Dakota.[26] Lowest Danian strata.[26] A large gar.
Cyclurus C. fragosus Schaff Quarry, Park County, Wyoming.[17] 3 vertebral centra (PU 21174).[17] A bowfin.
Engdahlichthys E. milviaegis Montana.[27] Tullock Member.[27] A fairly small sturgeon.
Polyodon P. tuberculata Montana.[27] Tullock Member.[27] 3 specimens.[27] A paddlefish.

Invertebrates

[edit]

Bivalves

[edit]
Bivalves reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Pisidium P. sp. indet. Powder River Basin.[28] Tongue River Member.[28] 8 specimens.[28] A sphaeriid.
P.? sp. indet. Powder River Basin.[28] Tongue River Member.[28] 3 specimens.[28] A sphaeriid.
Plesielliptio P. priscus Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A unionid.
cf. P. priscus Powder River Basin.[28] Tongue River Member.[28] Several specimens.[28] A unionid.
P. silberlingi Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A unionid.
cf. P. silberlingi Powder River Basin.[28] Tongue River Member.[28] 6 specimens.[28] A unionid.
P. sp. indet. Powder River Basin.[28] Tongue River Member.[28] 2 specimens.[28] A unionid.
Sphaeriidae Gen. & sp. indet. Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A sphaeriid.
Sphaerium S. sp. indet. Powder River Basin.[28] Tongue River Member.[28] 1 specimen.[28] A sphaeriid.
S.? sp. indet. Powder River Basin.[28] Tongue River Member.[28] Several specimens.[28] A sphaeriid.
Unionidae Gen. & sp. indet. Powder River Basin.[28] Tongue River Member.[28] 11 specimens.[28] A unionid.

Gastropods

[edit]
Gastropods reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Acroloxus A.? minutus Powder River Basin.[28] Tongue River Member.[28] 2 specimens.[28] A river limpet.
A. sp. indet. Powder River Basin.[28] Tongue River Member.[28] 1 specimen.[28] A river limpet.
Clenchiella C. n. sp. A Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A clenchiellid.
C. n. sp. A? Powder River Basin.[28] Tongue River Member.[28] 1 specimen.[28] A clenchiellid.
C. cf. C. n. sp. A Powder River Basin.[28] Tongue River Member.[28] 10 specimens.[28] A clenchiellid.
C. sp. indet. Powder River Basin.[28] Tongue River Member.[28] 30 specimens.[28] A clenchiellid.
Hydrobia H. anthonyi Powder River Basin.[28] Tongue River Member.[28] 2 specimens.[28] A hydrobiid.
H. sp. A Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A hydrobiid.
H. cf. H. sp. A Powder River Basin.[28] Tongue River Member.[28] 2 specimens.[28] A hydrobiid.
H. sp. B? Powder River Basin.[28] Tongue River Member.[28] Multiple specimens.[28] A hydrobiid.
H. sp. C? Powder River Basin.[28] Tongue River Member.[28] 1 specimen.[28] A hydrobiid.
H. sp. indet. Powder River Basin.[28] Tongue River Member.[28] Multiple specimens.[28] A hydrobiid.
H.? sp. indet. Powder River Basin.[28] Tongue River Member.[28] 2 specimens.[28] A hydrobiid.
Lioplacodes L. multistriata Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A viviparid.
L. tenuicarinata Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A viviparid.
L. tenuicarinata? Powder River Basin.[28] Tongue River Member.[28] 11 specimens.[28] A viviparid.
L. limneaformis Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A viviparid.
L. sp. indet. Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A viviparid.
L.? sp. indet. Powder River Basin.[28] Tongue River Member.[28] 1 specimen.[28] A viviparid.
Valvata? V.? sp. indet. Powder River Basin.[28] Tongue River Member.[28] 1 specimen.[28] A valvatid.
Viviparus V. raynoldsanus Powder River Basin.[28] Tongue River Member.[28] Numerous specimens.[28] A viviparid.
V. raynoldsanus? Powder River Basin.[28] Tongue River Member.[28] 1 specimen.[28] A viviparid.
V. cf. V. raynoldsanus Powder River Basin.[28] Tongue River Member.[28] 17 specimens.[28] A viviparid.
V. sp. Powder River Basin.[28] Tongue River Member.[28] Multiple specimens.[28] A viviparid.

Plants

[edit]
Plants reported from the Fort Union Formation
Genus Species Locality Stratigraphic member Material Notes Images
Aesculus A. hickeyi Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Leaves.[29] A horse chestnut.
Amersinia A. obtrullata Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Fruits.[29] A nyssaceaen, may be produced by the same plant as Beringiaphyllum cupanioides.
Beringiaphyllum B. cupanioides Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Leaf (UF 18969-60464).[29] A nyssaceaen, may be produced by the same plant as Amersinia obtrullata.
Browniea B. serrata Mexican Hat locality & Custer National Forest, Powder River County, Montana.[29][30] Lebo Member & Tongue River Member.[29][30] Leaves showing signs of insect damage.[30] A nyssaceaen.
Cercidiphyllum C. genetrix Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaves showing signs of insect damage.[30] A katsura tree.
Cornus C. swingii Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Leaves.[29] A dogwood.
Davidia D. antiqua Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Leaves & fruits.[29] A dove tree.
Cf. Dennstaedtia Cf. D. americana Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] A single specimen of sterile foliage (UF 18969-34532).[29] A fern.
Dicotylophyllum D. hansonium Williston Basin, North Dakota.[31] Tongue River Member.[31] Leaves.[31] A dicot.
D. horsecreekium Williston Basin, North Dakota.[31] Ludlow Member.[31] Leaves.[31] A dicot.
Eostangeria E. pseudopteris Sweetwater County, Wyoming.[32] Upper part of the formation.[32] Multiple specimens.[32] A cycad.
Equisetum E. sp. Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] A single stem (UF 18969-60476A).[29] A horsetail.
"Ficus" "F." artocarpoides Mexican Hat locality.[30] Lebo Member.[30] Leaves with signs of hole feeding and insect mining.[30] A fig-tree.
Glyptostrobus G. europaeus Mexican Hat locality.[30] Lebo Member.[30] Leafy branches.[30] A conifer.
Juglandiphyllites J. glabra Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaves with insect damage and probable lepidopteran leaf mines.[30] A member of the walnut family.
Lauraceae Species 1 Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaf with piercing and sucking marks from insects.[30]
Species 2 Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaves showing signs of insect damage.[30]
Macginistemon M. mikanoides Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Stamen groups.[29] A platanaceaen.
Macginitiea M. gracilis Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] A fragmentary leaf (UF 18969-38380).[29] A platanaceaen.
M. nascens Williston Basin, North Dakota.[31] Ludlow Member.[31] Leaves.[31] A platanaceaen.
Meliosma M. thriviensis Williston Basin, North Dakota.[31] Ludlow Member.[31] Leaves.[31] A sabiaceaen.
M. vandaelium Williston Basin, North Dakota.[31] Tongue River Member.[31] Multiple leaves.[31] A sabiaceaen.
Nordenskioeldia N. borealis Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Fruit.[29] A trochodendrale.
Paleonelumbo P. macroloba Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaves.[30] A nelumbonaceaen.
Paranymphaea P. crassifolia Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaves.[30] A nymphaeaceaen.
Phyllites P. demoresii Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Leaves.[29]
Platanus P. raynoldsii Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaves showing signs of insect damage.[30] A plane-tree.
P. sp. Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Leaves.[29] A plane-tree.
Polyptera P. manningii Mexican Hat locality, Montana.[30] Lebo Member.[30] Fruits.[30] A member of the walnut family.
"Populus" "P". nebrascensis Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaves showing signs of insect damage.[30] A poplar.
Porosia P. verrucosa Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Fruits.[29] A rutaceaen.
Taxodium T. olrikii Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] [29] A cypress tree.
Ternstromites cf. T. aureavallis Mexican Hat locality, Montana.[30] Lebo Member.[30] Leaf with a gall at the intersection of primary and secondary veins.[30] A theaceaen.
T. paucimissouriensis Williston Basin, North Dakota.[31] Ludlow & Tongue River Members.[31] Leaves.[31] A theaceaen.
Trochodendroides T. genetrix Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] A few leaves.[29] A saxifrage.
Ulmites U. microphylla Custer National Forest, Powder River County, Montana.[29] Tongue River Member.[29] Leaves.[29] An ulmaceaen.
Zizyphoides Z. flabella Mexican Hat locality, Montana & Custer National Forest, Powder River County, Montana.[30][29] Lebo Member & Tongue River Member.[30][29] Leaves showing signs of insect damage.[30] A trochodendrale.

See also

[edit]
  • List of fossiliferous stratigraphic units in Colorado
  • List of fossiliferous stratigraphic units in Montana
  • List of fossiliferous stratigraphic units in North Dakota
  • List of fossiliferous stratigraphic units in Wyoming
  • Uranium mining in Wyoming
  • Guaduas Formation, contemporaneous coal-bearing formation of northern South America

References

[edit]
  1. ^ a b Wyodak Coal, Tongue River Member of the Fort Union Formation, Powder River Basin, Wyoming: "No-Coal Zones" and Their Effects on Coalbed Methane Production, by Mark Ashley, 2005
  2. ^ Eocene and Paleocene rocks of the southern and central basins, by Robert E. McDonald, in Geologic Atlas of the Rocky Mountain Region, Rocky Mountain Association of Geologists, Denver, CO, 1972: p. 248
  3. ^ Cretaceous and Tertiary coals of the Rocky Mountains and Great Plains regions, by R.M. Flores and T.A. Cross, 1991, in Economic Geology, U.S., Geological Society of America, Decade of North American Geology Series, vol. P-2, p. 547-571.
  4. ^ a b c Clemens, William A. (2018-02-17). "A pantodont (Mammalia) from the latest Puercan North American Land Mammal Age (earliest Paleocene) of the Western Interior, USA". Historical Biology. 30 (1–2): 183–188. Bibcode:2018HBio...30..183C. doi:10.1080/08912963.2016.1276178. ISSN 0891-2963. S2CID 132830375.
  5. ^ a b c Clemens, W. (January 9, 2015). "(Leptictidae, Mammalia) from the Tullock Member of the Fort Union Formation, Garfield and McCone Counties, Montana, USA". PaleoBios. 32 (1): 1–17. doi:10.5070/P9321025382. S2CID 55974838.
  6. ^ a b c d Johanson, Zerina (November 1996). "New marsupial from the Fort Union Formation, Swain Quarry, Wyoming". Journal of Paleontology. 70 (6): 1023–1031. Bibcode:1996JPal...70.1023J. doi:10.1017/S0022336000038725. ISSN 0022-3360. S2CID 133554548.
  7. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac ad ae af ag ah ai aj Gazin, C. Lewis (1971). "Paleocene primates from the shotgun member of the Fort Union Formation in the Wind River Basin, Wyoming". Proceedings of the Biological Society of Washington. 84: 13–37. ISSN 0006-324X.
  8. ^ a b c d e f g h i j k l Burger, Benjamin J.; Honey, James G. (2008-09-12). "Plesiadapidae (Mammalia, Primates) from the late Paleocene Fort Union Formation of the Piceance Creek Basin, Colorado". Journal of Vertebrate Paleontology. 28 (3): 816–825. doi:10.1671/0272-4634(2008)28[816:pmpftl]2.0.co;2. ISSN 0272-4634. S2CID 128913932.
  9. ^ a b c d e f g h i Wilson Mantilla, Gregory P.; Chester, Stephen G. B.; Clemens, William A.; Moore, Jason R.; Sprain, Courtney J.; Hovatter, Brody T.; Mitchell, William S.; Mans, Wade W.; Mundil, Roland; Renne, Paul R. (2021). "Earliest Palaeocene purgatoriids and the initial radiation of stem primates". Royal Society Open Science. 8 (2) 210050. Bibcode:2021RSOS....810050W. doi:10.1098/rsos.210050. ISSN 2054-5703. PMC 8074693. PMID 33972886.
  10. ^ a b c Burger, Benjamin John (2013-10-29). "A new species of the archaic primate Zanycteris from the late Paleocene of western Colorado and the phylogenetic position of the family Picrodontidae". PeerJ. 1 e191. doi:10.7717/peerj.191. ISSN 2167-8359. PMC 3817582. PMID 24255808.
  11. ^ a b c d e f g h i O'Leary, Maureen A.; Rose, Kenneth D. (1995-05-12). "New mesonychian dentitions from the Paleocene and Eocene of the Bighorn Basin, Wyoming". Annals of the Carnegie Museum. 64 (2): 147–172. Bibcode:1995AnCM...64..147O. doi:10.5962/p.215127. ISSN 0097-4463. S2CID 89955337.
  12. ^ a b Thewissen, J. G. M. (1990). "Evolution of Paleocene and Eocene Phenacodontidae (Mammalia, Condylarthra)". hdl:2027.42/48629. {{cite journal}}: Cite journal requires |journal= (help)
  13. ^ Shelley, Sarah L.; Williamson, Thomas E.; Brusatte, Stephen L. (2018-07-18). "The osteology of Periptychus carinidens: A robust, ungulate-like placental mammal (Mammalia: Periptychidae) from the Paleocene of North America". PLOS ONE. 13 (7) e0200132. Bibcode:2018PLoSO..1300132S. doi:10.1371/journal.pone.0200132. ISSN 1932-6203. PMC 6051615. PMID 30020948.
  14. ^ a b McComas, Katie M.; Eberle, Jaelyn J. (May 2015). "A new earliest Paleocene (Puercan) arctocyonid mammal from the Fort Union Formation, Great Divide Basin, Wyoming, and its phylogenetic position among early 'condylarths'". Journal of Systematic Palaeontology. 14 (6): 445–459. doi:10.1080/14772019.2015.1066886. S2CID 127411164.
  15. ^ Longrich, N.R., Tokaryk, T. and Field, D.J. (2011). "Mass extinction of birds at the Cretaceous–Paleogene (K–Pg) boundary." Proceedings of the National Academy of Sciences, 108(37): 15253-15257. doi:10.1073/pnas.1110395108
  16. ^ Houde, Peter W. (1988). "Paleognathous Birds from the Early Tertiary of the Northern Hemisphere". The Auk. 107 (2): 455–456. doi:10.2307/4087644. ISSN 0004-8038. JSTOR 4087644.
  17. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac Estes, Richard (1975). "Lower Vertebrates from the Fort Union Formation, Late Paleocene, Big Horn Basin, Wyoming". Herpetologica. 31 (4): 365–385. ISSN 0018-0831. JSTOR 3891523.
  18. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z Sullivan, Robert M. (January 1982). "Fossil lizards from Swain Quarry "Fort Union Formation," middle Paleocene (Torrejonian), Carbon County, Wyoming". Journal of Paleontology. 56 (4): 996–1010.
  19. ^ a b c d Hutchison, J. Howard (2013), Brinkman, Donald B.; Holroyd, Patricia A.; Gardner, James D. (eds.), "New Turtles from the Paleogene of North America", Morphology and Evolution of Turtles, Vertebrate Paleobiology and Paleoanthropology, Dordrecht: Springer Netherlands, pp. 477–497, doi:10.1007/978-94-007-4309-0_26, ISBN 978-94-007-4309-0{{citation}}: CS1 maint: work parameter with ISBN (link)
  20. ^ a b Vitek, Natasha S. (2012-03-11). "Giant fossil soft-shelled turtles of North America". Palaeontologia Electronica. 15 (16): 1–43. doi:10.26879/299. ISSN 1094-8074.
  21. ^ a b Joyce, Walter G.; Claude, Julien (2020-01-15). "An alternative interpretation of the Paleogene turtle Cardichelyon rogerwoodi as a hinged kinosternoid". Journal of Paleontology. 94 (3): 557–567. Bibcode:2020JPal...94..557J. doi:10.1017/jpa.2019.92. ISSN 0022-3360. S2CID 210976208.
  22. ^ a b Lyson, Tyler R.; Joyce, Walter G. (November 2009). "A revision of Plesiobaena (Testudines: Baenidae) and an assessment of baenid ecology across the K/T boundary". Journal of Paleontology. 83 (6): 833–853. doi:10.1666/09-035.1. ISSN 0022-3360. S2CID 85964417.
  23. ^ a b c d e f g h Joyce, Walter G.; Revan, Ariel; Lyson, Tyler R.; Danilov, Igor G. (2009). "Two New Plastomenine Softshell Turtles from the Paleocene of Montana and Wyoming". Bulletin of the Peabody Museum of Natural History. 50 (2): 307. Bibcode:2009BPMNH..50..307J. doi:10.3374/014.050.0202. ISSN 0079-032X. S2CID 85505337.
  24. ^ a b c d e Brownstein, Chase Doran (November 2022). "Evidence of large sturgeons in the Paleocene of North America". Journal of Paleontology. 97: 218–222. doi:10.1017/jpa.2022.87. ISSN 0022-3360. S2CID 253653018.
  25. ^ a b Brownstein, Chase D.; Near, Thomas J. (2024). "A giant bowfin from a Paleocene hothouse ecosystem in North America". Zoological Journal of the Linnean Society. 202 (4). doi:10.1093/zoolinnean/zlae042. Retrieved 2024-04-30.
  26. ^ a b Brownstein, Chase Doran; Lyson, Tyler R. (2022). "Giant gar from directly above the Cretaceous–Palaeogene boundary suggests healthy freshwater ecosystems existed within thousands of years of the asteroid impact". Biology Letters. 18 (6) 20220118. doi:10.1098/rsbl.2022.0118. PMC 9198771. PMID 35702983.
  27. ^ a b c d e Murray, Alison M.; Brinkman, Donald B.; DeMar, David G.; Wilson, Gregory P. (2020-03-03). "Paddlefish and sturgeon (Chondrostei: Acipenseriformes: Polyodontidae and Acipenseridae) from lower Paleocene deposits of Montana, U.S.A.". Journal of Vertebrate Paleontology. 40 (2) e1775091. Bibcode:2020JVPal..40E5091M. doi:10.1080/02724634.2020.1775091. ISSN 0272-4634. S2CID 222213273.
  28. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac ad ae af ag ah ai aj ak al am an ao ap aq ar as at au av aw ax ay az ba bb bc bd be bf bg bh bi bj bk bl bm bn bo bp bq br bs bt bu bv bw bx by bz ca cb cc cd ce cf cg ch ci cj ck cl cm cn co cp cq cr cs ct cu cv cw cx cy cz da Hanley, John H.; Flores, Romeo M. (1987). "Taphonomy and Paleoecology of Nonmarine Mollusca: Indicators of Alluvial Plain Lacustrine Sedimentation, Upper Part of the Tongue River Member, Fort Union Formation (Paleocene), Northern Powder River Basin, Wyoming and Montana". PALAIOS. 2 (5): 479–496. Bibcode:1987Palai...2..479H. doi:10.2307/3514619. ISSN 0883-1351. JSTOR 3514619.
  29. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac ad ae af ag ah ai aj ak al am an ao ap aq ar as at au av aw ax ay az Manchester, Steven R.; Foster, Alyssa; Lott, Terry A. (2023-05-12). "The Paleocene Horse Creek florule, Tongue River Member of the Fort Union Formation, southeastern Montana, USA". Acta Palaeobotanica. 63 (1): 32–53. doi:10.35535/acpa-2023-0003. ISSN 0001-6594.
  30. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac ad ae af ag ah ai aj ak al am an ao ap Donovan, Michael P.; Wilf, Peter; Labandeira, Conrad C.; Johnson, Kirk R.; Peppe, Daniel J. (2014-07-24). "Novel Insect Leaf-Mining after the End-Cretaceous Extinction and the Demise of Cretaceous Leaf Miners, Great Plains, USA". PLOS ONE. 9 (7) e103542. Bibcode:2014PLoSO...9j3542D. doi:10.1371/journal.pone.0103542. ISSN 1932-6203. PMC 4110055. PMID 25058404.
  31. ^ a b c d e f g h i j k l m n o p q r Peppe, Daniel J.; Hickey, Leo J. (November 2014). "Fort Union Formation Fossil Leaves (Paleocene, Williston Basin, North Dakota, USA) Indicate Evolutionary Relationships Between Paleocene and Eocene Plant Species". Bulletin of the Peabody Museum of Natural History. 55 (2): 171–189. Bibcode:2014BPMNH..55..171P. doi:10.3374/014.055.0209. ISSN 0079-032X. S2CID 129724520.
  32. ^ a b c Kvaček, Zlatko; Manchester, Steven R. (1999). "Eostangeria Barthel (Extinct Cycadales) from the Paleogene of Western North America and Europe". International Journal of Plant Sciences. 160 (3): 621–629. Bibcode:1999IJPlS.160..621K. doi:10.1086/314152. ISSN 1058-5893. S2CID 83978433.
  • v
  • t
  • e
Chronostratigraphy of Colorado
  • v
  • t
  • e
Cenozoic chronostratigraphy of Colorado
Ph
Cz
Q
Pleistocene
  • Alamosa Formation
N
Pliocene
Zanclean
  • Dry Union Formation
  • Ogallala Formation
Miocene
Messinian
  • Dry Union Formation
  • Ogallala Formation
Aquitanian
  • Arikaree Formation
  • Browns Park Formation
  • Cedar Mountain Formation
  • Flat Tops Volcanics
  • Los Pintos Formation
  • Martins Canyon Formation
  • North Park Formation
  • Santa Fe Formation
  • Troublesome Formation
  • Trump Formation
  • Wagon Tongue Formation
  • Grouse Mountain Basalt
  • Pe
    Oligocene
    Chattian
  • Arikaree Formation
    • Brule Formation
    • Central Colorado Volcanics
    • Chadron Formation
    • Conejos Formation
    • Pinnacle Formation
    • Pitch Formation
    Eocene
  • Blanco Basin Formation
  • Cuchara Formation
  • D2 Sequence
  • Dawson Arkose
  • Echo Park Formation
  • Farisita Formation
  • Huerfano Formation
  • Green River Formation
  • Poison Canyon Formation
  • Uinta Formation
  • Wasatch Formation
  • Paleocene
    • Animas Formation
    • Arapahoe Conglomerate
    • Bridger Formation
    • Denver Formation
    • Fort Union Formation
    • Middle Park Formation
    • Nacimiento Formation
    • Ojo Alamo Formation
    • Raton Conglomerate
    • San Jose Formation
    • South Park Formation
    • Washakie Formation
    • Gravel Mountain Formation
    • Independence Mountain Formation
    • v
    • t
    • e
    Mesozoic chronostratigraphy of Colorado
    Ph
    Mz
    K
    Upper
  • Benton Formation
  • Carlile Shale
  • Castle Gate Formation
  • Cliff House Sandstone
  • Codell Sandstone
  • Dakota Group
  • Fort Hays Limestone
  • Fox Hills Formation
  • Fruitland Formation
  • Graneros Shale
  • Greenhorn Shale
  • Hygiene Formation
  • Juana Lopez
  • Kirtland Formation
  • Kremmling Formation
  • Lance Formation
  • Laramie Formation
  • Lewis Formation
  • Lion Canyon Formation
  • Mancos Shale
  • Menefee Formation
  • Mowry Shale
  • Niobrara Formation
  • Pando Porphyry
  • Pictured Cliffs Formation
  • Pierre Shale
  • Point Lookout Formation
  • Smoky Hill Chalk
  • Trinidad Formation
  • Vermejo Formation
  • Williams Fork Formation
  • Lower
    • Burro Canyon Formation
    • Horsetooth Formation
    J
    Upper
    • Curtis Formation
    • Morrison Formation
    • Ralston Creek Formation
    • Wanakah Formation
    Middle
    • Carmel Formation
    • Entrada Formation
    • Garo Formation
    • Page Formation
    • Sundance Formation
    Lower
    • Glen Canyon Formation
    • Kayenta Formation
    • Navajo Formation
    • Wingate Sandstone
    Tr
    Upper
    • Chinle Formation
    Middle
    Anisian
    • Chugwater Formation
    • Jelm Formation
    • Moenkopi Formation
    Lower
    Olenekian
  • Chugwater Formation
  • Induan
    • Chugwater Formation
    • Lykins Formation
    • Taloga Formation
    • Moenkopi Formation
    • v
    • t
    • e
    Paleozoic chronostratigraphy of Colorado
    Ph
    Pz
    P
    Lopingian
    Changhsingian
  • Chugwater Formation
  • Lykins Formation
  • Taloga Formation
  • Cisuralian
    Asselian
    • Fountain Formation
    • Madera Formation
    • Blaine Formation
    • Cedar Hills Formation
    • Chase Formation
    • Council Grove Formation
    • Crestone Conglomerate
    • Day Creek Formation
    • Falcon Formation
    • Forelle Formation
    • Glendo Formation
    • Glorieta Formation
    • Hermosa Formation
    • Ingleside Formation
    • Kaibab Limestone
    • Lansing Formation
    • Lyons Formation
    • Maroon Formation
    • Minnekahta Formation
    • Opeche Formation
    • Owl Canyon Formation
    • Phosphoria Formation
    • Sangre de Cristo Formation
    • Satanka Formation
    • Shawnee Formation
    • South Canyon Creek Formation
    • Stone Corral Formation
    • Sumner Formation
    • Wabaunsee Formation
    • Weber Formation
    • Wellington Formation
    • White Horse Group
    • Wolfcamp Formation
    • Yeso Formation
    C
    ⁋
    Gzhelian
  • Fountain Formation
  • Madera Formation
    • Atoka Formation
    • Belden Formation
    • Cherokee Formation
    • Eagle Valley Evaporite
    • Glen Eyrie Formation
    • Gothic Formation
    • Hermosa Formation
    • Jacque Mountain Formation
    • Kansas City Formation
    • Kerber Formation
    • Keyes Formation
    • Marmaton Formation
    • Maroon Formation
    • Minturn Formation
    • Molas Formation
    • Morgan Round Valley Formation
    • Morrow Formation
    • Sharpsdale Formation
    M
    Tournaisian
  • Williams Canyon Formation
    • Beulah Formation
    • Gilman Formation
    • Headscrabble Formation
    • Leadville Formation
    • Molas Formation
    • Osage Formation
    • Spergen Formation
    • St. Louis Formation
    • Ste. Genevieve Formation
    • Warsaw Formation
    D
    Upper
    Famennian
    • Williams Canyon Formation
    • Aneth Formation
    • Dyer Formation
    • Elbert Formation
    • Kinderhook Formation
    • Misener Formation
    • Ouray Formation
    • Parting Formation
    • Pinyon Park Formation
    O
    Upper
  • Fremont Limestone
  • Viola Formation
  • Middle
    • Harding Sandstone
    • Simpson Formation
    Lower
    Tremadocian
    • Dotsero Formation
    • Arbuckle Formation
    • Manitou Formation
    Є
    Furongian
    Stage 10
  • Dotsero Formation
  • Paibian
    • Lodore Formation
    • Sawatch Formation
    Series 3
    Guzhangian
    • Lodore Formation
    • Sawatch Formation
    • Reagan Formation
    • Tintic Formation
    • v
    • t
    • e
    Precambrian chronostratigraphy of Colorado
    pЄ
    ♇
    Z
    Tonian
  • Uinta Mountain Group
    • Tava Formation
    X
    Siderian
  • Owiyukuts Complex
    • Uncompahgre Formation
    Retrieved from "https://en.wikipedia.org/w/index.php?title=Fort_Union_Formation&oldid=1332457036"
    Categories:
    • Geologic formations of Montana
    • Geologic formations of North Dakota
    • Geologic formations of Wyoming
    • Cretaceous Montana
    • Cretaceous geology of North Dakota
    • Cretaceous geology of Wyoming
    • Paleogene Montana
    • Paleogene geology of North Dakota
    • Paleogene geology of Wyoming
    • Maastrichtian Stage of North America
    • Danian Stage
    • Cretaceous–Paleogene boundary
    • Clarkforkian
    • Lancian
    • Puercan
    • Tiffanian
    • Torrejonian
    • Paleontology in Wyoming
    • Fluvial deposits
    • Lacustrine deposits
    • Sandstone formations of the United States
    • Shale formations of the United States
    • Coal formations
    • Coal in the United States
    Hidden categories:
    • Pages using gadget WikiMiniAtlas
    • CS1 errors: missing periodical
    • CS1 maint: work parameter with ISBN
    • Articles with short description
    • Short description is different from Wikidata
    • Coordinates on Wikidata

    • indonesia
    • Polski
    • العربية
    • Deutsch
    • English
    • Español
    • Français
    • Italiano
    • مصرى
    • Nederlands
    • 日本語
    • Português
    • Sinugboanong Binisaya
    • Svenska
    • Українська
    • Tiếng Việt
    • Winaray
    • 中文
    • Русский
    Sunting pranala
    url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url url
    Pusat Layanan

    UNIVERSITAS TEKNOKRAT INDONESIA | ASEAN's Best Private University
    Jl. ZA. Pagar Alam No.9 -11, Labuhan Ratu, Kec. Kedaton, Kota Bandar Lampung, Lampung 35132
    Phone: (0721) 702022
    Email: pmb@teknokrat.ac.id