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Late Miocene of Lompoc, USA) Morus magnus (Late Miocene of California) Morus peruvianus (Pisco Late Miocene of Peru) Morus vagabundus (Temblor Late Miocene

Recent) Uria (Late Miocene – Recent) Aethia (Late Miocene – Recent) Alca (Late Miocene/Early Pliocene – Recent) Synthliboramphus (Late Miocene/Early Pliocene –

Ouranopithecus macedoniensis, a late Miocene (9.6–8.7 mya) hominoid from Greece and Ouranopithecus turkae, also from the late Miocene (8.7–7.4 mya) of Turkey

to Late Miocene of Asia, Late Miocene of Africa and Europe) †Hyaenotherium (Late Miocene to Early Pliocene of Eurasia) †Miohyaenotherium(Late Miocene of

Anserobranta (Late Miocene of C Europe) – includes "Anas" robusta, validity doubtful Presbychen (Temblor Late Miocene of Sharktooth Hill, US) Afrocygnus (Late Miocene

Asia, Late Miocene to Early Pliocene Genus †Sivaonyx – Asia and Africa, Late Miocene to Early Pliocene Genus †Teruelictis – Spain, Late Miocene Genus

species of the extinct elephantid genus Mammuthus. They lived from the late Miocene epoch (from around 6.2 million years ago) into the Holocene about 4,000

relationships are often undetermined: †Anas sp. (Late Miocene of China) †Anas sp. (mid-sized species from the Late Miocene of Rudabánya, Hungary) †Anas amotape (Campbell

extinct baiji of China and the fossil genus Parapontoporia from the Late Miocene and Pliocene of the Pacific coast of North America. The genus Prolipotes

genus of hegetotheriid notoungulate that lived from the Middle to the Late Miocene of what is now Argentina. It was a medium-sized animal and had long legs

Xotodon is an extinct genus of toxodontid mammal that lived during the Late Miocene (Huayquerian in the SALMA classification) in Argentina, South America

Huayqueriense) age is a period of geologic time (9.0–6.8 Ma) within the Late Miocene epoch of the Neogene, used more specifically within the SALMA classification

Notoungulates, belonging to the suborder Typotheria. It lived from the Late Miocene to the Late Pliocene, and its fossilized remains were discovered in South

belonging to the suborder Typotheria. It lived from the Middle to the Late Miocene, and its fossilized remains were discovered in South America. This animal

arayanensis - Late Miocene †Hystrix depereti - Pliocene †Hystrix paukensis - Late Miocene-Pliocene †Hystrix primigenia - Late Miocene-Pliocene †Hystrix

Sinoadapis is a genus of adapiform primate that lived in Asia during the late Miocene. Gebo 2002, pp. 33–34. Gebo, D.L. (2002). "Adapiformes: Phylogeny and

Promacrauchenia is an extinct genus of macraucheniids that lived during the Late Miocene to Late Pliocene epochs of what is now Argentina and Bolivia. It belongs

subfamily Toxodontinae whose remains were discovered in the Middle to Late Miocene (Mayoan to Montehermosan) Mauri Formation in the La Paz Department in

Gyrinodon is an extinct genus of toxodontid notoungulate that lived from the Late Miocene and Early Pliocene in what is now Brazil and Colombia. This animal was

 'Indian ape') is an extinct species of large ape that lived in the late Miocene of the Siwalik Hills in northern India. Although frequently assigned

Samburupithecus is an extinct primate that lived in Kenya during the middle to late Miocene. The one species in this genus, Samburupithecus kiptalami, is known only

†Eutamias ertemtensis Qiu, 1991 – late Miocene to Pliocene of China †Eutamias lishanensis Qiu et al., 2008 – late Miocene of China †Eutamias orlovi Sulimski

Acrecebus is a prehistoric cebid monkey from the Late Miocene Solimões Formation of Acre State, Brazil and Bolivia. The only species known is A. fraileyi

genus of gibbons that lived 8.2 to 7.1 million years ago during the late Miocene. As of 2022, it is the oldest gibbon known. The fossils, mainly of teeth

subfamily of adapiform primate that lived in Asia during the middle to late Miocene. Gebo 2002, p. 32. Gebo, D.L. (2002). "Adapiformes: Phylogeny and adaptation"

that lived off the coasts of Mexico and Peru, South America during the Late Miocene to Late Pliocene. Two species have currently been described: the type

Simocyon, which was about the size of a mountain lion, lived in the late Miocene and early Pliocene epochs, and has been found in Europe, Asia, and rarely

genus of gibbons that lived 8.2 to 7.1 million years ago during the late Miocene. As of 2022, it is the oldest gibbon known. The fossils, mainly of teeth

Stenasodelphis is an extinct genus of pontoporiid dolphin from the mid-late Miocene epoch. Its name roughly translates to "the narrow-nosed dolphin." The

estimated to have lived 8 to 10 million years ago (TGHLCA) during the late Miocene. The fossil find of Nakalipithecus nakayamai are closest in age to the

Phalacrocorax ibericus (Late Miocene of Valles de Fuentiduena, Spain) – Microcarbo, Phalacrocorax or Gulosus? Phalacrocorax lautus (Late Miocene of Golboçica, Moldavia)

an extinct hypocarnivorous canid mammal similar to Vulpes endemic to Late Miocene North America. Its sister taxon is the extant Urocyon; together, the

Feliformia. Fossils have been dated from the Middle Eocene through the Late Miocene epochs (Bartonian through Tortonian stages, 40.4–7.2 million years ago)

Pleistocene) †Ochotona guizhongensis (Tibet, late Miocene) †Ochotona lagreli (China: Inner Mongolia, late Miocene to late Pliocene) †Ochotona magna (China

crocodile") is an extinct monospecific genus of medium-sized caiman from the Late Miocene of western Brazil and Venezuela. The genus contains a single species

discovered in what are believed to be marine deposits, dating from the late Miocene, whereas the Amazon river dolphin is an exclusively freshwater species

litoptern mammal of the family Proterotheriidae that lived during the Late Miocene of Argentina and Chile. Fossils of this genus have been found in the

a large bodied notoungulate which inhabited South America during the Late Miocene to Early Pliocene (Mayoan to Montehermosan in the SALMA classification)

herbivorous mammal, native to South America, which lived in the Middle to Late Miocene period, typically during the Laventan stage. It is a member of the family

Brachydelphis is a genus of pontoporiid known from the Late Miocene Pisco Formation of Peru and the Bahía Inglesa Formation of Chile. Two species are recognized

monospecific genus of gavialoid crocodilian that lived during the Middle to Late Miocene in what is now Argentina. Fossils have been found in the formation then

Pristifelis is an extinct genus of feline from the late Miocene. It contains a single species, Pristifelis attica. The first fossil skull of P. attica

Beneziphius is an extinct genus of ziphiid cetacean known from late Miocene to Pliocene marine deposits in Belgium and fishing grounds off Spain. The genus

related genus Diceros. The placement of Ceratotherium neumayri from the Late Miocene of Europe and Western Asia within the genus has been questioned, with

Bambolinetta lignitifila is a fossil species of waterfowl from the Late Miocene of Italy, now classified as the sole member of the genus Bambolinetta.

an extinct genus of megalonychid ground sloth that lived during the Late Miocene in what is now Argentina. Fossils have been found in the Ituzaingó Formation

marine gavialid crocodilians remained widespread as recently as the Late Miocene. Some marine reptiles, such as ichthyosaurs, plesiosaurs, metriorhynchid

of dolphin that lived off the Pacific coast of North America from the Late Miocene until the genus' extinction during the Pliocene. It is related to the

paraphyletic/polyphyletic family Kentriodontidae. Remains have been found in the late Miocene (Serravallian) Choptank Formation of United States. Macrokentriodon is

mostly in the Nevada part of the Tertiary Colorado Plateau until the late Miocene Sequoiadendron fossil pollen and macrofossils may have been found as

"Brandtocetus, a new genus of baleen whales (Cetacea, Cetotheriidae) from the late Miocene of Crimea, Ukraine". Journal of Vertebrate Paleontology. 34 (2): 419–433

so it is proposed that genus is of African origin. By the middle to late Miocene (5–13 mya) they had spread to and become widespread across Eurasia. While

hoofed ungulates which inhabited South America during the Middle to Late Miocene, from 17.5 to 6.8 Ma and existed for approximately 10.7 million years

litoptern belonging to the family Proterotheriidae, that lived between the late Miocene and the early Pliocene (in the SALMAs Huayquerian and Montehermosan)

xenarthran, belonging to the order Cingulata. It lived from the Middle to the Late Miocene, and its fossilized remains are found in South America. This animal was

being the most basal clade of the Arvicolinae, diverging during the late Miocene, about 8 million years ago. Database, Mammal Diversity (2021-11-06),

an extinct genus of hominid that lived in southeast Europe during the late Miocene around 7.2 million years ago. Originally identified by a single lower

genus of medium-sized river dolphin cetaceans that lived during the Late Miocene epoch in what is now the coasts of Panama, about 6.1 million to 5.8 million

an extinct genus of hominid that lived in southeast Europe during the late Miocene around 7.2 million years ago. Originally identified by a single lower

Archaebalaenoptera is a genus of extinct rorqual known from late Miocene to Pliocene-age marine deposits of the Netherlands, northern Italy, and Peru.

Vulpes riffautae is an extinct species of fox from the late Miocene of Chad (approximately 7 ma). Fossils of V. riffautae potentially represent the earliest

both Africa (Kenya, Tunisia), Anatolia and Europe, dating to the Early-Late Miocene, with its earliest appearance in Europe being approximately 18-17 million

modern gray whale, about 16 metres (52 ft) long. It lived during the late Miocene. The Paleobiology Database Parabalaenoptera entry Deméré, T.A.; Berta

Solimoea acrensis is a prehistoric ateline monkey from the Late Miocene Solimões Formation of Brazil. It is the only known species of the genus Solimoea

dusignathine walrus found along the coast of what is now California, during the late Miocene. It was a huge-sized pinniped with skull length of around 47 cm (19 in)

gomphothere" native to Afro-Eurasia, that lived from the Tortonian stage of the late Miocene until its extinction during the Early Pleistocene, roughly from 8.5–2

species Imagotaria downsi. Fossils of Imagotaria are known from the early late Miocene of California (c. 10-12 million years ago). The 1.8 metres (6 ft) long

Tranatocetus is an extinct genus of mysticete from the late Miocene (Tortonian) of Jutland, Denmark. The type and only species is Tranatocetus argillarius

Hemimastodon ("half mastodont") is an extinct genus of proboscidean from the Late Miocene deposits of the Dera Bugti Beds in Pakistan. Its phylogenetic affinity

Plesiobalaenoptera is a genus of extinct rorqual which existed in Italy during the late Miocene epoch. The type species is P. quarantellii. It is the oldest known rorqual

Pontophoca is an extinct genus of earless seals from the middle-late Miocene of the eastern Paratethys basin and the North Sea. There are two recognized

mysticete in the subfamily Herpetocetinae. Remains have been found in Late Miocene marine deposits in Belgium. Herentalia is distinguished from other cetotheriids

Other species assigned to the genus include Diceros praecox from the Late Miocene (from about 7 million years ago) and the Pliocene of Sub-Saharan Africa

maxilla, was discovered in the nearby Sena Madureia locality of the late Miocene Solimões Formation, in and referred to the species in 1997. G. jessei

is an extinct gomphothere genus (of order Proboscidea) known from the Late Miocene to Early Pleistocene of Asia, including China, Japan, Thailand, Myanmar

Rangwapithecus is an extinct genus of ape from the Early Miocene of Kenya. Late Miocene phalanges from Hungary have also been assigned to this genus, but were

now Central Valley, California, United States, which lived during the late Miocene. It was an amphibious carnivore. The holotype specimen (USNM 13627) was

subfamily of canids native to North America. It lived from the Middle to the Late Miocene, 13.6 to 5.3 Ma Mya, existing for approximately 16.5 million years. The

Malta consists of a sequence of sedimentary rocks of late Oligocene to late Miocene age cut through by a set of extensional faults of Pliocene age. The Maltese

subfamily of canids native to North America. It lived from the Middle to Late Miocene, 16.3 – 5.3 mya, existing for approximately 11 million years. It was

Callophoca is an extinct genus of earless seals from the late Miocene to early Pliocene of Belgium and the US Eastern Seaboard. The type and only species

whale belonging to the family Tranatocetidae. It is known only from the late Miocene (Tortonian) of Los Angeles County, California. Mixocetus is a large-size

gomphotheres and mammutids. The oldest fossils of the genus are found in Late Miocene strata in Asia, likely originating from the more archaic Stegolophodon

Eosclerocalyptus is an extinct genus of glyptodont. It lived during the Late Miocene, and its fossilized remains were discovered in South America. This animal

river dolphin-like cetaceans of uncertain family placement from the Late Miocene epoch (Serravallian) of present-day Peru. The type species is Brujadelphis

Coscinocercus is an extinct genus of Glyptodont. It lived during the Late Miocene, and its fossilized remains were discovered in South America. This animal

changed very little, apart from growing much larger in size; by the late Miocene, they had become the largest land animals of their time. Their most distinctive

is a period of geologic time from 11.8 to 10 Ma, within the Middle to Late Miocene epoch of the Neogene, used more specifically within the SALMA classification

Miocaperea is an extinct genus of pygmy right whale from the Late Miocene Pisco Formation of Peru. Its type species is Miocaperea pulchra. The discovery

as belonging to the genus, extending back to the Pliocene or possibly late Miocene. Species of Elephas have distinct bossing of the parieto-occipital region

the mastodons (genus Mammut), which inhabited North America from the Late Miocene until their extinction at beginning of the Holocene, around 11,000 years

genus of ground sloth of the family Mylodontidae, living during the Late Miocene (Huayquerian). Fossil remains of Octomylodon have been found uniquely

is the only known species of the genus. Chamitataxus lived during the Late Miocene, around 6 million years ago in what is now North America. Out of the

species, D. carnifex, lived in Pakistan and India during the middle to late Miocene. Dissopsalis is the last known hyaenodont genus. It lived alongside its

genus of ground sloth of the family Mylodontidae, living during the Late Miocene (Huayquerian). Fossil remains of Octomylodon have been found uniquely

is the only known species of the genus. Chamitataxus lived during the Late Miocene, around 6 million years ago in what is now North America. Out of the

genus of hyena that lived across Europe and Asia during the Middle and Late Miocene, it is often considered to be the first hyena since it contains some

†Anser atavus (Middle/Late Miocene of Bavaria, Germany) – sometimes in Cygnus †Anser arenosus Bickart 1990 (Big Sandy Late Miocene of Wickieup, USA) †Anser

sloth which existed in Peru in the western Amazon Basin, during the late Miocene (Huayquerian age). It is known from the holotype LACM 4609/117533, which

xenarthran, related to the modern armadillos. It lived from the Early to the Late Miocene, and its fossilized remains were discovered in South America. This animal

Hyaenodonta. Fossil remains of these mammals are known from middle Eocene to late Miocene deposits in North America, Europe, Africa and Asia. Members of this group

Early to Middle Miocene Santa Cruz and Chichinales Formations and the Late Miocene (Montehermosan) Andalhuala Formation of Argentina. Three species are

of extinct saber-toothed cats that lived in North America during the Late Miocene, between 10.3 and 5.332 Ma. Despite its scientific name, Nimravides does

Palaeohoplophorus) is an extinct genus of glyptodont. It lived from the Middle to the Late Miocene, and its fossilized remains were discovered in South America. This animal

Phlyctaenopyga is an extinct genus of glyptodont. It lived from the Late Miocene to the Early Pliocene, and its fossilized remains were discovered in South

Protoglyptodon is an extinct genus of glyptodont. It lived during the Late Miocene, and its fossilized remains were found in South America. This animal

belonging to the family Diprotodontidae which inhabited Australia from the Late Miocene to Late Pleistocene. It was a large animal, weighing 500 kg (1100 lbs)

Urotherium is an extinct genus of Glyptodont. It lived from the Late Miocene to the Late Pliocene, and its fossilized remains were found in South America

Pseudaptenodytes have been found in deposits in Victoria (Australia) which are of Late Miocene or Early Pliocene age. Simpson, George Gaylord (1970): Miocene penguins

been found from Venezuela and Brazil that date back to the Middle to Late Miocene. Although Hesperogavialis is one of the best known gavialoids from South

cingulate belonging to the family Pampatheriidae. It lived from the Late Miocene to the Early Pliocene, and its fossilized remains were discovered in

Cetotheriinae. The type and only species is Brandtocetus chongulek from the late Miocene (Tortonian) of the Kerch Peninsula in Crimea. Brandtocetus chongulek

arose during the early Paleocene in Europe and persisted well into the late Miocene. Hyaenodonts are characterized by long, often disproportionately large

Stromaphorus is an extinct genus of Glyptodont. It lived during the Late Miocene, and its fossilized remains were discovered in South America. This animal

sub-Saharan Africa, but fossils classified in the genus have been found from Late Miocene deposits in Arabia and Europe. Mice in the genus Dendromus are small

belonging to the family Dasypodidae. It lived from the Early to the Late Miocene in South America. Stenotatus was a small to medium-sized armadillo, not

"Paranavis" (Middle/Late Miocene of Paraná, Argentina) – a nomen nudum Macranhinga Noriega, 1992 (Middle/Late Miocene – Late Miocene/Early Pliocene of SC

Plohophorus is an extinct genus of glyptodont. it lived from the Late Miocene to the Late Pliocene, and its fossilized remains were discovered in South

Plaisiodon is an extinct genus of Zygomaturinae from the late Miocene Alcoota Fossil Beds in the Northern Territory, Australia. Because of its robust skull

North America that includes species that lived during the Middle to Late Miocene. "Gnathabelodon" buckneri Sellards, 1940 has been renamed Blancotherium

extinct genus of even-toed ungulates that existed during the middle and late Miocene in Asia (India, Pakistan, Thailand, Myanmar). The last two pairs of premolars

carnivorous placental mammals that lived from the early Paleocene to the late Miocene epochs in North America, Europe, Asia and Africa. Originally thought

is an extinct genus of enormous flightless anatid waterfowl from the Late Miocene of Gargano, Italy. The genus contains one species, G. ballmanni, named

Cetotheriinae. The type and only species is Zygiocetus nartorum, known from the Late Miocene (Messinian) of Adygea in the Russian Caucasus. Zygiocetus nartorum is

(meaning "dog-coati" in Greek) is an extinct genus of procyonid from the Late Miocene to Middle Pleistocene of South America. Fossils of Cyonasua have been

genus of prehistoric xenarthrans that lived in Argentina, during the Late Miocene. This genus is regarded as closely related to the later, and more famous

2 (Late Miocene of Love Bone Bed, USA) Grus cf. antigone (Late Miocene/Early Pliocene of Lee Creek Mine, USA) Grus nannodes (Late Miocene/Early Pliocene

Eliomys quercinus The earliest records of the genus are known from the Late Miocene (Tortonian) of the Iberian Peninsula. Fossil species assigned to Eliomys

genus of prehistoric xenarthrans that lived in Argentina, during the Late Miocene. This genus is regarded as closely related to the later, and more famous

(meaning "dog-coati" in Greek) is an extinct genus of procyonid from the Late Miocene to Middle Pleistocene of South America. Fossils of Cyonasua have been

group than to the macroraptorial sperm whales known from middle and late Miocene. Miophyster may have had an adaptation to deep diving and / or developed

an extinct genus of nothrotheriid ground sloths that lived during the Late Miocene and Early Pliocene of Bolivia. Fossils of Aymaratherium have been found

Pliocene. By the late Miocene, around 10 Mya, the bovids rapidly diversified, leading to the creation of 70 new genera. This late Miocene radiation was partly

hyaenodonts. Fossil remains of these mammals are known from Middle Eocene to Late Miocene deposits in Africa, the Arabian Peninsula, and Asia. The genus Teratodon

of a modern donkey. Fossil evidence suggests that it lived during the Late Miocene (Clarendonian to Hemphillian), from about 13.6 Ma to 5.3 Ma. Analysis

Piscobalaena is an extinct genus of cetaceans, which lived from the Middle to Late Miocene epochs (about 11.6 to 5.3 million years ago) in Peru and Florida. Its

longirostris, sometimes called the swan-necked seal, is an extinct genus of Late Miocene pinniped. It was thought to have been the ancestor of the modern leopard

hyaenodonts. Fossil remains of these mammals are known from early to late Miocene deposits in Asia and Africa. Tribe: †Dissopsalini (Morales & Pickford

Stegodon, and transitional fossils between the two genera known from the Late Miocene of Southeast Asia and Yunnan in South China. Like modern elephants, Stegolophodon

subfamily Monachinae. It is known from fossils found in the middle to late Miocene of Belgium. The type and only species of Monotherium is M. delognii,

belonging to the subfamily Phocinae. It is known from fossils found in the late Miocene of Belgium. There are two species of Frisiphoca, F. aberratum and F.

early Miocene (23 mya). They had largely disappeared worldwide by the late Miocene (5 mya), with the latest recorded species at the end of the Miocene in

Large hypocarnivores (Ursus) were rare and developed in the mid-to-late Miocene-Pliocene as Borophaginae became extinct. Examination of dentition shows

Afrocygnus is an extinct genus of swan, which lived during the Late Miocene, and perhaps up to the Late Pliocene, in what is today North Africa. The only

late Miocene of Nebraska, United States. It had comparatively enormous, wing-like cheekbones. Prothero, D.R., and A. Pollen, 2013. New late Miocene peccaries

species (including the Eocene †G. clarkensis and †G. eaglesomei, Oligocene-late Miocene †G. aduncus, Miocene †G. mayumbensis, and Pliocene †G. capellinii) much

11 Ma, the Middle Miocene Warm Interval gave way to the much cooler Late Miocene. The ice caps on both poles began to grow and thicken, a process enhanced

found in Brazil and Colombia, in rocks dating back from the middle to late Miocene. The type specimen of Caninemys, a well preserved skull (DNPM-MCT 1496-R)

the emergence of C4 grasses about 6 to 8 million years ago during the Late Miocene and Pliocene. The genus Circus was introduced by the French naturalist

almost complete maxilla of Proscelidodon from the Maimará Formation (late Miocene), Jujuy province, provides new data on the plesiomorphic condition of

in the Pawnee Creek Beds of Colorado. It lived during the Middle to Late Miocene 16.0—10.3 mya, existing for approximately 5.7 million years. Fossils

Pakistan joint research project (Y-GSP) in the well-dated middle and late Miocene deposits of the Pothohar Plateau in northern Pakistan. In life, the average

Elasmotherium is an extinct genus of large rhinoceros endemic to Eurasia during Late Miocene through to the Late Pleistocene, with the youngest reliable dates around

primarily calcium phosphate. The mining uncovered fossils dating from the late Miocene and early Pliocene, approximately 5 million years ago. Fossil species

oldest known Olduwan stone artifacts, have been found at the site—all of late Miocene, the Pliocene, and the very early Pleistocene times, that is, about 5

Allodesmus is an extinct genus of pinniped from the middle to late Miocene of California and Japan that belongs to the extinct pinniped family Desmatophocidae

members of the genus at the initial branching of Citrus radiation in the Late Miocene. It is genetically similar to another wild citrus of the region, the

Paracamelus migrating over the Bering Land Bridge into Eurasia during the Late Miocene, around 6 million years ago, becoming ancestral to Camelus. The last

Pediolophodon is an extinct gomphotheriid proboscidean genus from the middle to late Miocene of North America (Nebraska and Texas). Pediolophodon was a close relative

divided into six major groups; basal sparassodonts (?earliest Paleocene-late Miocene), species that cannot be easily assigned to any of the other sparassodont

mammal related to the elephant (order Proboscidea). It lived during the late Miocene Epoch in Asia and North America. Shoshani (1996) placed Torynobelodon

content. The Ware Formation dates to the Neogene and Quaternary periods; Late Miocene to Early Pleistocene epochs, typically Pliocene (3.5 to 2.8 Ma), Uquian

Clifton Banks – Middle to late Miocene Forsyth's Banks and Fossil rock stack – Early Pliocene Spring Creek – Late Miocene to Early Pliocene Kawarren

American plains it inhabited. Fossils of Pliohippus have been found at many late Miocene localities in Colorado, the Great Plains (Nebraska, including Ashfall

"A New Species of Tsuga (Pinaceae) based on Lignified Wood from the Late Miocene of Central Yunnan, China, and Its Paleoenvironmental Implications". Acta

(2014). "A new genus of Megalonychidae (Mammalia, Xenarthra) from the Late Miocene of Argentina". Revista Brasileira de Paleontologia. 17 (1): 33–42. doi:10

mammal related to the elephant (order Proboscidea). It lived during the late Miocene Epoch in Asia and North America. Shoshani (1996) placed Torynobelodon

"New material of Chalicotheriidae (Perissodactyla, Mammalia) from the Late Miocene of Axios Valley, Macedonia (Greece) with the description of a new species"

native to the North Pacific from the early Oligocene (Rupelian) to the late Miocene (Tortonian) (30.8 to 7.25 million years ago). Desmostylians are the only

of the Miocene. The species Konobelodon cyrenaicus is known from the Late Miocene of North Africa, representing the latest surviving amebelodont on the

(2017). "Taxonomy and Ecology of the Fossil Freshwater Molluscs from Late Miocene Palaeolake Obweruka in the Albertine Basin (Uganda)". Münchner Geowissenschaftliche

volcanic in origin and probably broke through the ocean's surface in the late Miocene, 8 to 10 million years ago. The substrate of the island is either directly

Hapalops is an extinct genus of ground sloth from the Early to Late Miocene of Brazil (Solimões Formation), Bolivia (Honda Group), Colombia (Honda Group)

found at Riversleigh in Australia, material dating from the Middle to Late Miocene Epoch. The type species of the genus is Ganguroo bilamina, published

came from a locality near Csákvár, Hungary, and was dated back to the Late Miocene. Kretzoi, Miklós (1938). "Die Raubtiere von Gombaszög nebst einer Ubersicht

inhabited North America, Eurasia, and Africa from the middle Eocene to the late Miocene. Amphicyoninae was named by Trouessart (1885). It was assigned to Canidae

Mesohippus in North America during the middle Eocene and thrived until the late Miocene. The subfamily continued in Eurasia with the genus Sinohippus until the

of horse that lived in Africa and the Indian subcontinent during the late Miocene. This genus has a convoluted taxonomic history. After being described

Stegolophodon, known from the Miocene of Asia and the later Stegodon, from the Late Miocene to Late Pleistocene of Africa and Asia (with a single occurrence in Greece)

South America. The fossil species Leporinus scalabrinii, known from the late Miocene of Entre Ríos in Argentina, has only recently been added to this genus

?Oryzomys pliocaenicus is a fossil rodent from the Hemphillian (late Miocene) of Kansas, central United States. It is known from a single mandible (lower

Loma de Las Tapias Formation of Argentina in rocks dating back to the Late Miocene epoch. The presence of glyptodonts in the Arroyo Chasicó Formation was

sanctialbani (Middle - Late Miocene of Central Europe) - formerly in Strix; includes T. campiterrae Tyto robusta (Late Miocene/Early Pliocene of the Gargano

leading to the giant forest hog and the warthogs much earlier, in the late Miocene, between 11.9 and 5.6 million years ago. The same studies suggest that

†Hesperotestudo gilbertii (Hay, 1899) Ogallala Formation, Kansas, Hemphillian, Late Miocene-Early Pliocene (Tortonian–Zanclean) †Hesperotestudo orthopygia (Cope

tentative. The genus Hadrictis Pia, 1939, described from a skull found in late Miocene deposits in Austria, is a synonym of Eomellivora. Valenciano, Alberto;

found in Late Paleocene, Late Oligocene, Early Miocene and possibly Late Miocene deposits (~56-20 or possibly 11.6 million years ago) in France, Germany

of machairodontine (sabre-toothed) cat that lived in China during the Late Miocene. The type and only species, Longchuansmilus xingyongi, was described

is an extinct genus of barbourofelid that lived in Europe during the Late Miocene epoch (16.9—7.246 mya), existing for approximately 9.654 million years

managing to escape and heal. Tseng, Z. J. (2008). "Cranial function in a late Miocene Dinocrocuta gigantea (Mammalia: Carnivora) revealed by comparative finite

is estimated to have diverged from Aselliscus stoliczkanus during the late Miocene. Tu, V.; Görföl, T.; Csorba, G. (2023). "Aselliscus dongbacanus". IUCN

The Huayquerías Formation (Spanish: Formación Huayquerías) is a Late Miocene fossiliferous geological formation of the Frontal Cordillera and Cuyo Basin

new species of Peltephilidae (Mammalia: Xenarthra: Cingulata) from the late Miocene (Chasicoan SALMA) of Argentina. Zootaxa 3359. 55–64. Accessed 2019-02-15

Middle Miocene, before spreading across the world in waves from the Late Miocene to Pleistocene. The genus Porphyrio was introduced by the French zoologist

would have been the largest fragments of that collision which caused a "late Miocene dust shower". The family consists of more than a thousand known members

1931) - from late Miocene † Bulinus pavlovici (Atanacković, 1959) - from late Miocene † Bulinus stevanovici (Atanacković, 1959) - late Miocene † Bulinus

Cetotherium maicopicum Spasski, 1951, based on a specimen from the late Miocene of the Russian Caucasus, was reassigned to the genus Kurdalagonus from

sister group to the tribe Ellobiusini, from which it diverged during the late Miocene; however, this still remains uncertain. Kryštufek, B. (2018). "Dinaromys

Pliocene †Bohra Australia, Pliocene-Late Pleistocene †Kurrabi Australia, Late Miocene †Baringa Australia, Early Pleistocene Different common names are used

mustelids known from Africa, Pakistan and India that lived from the late Miocene to the early Pleistocene. It contains 9 confirmed species, 2 debated

Pliocene Asia Gazella deperdita - Late Miocene Europe Gazella dorcadoides - Middle Miocene Asia Gazella pilgrimi - Late Miocene Europe Gazella gaudryi - Middle

into an ice age and global drying possibly colder and drier than the late Miocene (Messinian) through early Pliocene (Zanclean) cold period. Originally

Tiucetus is an extinct genus of cetotheriid baleen whale known from the Late Miocene Pisco Formation of Peru. Tiucetus is distinct from other cetotheriids

Samos dragon, is an extinct species of monitor lizard from the middle to late Miocene of Greece and Spain, known from several specimens. A specimen consisting

Odontaspididae. These extinct sharks lived from the Early Paleocene to Late Miocene (61.7 to 10.3 Ma). The Latin genus name Striatolamia refers to the striations

found in early to mid-Miocene strata, while P. germaini is found in Late Miocene strata. P. primaevus is distinguished from P. germaini by the lack of

the Mediterranean Sea, the first of several such periods during the late Miocene. After the strait closed for the last time around 5.6 Ma, the region's

Pleistocene C. australis Hendey, 1974 - Africa, Late Miocene C. bonisi Koufos, 1987 - Greece, Late Miocene C. borissiaki Khomenko, 1932 - Russia, Pliocene

(Middle/Late Miocene of Grive-Saint-Alban, France) ?Aquila pennatoides (Middle/Late Miocene of Grive-Saint-Alban, France) Aquila sp. (Late Miocene – Late

Tetralophodon. The earliest members of the family, are known from the Late Miocene, around 9–10 million years ago. The modern genera of elephants and mammoths

from Miocene-age fossils in China and Turkey and persisted until the Late Miocene (early Vallesian). Fossils of this machairodont have been found in the

Andalhualá Formations in central and northwestern Argentina dating to the Late Miocene (Huayquerian), where a good sample of fossils has been obtained. The

the Great Plains and Gulf Coast regions of North America during the late Miocene, roughly 9 million years ago, and apparently became extinct on this continent

†Buteo contortus (snake Creek Late Miocene of Sioux County, US) – formerly in Geranoaetus †Buteo spassovi (Late Miocene of Chadžidimovo, Bulgaria) †Buteo

M. (2005). "Evidence of a fossil stork (Aves: Ciconiidae) from the Late Miocene of the Pisco Formation, Peru". Bol.Soc.Geol.Peru. 100 (2): 63–66. Aguada

extinct genus of amphicyonids that inhabited North America during the Late Miocene. It lived ~13.6—10.3 Ma ago, existing for approximately 4 million years

of Early to Middle Miocene age. Later occurrences are apparently from Late Miocene or possibly even Early Pliocene deposits. Together with the related genus

family Dromomerycidae, endemic to North America. It lived during the Late Miocene 10.3—4.9 Ma, existing for approximately 5 million years. Fossils have

the Great Plains and Gulf Coast regions of North America during the late Miocene, roughly 9 million years ago, and apparently became extinct on this continent

mammalian fauna of the European forests were replaced by the faunas of the Late Miocene, adapted to a dry climate and to an open terrain. The beginning of the

(2013). "A new species of Dasypodidae (Xenarthra: Cingulata) from the late Miocene of northwestern South America: implications in the Dasypodini phylogeny

Castor C. californicus An extinct beaver species Western North America Late Miocene to Early Pleistocene Castoroides Giant beavers North America Up to 100 kg

new species S. bravardi in the fauna of Entre Rios which dates to the Late Miocene. Later, in 1885, the same author described an additional species, S.

of Puerto Rico and Aktiogavialis caribesi from the Huayquerian of the Late Miocene of Venezuela. As a typical gavialoid, Aktiogavialis followed the standard

observations, and has experienced significant left-slip movement since the late Miocene. Its minimum and maximum dip-slip displacement rates are estimated at

were established only in 2004. Their basal position consists of the late Miocene representatives of northern South America. In principle, a revision for

lived on the Pacific coast of today's California and Mexico from the late Miocene epoch to the early Pleistocene (ranging from at least 7.4 million to

the largest ruminants of all time. Sivatherium originated during the Late Miocene (around 7 million years ago) in Africa and survived through to the late

genus of camelid endemic to North America. It lived from the Early to Late Miocene 20.4—5.3 mya, existing for approximately 15 million years. Fossil distribution

Pierce (2017). A study on the ontogenetic changes in the teeth of the late Miocene hipparionines based on fossils from Fugu (Shaanxi, China) is published

extinct genus of camelid, endemic to North America. They lived during the Late Miocene 10.3—5.3 mya existing for approximately 5 million years. Alforjas is

in the genus Eubalaena. The fossil record of Balaena, dating to the late Miocene, encompasses ten species known from finds in Europe, North America, and

S2CID 227249176. Haile-Selassie, Yohannes (2009). Ardipithecus Kadabba: Late Miocene Evidence from the Middle Awash, Ethiopia. University of California Press

Hamada nephelinite lava flow in southwest Japan which occurred in the late Miocene age. Nephelinite is also associated with the highly alkalic volcanism

25249/0375-7536.1990230233. Scheyer, T.M., and M. Delfino. 2016. The late Miocene caimanine fauna (Crocodylia: Alligatoroidea) of the Urumaco Formation

Tyarrpecinus rothi is an extinct thylacinid marsupial that lived during the late Miocene and has been found at the Alcoota scientific reserve in the Northern

to the Koroqara Limestone (Tokalau Limestone Group) and is probably Late Miocene in age. It is mostly fragmental in nature but true reef occurs along

robustiter, sp. nov. (Macropodoidea, Marsupialia), a middle to early late Miocene basal macropodid from Riversleigh World Heritage Area, Australia". Journal

the Late Miocene-Early Pleistocene, a massive basaltic volcanic activity occurred. After the emission of alkali basalts during the Late Miocene, major

pollen that the Trochetiopsis lineage has been on Saint Helena since the late Miocene (some 9.5 million years). The species of this genus were formerly included

stratovolcanoes. Previous studies (Davydov et al.; Vitukhin et al.) suggested a late Miocene to Pliocene age for the Lower Complex, and accordingly older rocks were

the genus Uropsilus, diverging from the rest of the genus during the late Miocene. Johnston, C.; Smith, A.T. (2016). "Uropsilus investigator". IUCN Red

Oioceros is an extinct genus of spiral-horned antelope from the late Miocene. Its fossils have been found in Greece, China, Iran, and Africa. It was first

- Early Cretaceous, Early Cenozoic Thin-skin California Coast Ranges Late Miocene - Quaternary Transpressional Chihuahua Belt Paleocene Unknown Chugach

biostratrigraphic analysis Encinas et al. (2008b) suggested a Tortonian to Zanclean (Late Miocene–Early Pliocene) age for Navidad Formation. They further suggested that

snake mackerels. Fossils of euzaphlegids are found from Paleocene to Late Miocene-aged marine strata of Europe, the Caucasus Mountains, India, Iran, Turkmenistan

of the continent and the expansion of Eucalyptus forests towards the late Miocene may have delayed the evolution of cranial features unique to the modern

Pacific coast of North America and Japan. They first appeared in the late Miocene in California, then died out some time during the Early Pliocene. They

Harper Perennial. pp. 92. ISBN 0-06-055804-0. Haile-Selassie, Y. (2001). "Late Miocene hominids from the Middle Awash, Ethiopia". Nature. 42 (6843): 179–181

Takeuchi; Richard W. Huddleston (2008). "Genyonemus whistleri new species, a late Miocene sciaenid fish from California". In Xiaoming Wang; Lawrence G. Barnes

snake mackerels. Fossils of euzaphlegids are found from Paleocene to Late Miocene-aged marine strata of Europe, the Caucasus Mountains, India, Iran, Turkmenistan

making it the largest known hyena. Pachycrocuta first appeared during the late Miocene (Messinian, 7.2 to 5.3 million years ago). By 800,000 years ago, it became

The Latah Formation is a series of late Miocene lacustrine sedimentary deposits which outcrop in eastern Washington and northwestern Idaho. The lake beds

the middle Miocene Miomachairodus from Africa and Turkey. Until the late Miocene, machairodontines co-existed at several places together with barbourofelids

belonging to the tribe Hipparionini that lived in North America during the late Miocene to Pliocene (Hemphillian to Blancan in the NALMA classification). They

species disappeared from the fossil record of Central Europe during the late Miocene with the last known specimen being recovered from a site in the modern

During late Miocene-Pliocene time (~10 to ~4 million years) the area was attended by volcanism (Late Miocene Tolay Volcanics and Late Miocene - Pliocene

(Early Miocene) Thylacinus megiriani (Late Miocene) Thylacinus potens (Late Miocene) Thylacinus yorkellus (Late Miocene-Pliocene) Genus Tyarrpecinus Murray

(Middle/Late Miocene of Turkey) †Pelophylax meriani (Early Miocene of Germany) †Pelophylax pueyoi (Late Miocene of Spain) †Pelophylax quellenbergi (Late Miocene

inhabited the so-called sub-Paratethyan or Greek-Iranian province during the late Miocene when this region was invaded by advanced rhinos from Africa, such as

"Brandtocetus, a new genus of baleen whales (Cetacea, Cetotheriidae) from the late Miocene of Crimea, Ukraine". Journal of Vertebrate Paleontology. 34 (2): 419–433

Eurasian and African plates occurred during the middle Oligocene to the late Miocene, followed by northwest–southeast convergence from the late Tortonian

the hairy Atlantic spiny rat, around 8.5 million years ago, during the Late Miocene. This is a comparatively small spiny rat, with an average head and body

and is the smallest known horned mammal. Ceratogaulus lived from the late Miocene to the early Pliocene epochs. The horned gopher had two horns; these

Scaphokogia, and Praekogia. The earliest kogiids are known from the late Miocene, around 7 million years ago. The close relationship between extant Physeteridae

macgregori Bombus melaleucus Bombus morrisoni †Bombus pristinus - Middle- Late Miocene, Kumi Formation, Euboea, Greece †Bombus randeckensis Bombus robustus

to a living pika. A specimen with preserved soft-tissue is known from late Miocene aged deposits from Andance in France, which shows that its overall proportions

100 mm per year. It is a relatively young structure, forming during the late Miocene to Pliocene. This age is consistent with the estimated age of the sedimentary

a genus of ground sloth that had arrived in North America during the Late Miocene around 9 million years ago, prior to the main phase of the Great American

(Xenarthra, Tardigrada, Nothrotheriidae) from the Late Miocene (Huayquerian) of Peru: NEW LATE MIOCENE NOTHROTHERIID SLOTH FROM PERU". Palaeontology. 54

an extinct genus of large ungulate native to South America from the Late Miocene to early Holocene epochs (Mayoan to Lujanian in the SALMA classification)

conglomerates. The Marichuela Formation dates to the Neogene period; Late Miocene to Early Pliocene epochs, and has a maximum thickness of 40 metres (130 ft)

into a decline. They went extinct in Eurasia by the beginning of the Late Miocene, with the African species B. lewisi surviving until the end of the epoch

Enhydritherium, a bunodont otter endemic to North America during the late Miocene and early Pliocene epochs. Enhydra reevei, the oldest known species,

the great hornbill is not found there. In the Neogene (at least in the late Miocene), hornbills inhabited North Africa and South Europe. Their remains have

Alsdorf, North Rhine-Westphalia (Miocene) †Tsuga nanfengensis - Yunnan (Late Miocene) †Tsuga swedaea - Buchanan Lake Formation, Axel Heiberg Island (Lutetian)

Pseudomelatomidae. This genus was long considered as extinct since the late Miocene, until Sedeliopsis riosi was discovered off Brazil, obviously a relict-pocket

and W. Landini. 2006. The southernmost sirenian record in the eastern Pacific Ocean, from the Late Miocene of Chile. Systematic Palaeontology 5:945-952

Mylagaulidae. Mylagaulus lived in the Americas during the middle to late Miocene. The genus contains the following species: M. cambridgensis M. cornusaulax

the great hornbill is not found there. In the Neogene (at least in the late Miocene), hornbills inhabited North Africa and South Europe. Their remains have

Apatosagittarius is an extinct monotypic genus of Accipitridae from the Late Miocene of Nebraska. Only one species has been described, Apatosagittarius terrenus

Pseudomelatomidae. This genus was long considered as extinct since the late Miocene, until Sedeliopsis riosi was discovered off Brazil, obviously a relict-pocket

the TM 266 locality to 7 or 6 million years ago (near the end of the Late Miocene) based on the animal assemblage, which made Sahelanthropus the earliest

remains also near Antwerp from the Diest Formation date to the Tortonian (late Miocene). Synonyms of Scaldicetus include Palaeodelphis, Homocetus, and Eucetus

Masanaru Takai. "New species of Agriotherium (Mammalia, Carnivora) from the late Miocene to early Pliocene of central Myanmar." Journal of Asian Earth Sciences

†Anaxyrus hibbardi (Taylor, 1937) (Late Miocene of Kansas) †Anaxyrus pliocompactilis (Wilson, 1968) (Late Miocene of Kansas, possibly synonymous with

Orientornis Temporal range: late Miocene PreꞒ Ꞓ O S D C P T J K Pg N Late Miocene Pelvis Scientific classification Domain: Eukaryota Kingdom: Animalia

Ailurarctos ("cat bear") is an extinct genus of panda from the Late Miocene of China, some 8 million years ago. Different teeth structures in the Ailuropoda

geologic formation in California. It preserves fossils dating from the Late Miocene to Late Pliocene. Earth sciences portal California portal Paleontology

being the closest living relatives of one another and diverging the mid-late Miocene, about 11.59 million years ago. It is thought that the uplift of the

giant caviomorph rodent Phoberomys burmeisteri (Ameghino, 1886) from the late Miocene of northeastern Argentina, and the phylogeny and diversity of Neoepiblemidae"

region of Ethiopia. A study on the phylogenetic relationships for Middle-Late Miocene fossil apes is published by Pugh (2022). Rossie & Cote (2022) describe

Ilingoceros is an extinct genus of pronghorn artiodactyl from the Late Miocene of North America. At 1.8 metres (5.9 ft) in body length, the animal would

species of Lycopsis (Borhyaenidae: Marsupialia) from the La Venta fauna (Late Miocene) of Colombia, South America. Journal of Paleontology, 633–642. Lycopsis

narcisoi, a New Genus of Pliopithecidae (Primates, Catarrhini) From the Late Miocene of Spain". American Journal of Physical Anthropology. 114 (4): 312–324

assigned to the genus Ekaltadeta, placing its occurrence in the middle or late Miocene epoch. The description of a new species and genus was published in 2016

Ophiodon ozymandias is an extinct species of lingcod from the Late Miocene of Southern California. Jordan, D. (1921). "The fish fauna of the California

ringoldensis - Late Miocene to Early Pleistocene, Ringold Formation, Washington Hypolagus tedfordi- Late Pliocene Hypolagus vetus - Late Miocene Hypolagus

canids endemic to North America from the early Miocene epoch through the late Miocene epoch 23.3—5.3 Ma. Borophagus pugnator existed for approximately 18 million

may be exposed near the modern volcanic front, in Central Mexico. A Late Miocene ~11 Ma eastward traveling pulse of mafic volcanism swept across the whole

known extinct cyclopedid species is Palaeomyrmidon incomtus, from the Late Miocene (c. 7 to 9 million years ago) of modern-day Argentina. Silky anteaters

2017-08-15. Benson, Richard D. 2015. A new species of penguin from the late Miocene of Chile, with comments on the stratigraphic range of Palaeospheniscus

known from the Late Miocene Alcoota fossil site about 200km (125 miles) from Alice Springs, corresponding with the middle Late Miocene strata of the Waite

Caviodon is an extinct genus of Late Miocene to Late Pliocene (Chapadmalalan to Montehermosan in the SALMA classification) rodents, related to the modern

66-11.42 Ma the site dates to the transition between the Middle and Late Miocene epoch, providing an important window into the faunal changes taking place

extinct barn owl from what is now Gargano, Italy, dating back to the late Miocene. From its remains, T. gigantea is suggested to have been as large as

2307/2420435. ISSN 0003-0031. JSTOR 2420435. Hulbert, Richard C. (1993). "Late Miocene Nannippus (Mammalia: Perissodactyla) from Florida, with a Description

genus of superficially moose-like or antelope-like giraffids from the late Miocene epoch of Shanxi Province, China. They are closely related to the genus

megalonychid sloths (Mammalia: Xenarthra) from the Urumaco Formation (late Miocene), and their phylogenetic affinities". Journal of Systematic Palaeontology

macaque from the Late Miocene of Wadi Natrun, Egypt. Yohannes Haile-Selassie; Giday WoldeGabriel (2009). Ardipithecus Kadabba: Late Miocene Evidence from

megalonychid sloths (Mammalia: Xenarthra) from the Urumaco Formation (late Miocene), and their phylogenetic affinities". Journal of Systematic Palaeontology

which was thought to have been extinct for 11 million years, since the late Miocene. It would thereby represent a Lazarus species. The animals resemble large

Republic, Hungary and Poland. It preserves fossils dated to the Middle to Late Miocene period. The type locality is the Leitha Mountains in Austria. The limestone

traversing open, brushy country. Isotopic evidence suggests that, in the late Miocene, Teleoceras had limited intake on newly-emergent C4 grasses, but Aphelops

Blieux (2010). "Rodents and Lagomorphs (Mammalia) from the Hemphillian (Late Miocene) of Utah". Journal of Vertebrate Paleontology. 30 (1): 226–235. doi:10

Elephantidae emerged in Africa, having originated from gomphotheres. The Late Miocene saw major climatic changes, which resulted in the decline and extinction

Miocene of Sihong, China) Apatosagittarius (Late Miocene of Nebraska, US) Gansugyps (Liushu Late Miocene of China) Palaeoborus (Miocene) Qiluornis (Miocene

known species of the genus Osbornoceros. Osbornoceros lived during the Late Miocene around 7 to 6 million years ago in what is now North America. It is well

which was named based on a snout fragment from Turkey and dated to the late Miocene, concluded that Felis pamiri and Pseudaelurus lorteti were likely closely

Cervavitus is a genus of prehistoric deer that lived from the late Miocene (Vallesian age) to the Early Pleistocene (Villafranchian age) in parts of Western

those of pedogenic carbonate increased by 5% over the course of the Late Miocene and Pliocene, indicating increased aridification. Further aridification

tetrapod footprints which show hominin-like characteristics from the late Miocene on the western Crete, close to the village of Trachilos, west of Kissamos

the baleen microstructures found in association with the skeleton of a late Miocene balaenopteroid whale recovered from the Pisco Formation (Peru) is published

Blieux (2010). "Rodents and Lagomorphs (Mammalia) from the Hemphillian (Late Miocene) of Utah". Journal of Vertebrate Paleontology. 30 (1): 226–235. doi:10

Inglesa Formation, Late Miocene/Early Pliocene of Bahía Inglesa, Chile) Pygoscelis calderensis (Bahía Inglesa Formation, Late Miocene of Bahía Inglesa,

The King Island Pluton is a mid-to-late Miocene intrusion of syenite and alkali granite on the Central Coast of British Columbia, Canada. It is over 20 km

Billy-Créchy, France) Genus Palaeoaramides (Late Oligocene/Early Miocene – Late Miocene of France) Genus Rhenanorallus (Late Oligocene/Early Miocene of Mainz

saber-toothed cats. Its fossils were discovered in Cerro de los Batallones, a Late Miocene fossil site near Madrid, Spain. However, it was only known from skull

traversing open, brushy country. Isotopic evidence suggests that, in the late Miocene, Teleoceras had limited intake on newly-emergent C4 grasses, but Aphelops

Harrison, Terry (April 2017). "A highly derived pliopithecoid from the Late Miocene of Haritalyangar, India". Journal of Human Evolution. 105: 1–12. doi:10

remains of Loxodonta species have been found in Africa, spanning from the Late Miocene (from around 7-6 million years ago) onwards. The first scientific description

species of long-necked turtle (Pleurodira: Chelidae: Chelodina) from the late Miocene Alcoota Local Fauna, Northern Territory, Australia". PeerJ. 1: e170.

Honanotherium is a genus of extinct giraffid from the late Miocene of Henan Province, China, and East Azerbaijan Province, northwestern Iran. It was closely

Joeckel, R. M.; Otto, Rick E. (2018-11-08). "First U-Pb zircon ages for late Miocene Ashfall Konservat-Lagerstätte and Grove Lake ashes from eastern Great

sometimes referred to as the West Cariboo. The Cariboo Plateau is made of Late Miocene flood basalt lavas of the Chilcotin Group, a group of related volcanic

the Amazon river dolphin in marine deposits: a new Iniidae from the late Miocene of Angola". PeerJ. 6: e5556. doi:10.7717/peerj.5556. PMC 6139015. PMID 30225172

were established only in 2004. Their basic population is formed by the late Miocene representatives of northern South America. In principle, a revision is

amebelodontine Konobelodon Lambert, 1990 (Proboscidea, Mammalia) from the Late Miocene of China. Geodiversitas 38 (1): 65-97. http:// dx.doi.org/10.5252/g2016n1a4

[citation needed] The Asian hipparionin "Hipparion" weihoense from early Late Miocene deposits in northern China has also been referred to the genus. H. primigenium

scarabellii (Late Miocene of Senigallia, Italy) Tringa sp. 1 (Late Miocene/Early Pliocene of Lee Creek Mine, USA) Tringa sp. 2 (Late Miocene/Early Pliocene

is an extinct genus of chalicothere that lived in Europe during the late Miocene. It stood at about 150 cm and weighed around 600 kg. It is thought that

around the western edge of Afar. Bio chronologically, these are from the late Miocene. They haven't found any skeletons of hominids. The heaviest and most

Marandat; J.-J. Jaeger (2004). "A new orang-utan relative from the Late Miocene of Thailand". Nature. 427 (6973): 439–441. Bibcode:2004Natur.427..439C

Kürten (1999). "Allohyaena (Mammalia: Carnivora): giant hyaenid from the Late Miocene of Hungary". Zoological Journal of the Linnean Society. 126 (3): 319–334

east of the Andes, they later became extinct in this region after the Late Miocene, likely due to increasingly cold and arid conditions. A particularly

Asoriculus, Asoriculus gibberodon, was widespread in Europe from the Late Miocene (Messinian, MN13, from around 7.2-5.3 million years ago) to the Early

They are classified in the late Tertiary, occurring in the middle to late Miocene and early Pliocene epochs less than 10 million years ago. The genus and

an extinct genus of neoepiblemid rodent that lived from the Early to Late Miocene in what is now South America. Fossils have been found in the Cerro Bandera

Podiceps miocenicus is an extinct species of large Late Miocene grebe from Moldova. The species was found at Chișinău as part of fossil collecting survey

Eumegamys is an extinct genus of dinomyid rodent from the late Miocene and Pliocene of Brazil (Solimões Formation), Venezuela (Urumaco Formation, Urumaco)

prehistoric species are also known: Uria brodkorbi (Monterey or Sisquoc Late Miocene of Lompoc, USA) Uria affinis (Late Pleistocene of E USA)—possibly a subspecies

Persististrombus coronatus is an extinct species of fossil true conch from the Late Miocene to Pliocene (11.6-2.58 million years ago). Persististrombus coronatus

present-day Japan separated from the rest of Asia, forming islands in the late Miocene. Speciation of Ryuthela and Heptathela also occurred during this time

genus surviving for 35 millions of years, from the Early Eocene to the Late Miocene. Amphiperatherium must have been an evolutionary success, allowing the