New insights into tragulid phylogeny of Europe: Dorcatherium naui from the latest Middle Miocene of Austria [PDF]
Aiglstorfer, Manuela +3 more
core +1 more source
First hominoid from the Late Miocene of Niger
Since the discovery of Orrorin tugenensis in the Late Miocene Lukeino Formation, Tugen Hills, Kenya, it is generally admitted that the origin of bipedal hominids occurred earlier than 6 Myr ago and that the adaptation to bipedal stance and locomotion initially occurred in a forested or well-wooded setting.
Pickford, M. +3 more
openaire +2 more sources
The lacustrine Gördes Supradetachment Basin was developed along the Simav detachment fault during postorogenic extension in the north of the Menderes Massif in western Anatolia. The basin‐fill succession is represented by alluvial fan, Gilbert‐type delta, shoal‐water delta, foreshore, shoreface, offshore‐transition and peat‐forming mire deposits.
Ayhan Ilgar +5 more
wiley +1 more source
<i>Samotherium boissieri</i> from the Late Miocene of Southern Italy. [PDF]
Marra AC.
europepmc +1 more source
Sperm whales (Physeteroidea) from the Pisco Formation, Peru, and their trophic role as fat sources for late Miocene sharks. [PDF]
Benites-Palomino A +5 more
europepmc +1 more source
<i>Nakalipithecus</i> and Evolution of Late Miocene Hominoids
Masato Nakatsukasa, Yutaka Kunimatsu
openalex +2 more sources
Dental eruption in ruminants and other mammals [PDF]
Asher, Robert J., Wörheide, Gert
core +1 more source
Raman Spectroscopic Analysis and In Situ Heating Experiments on Adranosite Minerals
This study provides the first detailed Raman spectroscopic characterization of rare ammonium sulfates adranosite, iron‐rich adranosite, and adranosite‐(Fe) from volcanic and coal‐fire environments. Distinct spectral features reveal compositional differences and structural effects of Fe substitution.
Filip Košek +4 more
wiley +1 more source
Terrestrial temperature history reveals Late Miocene rapid uplift of the northern Tibetan Plateau. [PDF]
Liang Y +9 more
europepmc +1 more source
Large-number detrital zircon U-Pb ages reveal global cooling caused the formation of the Chinese Loess Plateau during Late Miocene. [PDF]
Zhang H +10 more
europepmc +1 more source

