A comparison of vestigial zeugopodal and autopodal elements in ruminants and their potential use in establishing phylogenetic relationships [PDF]
, 2013 Hamilton, Charles H. +3 more
core +1 more source
New giraffoid fossils from the later Early Miocene Lothidok Formation (West Turkana, Kenya): Implications for early giraffoid diversity [PDF]
, 2013 Grossman, Ari +2 more
core +1 more source
New Middle Miocene Ape (Primates: Hylobatidae) from Ramnagar, India fills major gaps in the hominoid fossil record. [PDF]
Proc Biol Sci, 2020 Gilbert CC +7 more
europepmc +1 more source
Ruminant macroevolution: a phylogenetic approach based on extant faunas [PDF]
, 2013 Cantalapiedra, Juan L. +2 more
core +1 more source
Combined LM and SEM study of the middle Miocene (Sarmatian) palynoflora from the Lavanttal Basin, Austria: Part V. Magnoliophyta 3 - Myrtales to Ericales. [PDF]
Grana, 2020 Grímsson F +3 more
europepmc +1 more source
New insights into tragulid phylogeny of Europe: Dorcatherium naui from the latest Middle Miocene of Austria [PDF]
, 2013 Aiglstorfer, Manuela +3 more
core +1 more source
Geological processes shaping freshwater biodiversity: a synthesis of global evidence
Biological Reviews, Volume 101, Issue 3, Page 1568-1581, June 2026.ABSTRACT Recent genomic data highlight the key roles of geological processes in shaping the diversification and biogeography of freshwater lineages. Specifically, physical processes such as tectonic uplift, erosion, glaciation, lake formation, and sea‐level fluctuation contribute extensively to the evolution of biotic diversity within and among ...
Jonathan M. Waters +3 more
wiley +1 more source
Dental eruption in ruminants and other mammals [PDF]
, 2013 Asher, Robert J., Wörheide, Gert
core +1 more source
New Zealand Journal of Geology and Geophysics, Volume 69, Issue 2, June 2026.Clasts of albite‐porphyroblastic quartzofeldspathic schist, derived from the Otago Schist basement, occur within the Port Chalmers Breccia, a diatreme at the centre of the Dunedin stratovolcano, New Zealand. Schists have undergone varying degrees of replacement reactions (at temperatures of 300° to >500°C) producing hornfelses, with Ca‐ and K‐enriched ...
Alan F. Cooper
wiley +1 more source
New Zealand Journal of Geology and Geophysics, Volume 69, Issue 2, June 2026.Mordenite is a naturally occurring zeolite mineral that is the seventh most common zeolite mineral globally, forming at low temperatures (≥100°C) in hydrothermal systems. In New Zealand, extensive deposits of mordenite are commonly associated with areas of hydrothermal alteration, particularly in the Coromandel and Taupo Volcanic Zones.
Ayrton R. Hamilton +6 more
wiley +1 more source