gady-i-płazy: Amniote

Evidence: 100 • authority: 72

Amniotes are tetrapod vertebrate animals belonging to the clade Amniota, a large group that comprises the vast majority of living terrestrial and semiaquatic vertebrates. Amniotes evolved from amphibious stem tetrapod ancestors during the Carboniferous period. Amniota is defined as the smallest crown clade (the group including all descendants of the last common ancestor) containing humans, the Greek tortoise, and the Nile crocodile. Amniotes represent a crucial evolutionary step in vertebrate history, marking the transition from aquatic to fully terrestrial life. Amniotes are distinguished from the other living tetrapod clade — the non-amniote lissamphibians (frogs/toads, salamanders/newts…

Evidence: 59 • authority: 72

Stegocephali (or Stegocephalia, from Ancient Greek: στεγοκεφαλια, lit. "roofed head") is a clade of vertebrate animals containing all fully limbed tetrapodomorphs. It is equivalent to a broad definition of the superclass Tetrapoda: under this broad definition, the term "tetrapod" applies to any animal descended from the first vertebrate with four limbs each with digits in the extremity (pentadactyly), rather than fins of their sarcopterygian relatives. Stegocephalians include both the modern lineage of limbed vertebrates (the crown group tetrapods, including modern amphibians, reptiles, birds and mammals) as well as a portion of the stem group, the earliest limbed tetrapodomorphs such as Ic…

Evidence: 53 • authority: 88

Clade dynamics support an early origin of crown eukaryotes. The timing of the last eukaryotic common ancestor (LECA) remains a fundamental question in evolutionary biology and palaeontology. Unambiguous eukaryotic-grade fossils appear from 1780 Ma, but no crown-group supergroups are confidently identified before the end of the Mesoproterozoic (ca. 1050 Ma). The late LECA hypothesis suggests that this absence of crown-assignable fossils and biosignatures implies a late Mesoproterozoic origin of the crown. Here we show that this hypothesis is incompatible with the evolutionary dynamics of the eukaryote clade, even under the limited constraints of the fossil record. Studying stem-crown dynamic…

Evidence: 53 • authority: 72

Reptiles, as commonly defined, are tetrapod vertebrate animals with an ectothermic metabolism and amniotic development. Reptiles traditionally comprise four orders: Testudines (turtles), Crocodilia (crocodiles, alligators and gharials), Squamata (lizards and snakes) and Rhynchocephalia (tuatara), with about 12,000 extant species listed in the Reptile Database. The study of the traditional reptile orders, customarily in combination with the study of modern amphibians, is called herpetology. Reptiles have been subject to several conflicting taxonomic definitions. In classical evolutionary taxonomy, reptiles are gathered together under the class Reptilia ( rep-TIL-ee-ə), which corresponds to c…

Evidence: 42 • authority: 72

Phylogenetic nomenclature (sometimes called cladistic nomenclature) is a method of nomenclature for taxa in biology that uses phylogenetic definitions for taxon names. Phylogenetic nomenclature assigns names to clades, groups consisting solely of an ancestor and all its descendants. This contrasts with the traditional method, by which taxon names are defined by a type, which can be a specimen or a taxon of lower rank, and a description in words. Phylogenetic nomenclature is regulated currently by the International Code of Phylogenetic Nomenclature (PhyloCode).

Evidence: 36 • authority: 92

<i>Cryptovaranoides</i> is not a squamate.. Accurate reconstruction of the timescale of organismal evolution requires placement of extinct representatives among living branches. In this way, the fossil record has the capacity to revise hypotheses of organismal evolution by producing representatives of clades that far pre-date the age of the clade inferred using phylogenies built from molecular data and previous fossil calibrations. Recently, one fossil with the potential to drastically change current understanding surrounding the timescale of reptile diversification was described from Triassic fissure-fill deposits in the United Kingdom. This taxon, † Cryptovaranoides microlaniu…

Evidence: 36 • authority: 92

Mandibular form and function is more disparate in amniotes than in non-amniote tetrapods from the late Palaeozoic.. Terrestrial tetrapods originated during the Middle Devonian, and the group rapidly diversified throughout the subsequent Carboniferous and Permian periods. Feeding in air rather than water is expected to require changes to tetrapod mandibular form and function. Previous biomechanical studies on jaw evolution, however, found that the increase in functional disparity lagged behind terrestrialisation by approximately 70 Myr, coinciding with the origin of amniotes and herbivory. We expand on a previous dataset composed primarily of non-amniote tetrapods to identify the drivers of…