<div><p>The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transformations in the history of life, and the established timing and environment of this transition has recently come under scrutiny. The discovery and description of a well-preserved fossil sarcopterygian (fleshy-limbed vertebrate) from the Middle Devonian of Nevada helps to refine and question aspects of the temporal and anatomical framework that underpins the tetrapod condition. This new taxon, <em>Tinirau clackae</em>, demonstrates that substantial parallelism pervaded the early history of stem-tetrapods, raises additional questions about when digited sarcopterygians first evolved, and further documents that incipient stages of the te...
The fossil record provides unique clues about the primitive pattern of lobed fins, the precursors of...
The hypothesis that tetrapods evolved from elpistostegids during the Frasnian, in a predominantly aq...
The end-Devonian to mid-Mississippian time interval has long been known for its depauperate palaeont...
The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transf...
The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transf...
The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transf...
Major evolutionary transitions transpire in an environmental context. Thus, to understand the advent...
Recent discoveries of advanced fish-like stem-tetrapods (for example, Panderichthys and Tiktaalik) h...
Synopsis The diversification of the tetrapod stem group occurred during the late Middle through the ...
ABSTRACT—The origin of tetrapods from sarcopterygian fish in the Late Devonian is one of the best kn...
Among the morphological changes that occurred during the ‘fish-to-tetrapod’ transition was a marked ...
Exploration and analysis of vertebrate fossils from the non-marine facies of the Upper Devonian Cats...
Tetrapod fossil tracks are known from the Middle Devonian (Eifelian at ca. 397 million years ago--MY...
The origin of digit-bearing tetrapods in the Middle to Late Devonian (ca. 393–360 Mya) and their sub...
Evidence for terrestriality in early tetrapods is fundamentally contradictory. Fossil trackways attr...
The fossil record provides unique clues about the primitive pattern of lobed fins, the precursors of...
The hypothesis that tetrapods evolved from elpistostegids during the Frasnian, in a predominantly aq...
The end-Devonian to mid-Mississippian time interval has long been known for its depauperate palaeont...
The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transf...
The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transf...
The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transf...
Major evolutionary transitions transpire in an environmental context. Thus, to understand the advent...
Recent discoveries of advanced fish-like stem-tetrapods (for example, Panderichthys and Tiktaalik) h...
Synopsis The diversification of the tetrapod stem group occurred during the late Middle through the ...
ABSTRACT—The origin of tetrapods from sarcopterygian fish in the Late Devonian is one of the best kn...
Among the morphological changes that occurred during the ‘fish-to-tetrapod’ transition was a marked ...
Exploration and analysis of vertebrate fossils from the non-marine facies of the Upper Devonian Cats...
Tetrapod fossil tracks are known from the Middle Devonian (Eifelian at ca. 397 million years ago--MY...
The origin of digit-bearing tetrapods in the Middle to Late Devonian (ca. 393–360 Mya) and their sub...
Evidence for terrestriality in early tetrapods is fundamentally contradictory. Fossil trackways attr...
The fossil record provides unique clues about the primitive pattern of lobed fins, the precursors of...
The hypothesis that tetrapods evolved from elpistostegids during the Frasnian, in a predominantly aq...
The end-Devonian to mid-Mississippian time interval has long been known for its depauperate palaeont...