Major evolutionary transitions transpire in an environmental context. Thus, to understand the advent of novelty or exaptation in evolution, aptations and nonaptations must be resolved with ecological insight. Previous work on the origin of terrestrial vertebrates has focused on reconstructions of paleoenvironments or isolated examples of axial and appendicular function, but little work has been done to synthesize the role of evolutionary morphology and evolutionary theory in the origin of terrestrial locomotion, or to integrate paleoecological reconstructions to address the environments within which these changes evolved. To understand the origin of axial and appendicular systems in their ecological context, I have combined data from a desc...
The taxonomically diverse terrestrial tetrapod fauna from the late Mississippian East Kirkton Limest...
One of the most intriguing questions in vertebrate evolution is how tetrapods gained the ability to ...
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...
<div><p>The origin of terrestrial vertebrates represents one of the major evolutionary and ecologica...
The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transf...
The hypothesis that tetrapods evolved from elpistostegids during the Frasnian, in a predominantly aq...
Evidence for terrestriality in early tetrapods is fundamentally contradictory. Fossil trackways attr...
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...
Synopsis The diversification of the tetrapod stem group occurred during the late Middle through the ...
The fish-tetrapod transition is one of the most important evolutionary events in Earth’s history, gi...
The colonisation of freshwater and marine ecosystems by land vertebrates has repeatedly occurred in ...
Living tetrapods owe their existence to a critical moment 360-340 million years ago when their ances...
ABSTRACT—The origin of tetrapods from sarcopterygian fish in the Late Devonian is one of the best kn...
The taxonomically diverse terrestrial tetrapod fauna from the late Mississippian East Kirkton Limest...
One of the most intriguing questions in vertebrate evolution is how tetrapods gained the ability to ...
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...
<div><p>The origin of terrestrial vertebrates represents one of the major evolutionary and ecologica...
The origin of terrestrial vertebrates represents one of the major evolutionary and ecological transf...
The hypothesis that tetrapods evolved from elpistostegids during the Frasnian, in a predominantly aq...
Evidence for terrestriality in early tetrapods is fundamentally contradictory. Fossil trackways attr...
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...
Synopsis The diversification of the tetrapod stem group occurred during the late Middle through the ...
The fish-tetrapod transition is one of the most important evolutionary events in Earth’s history, gi...
The colonisation of freshwater and marine ecosystems by land vertebrates has repeatedly occurred in ...
Living tetrapods owe their existence to a critical moment 360-340 million years ago when their ances...
ABSTRACT—The origin of tetrapods from sarcopterygian fish in the Late Devonian is one of the best kn...
The taxonomically diverse terrestrial tetrapod fauna from the late Mississippian East Kirkton Limest...
One of the most intriguing questions in vertebrate evolution is how tetrapods gained the ability to ...
The end-Devonian to mid-Mississippian time interval has long been known for its depauperate palaeont...