MDKPAD

The radiation of modern mammals: release from dinosaur incumbency or response to environmental change?

 Coordinatore UNIVERSITY OF BRISTOL 

 Organization address address: TYNDALL AVENUE SENATE HOUSE
city: BRISTOL
postcode: BS8 1TH

contact info
Titolo: Mrs.
Nome: Maria
Cognome: Davies
Email: send email
Telefono: +44 117 3317352

 Nazionalità Coordinatore United Kingdom [UK]
 Totale costo 299˙558 €
 EC contributo 299˙558 €
 Programma FP7-PEOPLE
Specific programme "People" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013)
 Code Call FP7-PEOPLE-2013-IIF
 Funding Scheme MC-IIF
 Anno di inizio 2015
 Periodo (anno-mese-giorno) 2015-01-01   -   2016-12-31

 Partecipanti

# participant  country  role  EC contrib. [€] 
1    UNIVERSITY OF BRISTOL

 Organization address address: TYNDALL AVENUE SENATE HOUSE
city: BRISTOL
postcode: BS8 1TH

contact info
Titolo: Mrs.
Nome: Maria
Cognome: Davies
Email: send email
Telefono: +44 117 3317352

UK (BRISTOL) coordinator 299˙558.40

Mappa


 Word cloud

Esplora la "nuvola delle parole (Word Cloud) per avere un'idea di massima del progetto.

determination    mesozoic    substrate    evolution    time    mammal    did    fossil    forests    dwelling    dinosaurs    diversity    habitat    mammals    dinosaur    angiosperm    cretaceous    until   

 Obiettivo del progetto (Objective)

'Did dinosaurs suppress the evolution of large mammals, or was early mammal size and diversity more related to the environmental conditions? Mammals first appeared in the Late Triassic, and lived alongside dinosaurs during the rest of the Mesozoic (Jurassic and Cretaceous), during which time they were all small and generalized in their ecologies. Only after dinosaur extinction (at the end of the Mesozoic) did mammals diversify into larger and more specialized forms, and so suppression by dinosaur competition is the usual explanation for this evolutionary pattern. I propose that the vegatational habitat was the more important factor. The angiosperms (flowering plants) that make up the majority of today’s vegetation did not appear until the Cretaceous, and did not become the dominant flora until the Cenozoic. Angiosperm forests are multi-strated with a large diversity of fruits and seeds, and provide a more suitable habitat for mammals than the gymnosperm (e.g.. conifers) forests of the Mesozoic. Towards the end of the Cretaceous, angiosperm leaf morphology had evolved such that the trees would be able to create their own microhabitats, making rain forests possible. This time period provides a window of opportunity to see if mammal evolution changed in response to the encroaching angiosperm dominance. There is evidence of dietary change at this time (to more herbivory), but was there also a change in substrate use; i.e., in the proportions of tree-dwelling versus ground-dwelling mammals? Many isolated skeletal elements can be used in the determination of locomotor behavior, but while they can be found in fossil assemblages they are usually not described. Examination of such elements will enable the determination of whether or not fossil mammal communities underwent an ecological shift in substrate use at the end of the Cretaceous, and will answer the question of whether mammal evolution is influenced more by the floral environment than by the presence of dinosaurs.'

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