Grant: Discovery Grants Program - Individual
Queen's University
$77,000.00
Neoproterozoic paleobiology
EF 2009-10
Résumé
The Neoproterozoic (1000-542 million years ago) was an era of profound change in the Earth system. Large-scale changes in the physical and chemical environment of Earth, including break-up of a supercontinent and a series of extreme global ice ages, occurred in concert with equally fundamental changes in the evolution of life. Over the next five years my students and I will carry out research on the appearance of the first animals and other large creatures on Earth (as represented by the Ediacara Biota) and on the evolution of carbonate systems towards modern-style systems, including early reefs. Most of my research efforts will focus on the Ediacara Biota (578-542 million years ago). These soft-bodied creatures that appeared at the end of the Neoproterozoic ice ages mark "when life got big" after 3 billion years of mostly microbial evolution, and represent the oldest large, complex life forms anywhere. Almost all of them were entirely soft-bodied, without any evidence of skeletons, muscles, guts, or brains. Some Ediacaran forms may have been stem-groups that led to all modern animal life; others appear to represent "failed experiments" in the evolution of life. Our studies will focus on Newfoundland, which contains the oldest and some of the best preserved Ediacaran assemblages known anywhere. Investigating deep-water Ediacaran assemblages from NW Canada will help to assess the global character of the fossils. Searches for as yet undiscovered Ediacaran fossils below the main fossil levels in Newfoundland and Australia will test the roles of glaciation and oxygenation in the evolution of large animals I also will study carbonates from NW Canada and Australia that were deposited between the two greatest Proterozoic ice ages (Cryogenian, about 750-635 million years ago) to document the effects of biotic evolution and global climate change on the development of carbonate systems through the Proterozoic Eon. These studies will form the core of my research activities and will provide support and research materials for 3 MSc students, 2 PhD students, a PDF, and 13 undergraduate field assistants over the next five years.
Programme
Discovery Grants Program - Individual
Bénéficiaire
Emplacement
Ontario, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data
Tel que publié
Application id
2648-2009
Name nom
Narbonne, Guy
Department département
Geological Sciences and Geological Engineering
Organization id
29
Institution établissement
Queen's University
Province en
Ontario
Province fr
Ontario
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2009
Competition year année de concours
2009
Award amount
77000
Program id
RGPIN
Program nane en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
8
Committee name en
Solid Earth Sciences
Committee name fr
Sciences de la Terre solide
Area of application code
1200
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Advancement of knowledge
Area of application fr
Avancement des connaissances
Research subject code
4010
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Paleontology, paleobiology
Research subject fr
Paléontologie, paléobiologie
Partie
1
Nb partie
5
Application title
Neoproterozoic paleobiology
Keyword
NA
Application summary
The Neoproterozoic (1000-542 million years ago) was an era of profound change in the Earth system. Large-scale changes in the physical and chemical environment of Earth, including break-up of a supercontinent and a series of extreme global ice ages, occurred in concert with equally fundamental changes in the evolution of life. Over the next five years my students and I will carry out research on the appearance of the first animals and other large creatures on Earth (as represented by the Ediacara Biota) and on the evolution of carbonate systems towards modern-style systems, including early reefs. Most of my research efforts will focus on the Ediacara Biota (578-542 million years ago). These soft-bodied creatures that appeared at the end of the Neoproterozoic ice ages mark "when life got big" after 3 billion years of mostly microbial evolution, and represent the oldest large, complex life forms anywhere. Almost all of them were entirely soft-bodied, without any evidence of skeletons, muscles, guts, or brains. Some Ediacaran forms may have been stem-groups that led to all modern animal life; others appear to represent "failed experiments" in the evolution of life. Our studies will focus on Newfoundland, which contains the oldest and some of the best preserved Ediacaran assemblages known anywhere. Investigating deep-water Ediacaran assemblages from NW Canada will help to assess the global character of the fossils. Searches for as yet undiscovered Ediacaran fossils below the main fossil levels in Newfoundland and Australia will test the roles of glaciation and oxygenation in the evolution of large animals I also will study carbonates from NW Canada and Australia that were deposited between the two greatest Proterozoic ice ages (Cryogenian, about 750-635 million years ago) to document the effects of biotic evolution and global climate change on the development of carbonate systems through the Proterozoic Eon. These studies will form the core of my research activities and will provide support and research materials for 3 MSc students, 2 PhD students, a PDF, and 13 undergraduate field assistants over the next five years.