Grant: Discovery Grants Program - Individual
Queen's University
$141,000.00
Facies anatomy and early diagenesis of carbonate rocks
FY 2011-12
Summary
Research Summary
) Limestones, made of marine fossils, are archives of evolution in the marine biosphere, our best record of past oceans and development of the ocean-atmosphere system, amongst the nation's most prolific hydrocarbon reservoirs, and aquifers for fresh waters. Research is focused on the least understood but widespread type of limestone, those that formed in cool to very cold ocean waters. Studies are located in the modern ocean and the rock record and include the Southern Ocean (the largest modern area of these deposits), relatively young rocks of similar composition exposed onshore, limestones in the Canadian Arctic that formed during the Late Paleozoic Ice Age (LPIA-350-245 Ma), and carbonates that were deposited during the most profound glaciation the world has ever known (Neoproterozoic ~800 Ma) and exposed in the Mackenzie Mountains, NWT and Australia.
) Funds are requested for the: 1) acquisition and analysis of marine samples from the Australian continental shelf and slope, 2) detailed study of relatively unknown modern cold-water neritic environments wherein kelp control production of carbonate sediment, 3) documentation of the relationship between nutrients and coral reef growth at the tropical-temperate interface, 4) utilization of bryozoan proxies to determine specific cool-water paleoceanographic environments, 5) establishment of sedimentological and paleontological criteria to define boundaries between depositional realms, 6) use of the LPIA to understand how the globe came out of a glacial period like the one we are in today, 7) determination, via the nature of carbonate sedimentation, how the ocean evolved during the Neoproterozoic global glaciation just before the evolution of animals and finally, 8) experimentation to determine, via direct observation under controlled conditions, how microbes affect specific aspects of carbonate sediment formation. A total of 11 students will be trained.
Program
Discovery Grants Program - Individual
Recipient
Location
Ontario, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data
As published
Application id
2028-2009
Name nom
James, Noel
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
2011
Competition year année de concours
2009
Award amount
141000
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
1203
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Earth sciences
Area of application fr
Sciences de la terre
Research subject code
4000
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Earth science (see also marine geology 4604)
Research subject fr
Sciences de la terre (voir aussi géologie marine, 4604)
Partie
3
Nb partie
5
Application title
Facies anatomy and early diagenesis of carbonate rocks
Keyword
NSERC
Application summary
Research Summary
) Limestones, made of marine fossils, are archives of evolution in the marine biosphere, our best record of past oceans and development of the ocean-atmosphere system, amongst the nation's most prolific hydrocarbon reservoirs, and aquifers for fresh waters. Research is focused on the least understood but widespread type of limestone, those that formed in cool to very cold ocean waters. Studies are located in the modern ocean and the rock record and include the Southern Ocean (the largest modern area of these deposits), relatively young rocks of similar composition exposed onshore, limestones in the Canadian Arctic that formed during the Late Paleozoic Ice Age (LPIA-350-245 Ma), and carbonates that were deposited during the most profound glaciation the world has ever known (Neoproterozoic ~800 Ma) and exposed in the Mackenzie Mountains, NWT and Australia.
) Funds are requested for the: 1) acquisition and analysis of marine samples from the Australian continental shelf and slope, 2) detailed study of relatively unknown modern cold-water neritic environments wherein kelp control production of carbonate sediment, 3) documentation of the relationship between nutrients and coral reef growth at the tropical-temperate interface, 4) utilization of bryozoan proxies to determine specific cool-water paleoceanographic environments, 5) establishment of sedimentological and paleontological criteria to define boundaries between depositional realms, 6) use of the LPIA to understand how the globe came out of a glacial period like the one we are in today, 7) determination, via the nature of carbonate sedimentation, how the ocean evolved during the Neoproterozoic global glaciation just before the evolution of animals and finally, 8) experimentation to determine, via direct observation under controlled conditions, how microbes affect specific aspects of carbonate sediment formation. A total of 11 students will be trained.