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Grant: Discovery Grants Program - Individual

Brock University

$20,000.00

Oceans, basins and dancing dust: a palynological investigation of late cenozoic climate change and sedimentary basin analsyis

FY 2009-10

Summary
The North Atlantic Current is an important conveyor of heat and moisture to the high northern latitudes. The proposed research aims to reconstruct sea-surface conditions numerically in the North Atlantic for the past 4.9 million years as means of assessing the fluctuating influence of the North Atlantic Current over time. Such reconstructions are critical for understanding the ocean-climate system and validating computer-generated climate simulations. Described as the "dancing dust of the sea", dinoflagellates are mostly free-swimming cells and rank among the most important primary producers in today's oceans. Their organic-walled cysts, "dinocysts", are now routinely used in quantitative reconstructions of later Quaternary marine environments, especially at higher latitudes. The analysis of their fossil record allows us to reconstruct both summer and winter sea-surface temperature and salinity, the duration of sea-ice cover, and even levels of nutrient enrichment. The proposed research examines dinocysts at very high temporal resolution across seven time intervals (each about 100 thousand years duration or less) of critical paleoclimatic interest for the Pliocene through Holocene. Material will be examined from across the North Atlantic region based on existing deep-sea core material. Assemblages will be calibrated using a novel method that obtains stable isotopes and Mg/Ca ratios to serve as fully independent proxies for climate change, allowing precise tuning to an orbital timescale. Results will provide new insights into the timing and causes of Northern Hemisphere glaciations, past episides of global warming, and indeed the very mechanisms of climate change. The oil sands of Alberta place Canada second after Saudi Arabia in global oil reserves. Vitrinite reflectance and palynofacies analyses of selected units with in the Western Canada Sedimentary Basin will elucidate the potential source rocks of the Alberta oil sands, and help assess in-situ transformation of the oil. Source rock analysis will allow oil migration routes to be plotted, aiding oil exploration/exploitation in the region.
Program
Discovery Grants Program - Individual
Location
Ontario, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
327150-2009
Name nom
Head, Martin
Department département
Earth Sciences
Organization id
22
Institution établissement
Brock 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
20000
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
1
Nb partie
1
Application title
Oceans, basins and dancing dust: a palynological investigation of late cenozoic climate change and sedimentary basin analsyis
Keyword
NA
Application summary
The North Atlantic Current is an important conveyor of heat and moisture to the high northern latitudes. The proposed research aims to reconstruct sea-surface conditions numerically in the North Atlantic for the past 4.9 million years as means of assessing the fluctuating influence of the North Atlantic Current over time. Such reconstructions are critical for understanding the ocean-climate system and validating computer-generated climate simulations. Described as the "dancing dust of the sea", dinoflagellates are mostly free-swimming cells and rank among the most important primary producers in today's oceans. Their organic-walled cysts, "dinocysts", are now routinely used in quantitative reconstructions of later Quaternary marine environments, especially at higher latitudes. The analysis of their fossil record allows us to reconstruct both summer and winter sea-surface temperature and salinity, the duration of sea-ice cover, and even levels of nutrient enrichment. The proposed research examines dinocysts at very high temporal resolution across seven time intervals (each about 100 thousand years duration or less) of critical paleoclimatic interest for the Pliocene through Holocene. Material will be examined from across the North Atlantic region based on existing deep-sea core material. Assemblages will be calibrated using a novel method that obtains stable isotopes and Mg/Ca ratios to serve as fully independent proxies for climate change, allowing precise tuning to an orbital timescale. Results will provide new insights into the timing and causes of Northern Hemisphere glaciations, past episides of global warming, and indeed the very mechanisms of climate change. The oil sands of Alberta place Canada second after Saudi Arabia in global oil reserves. Vitrinite reflectance and palynofacies analyses of selected units with in the Western Canada Sedimentary Basin will elucidate the potential source rocks of the Alberta oil sands, and help assess in-situ transformation of the oil. Source rock analysis will allow oil migration routes to be plotted, aiding oil exploration/exploitation in the region.