Principal Investigator:Vavrek, Matthew J Licensed Year(s):
2013
Summary:
This project is a continuation of the collaborative research program on ancient biodiversity in the Canadian Arctic. Recently, the group completed work supported by Polar Continental Shelf Project in the Brackett Basin in the westcentral Northwest Territories and the Bonnet Plume Basin in northeastern the Yukon Territory, during which the research team recovered both new vertebrate (dinosaur) foss...
Principal Investigator:Cumbaa, S.L. Licensed Year(s):20102008
1997
1995 Summary:
We plan to conduct geological and paleontological exploration and research, checking Devonian-age rocks exposed along a 1-2 km stretch of the Anderson River to look for bones and scales of fossil fish contained within the rocks. These rocks, and the fossils within them, are approximately 400 million years old. In 1995, we discovered bones of a primitive lungfish (an ancient, lobe-finned, air-bre...
Principal Investigator:Johnston, Paul A. Licensed Year(s):
1994
1991 Summary:
The research team will search parts of Cornwallis and Ellesmere Islands for fossils of ancient sea and land creatures that lived more than 400 million years ago. Of special interest are remains of eurypterids (sea scorpions), giant armoured fishes, jawless fishes, molluscs and early land animals. The fossils will be used for new exhibits and educational programs at the Royal Tyrrell Museum and t...
Principal Investigator:Basinger, James F. Licensed Year(s):
1994
1993199219911990198919881987 Summary:
The oldest known land plants are found in rocks of about 400 million years old. Rocks of this age are rarely found in North America. Recently, fossils from this critical interval have been found on Bathurst Island (preliminary work in 1993). The researchers will explore other possisible sites on central Bathurst Island. The fossils recovered will contribute to the understanding of early plant ...
Principal Investigator:Marino, Bruno D. Licensed Year(s):
1992
Summary:
The researcher will sample plants and shells containing records of the stable isotopic composition of the constituents in the environment that are used for growth. The natural abundance of the stable isotopes of carbon in atmospheric CO2 and in dissolved groundwater as well as the hydrogen and oxygen isotopes in water can be related to climatic factors. Thus, these isotope ratios in shells and p...