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Cornwallis Island
Cryostratigraphical studies of ground ice formation and distribution in a High Arctic polar desert landscape, Resolute Bay, Nunavut 1
Hirnantian (Ordovician) through Wenlock (Silurian) conodont biostratigraphy, bioevents, and integration with graptolite biozones, Cape Phillips Formation slope facies, Cornwallis Island, Canadian Arctic Islands
Retiolitine graptolites from the Aeronian and lower Telychian (Llandovery, Silurian) of Arctic Canada
A new Gorstian radiolarian fauna from the upper Silurian of the Cape Phillips Formation, Cornwallis and Bathurst islands, Canadian Arctic
Excessive thickening of the cortical layer in graptolites
Ontogeny and Astogeny of the Graptolite Genus Appendispinograptus (Li and Li, 1985)
Complex Noncalcified Macroalgae from the Silurian of Cornwallis Island, Arctic Canada
Palaeocope ostracods from the Silurian Wenlock Series of Arctic Canada
UPPER WENLOCK CERATOIKISCIDAE (RADIOLARIA) FROM THE CAPE PHILLIPS FORMATION, ARCTIC CANADA
Structural geology and Zn-Pb mineral occurrences of northeastern Cornwallis Island: implications for exploration of the Cornwallis Fold Belt, northern Nunavut
GRAPTOLITES FROM THE LUNDGRENI BIOZONE (LOWER HOMERIAN: SILURIAN), ARCTIC ISLANDS, CANADA: NEW SPECIES AND SUPPLEMENTARY MATERIAL
The brachymetopid trilobite Radnoria in the Silurian (Wenlock) of New York State and Arctic Canada
HAPLOTAENIATUMIDAE AND INANIGUTTIDAE (RADIOLARIA) FROM THE LOWER SILURIAN OF THE CAPE PHILLIPS FORMATION, CORNWALLIS ISLAND, NUNAVUT, CANADA
Sheinwoodian (uppermost Lower Silurian) Radiolaria from the Cape Phillips Formation, Nunavut, Canada
Early Silurian (Wenlockian) δ 13 C profiles from the Cape Phillips Formation, Arctic Canada and their relation to biotic events
PALAEOSCENIDIIDAE (RADIOLARIA) FROM THE LOWER SILURIAN OF THE CAPE PHILLIPS FORMATION, CORNWALLIS ISLAND, NUNAVUT, CANADA
The Setting and Age of the Bermuda Zn-Pb Showing, Grinnell Peninsula, Devon Island: Implications for MVT Mineralization in the Canadian Arctic
Abstract Graptolites flourished from earliest Ordovician to Early Devonian, a time range of about 90 million years, and were widely distributed as marine benthic and planktonic colonial organisms around the world. They were diverse and rapidly evolving and, as such, make excellent “index fossils” for relative age-dating of their enclosing basinal rocks. Rarely, however, graptolites are beautifully preserved in their original three-dimensional form, and can be extracted from the enclosing rock for detailed study under scanning electron microscope. Such a unique preservation is pervasive in the latest Ordovician to latest Silurian rocks of the central Arctic Islands of Canada, presenting an opportunity to study their complex morphology and evolution, making the Arctic graptolite sequence unique in the world. The present study examines the isolated, uncompressed as well as flattened forms from the Ludlow and Pridoli (Upper Silurian) graptolites of the Arctic, recognizing 46 species of monograptids and retiolitids of which seven are described as new species or subspecies.