Vancouver Island Marmot Bones From Subalpine Caves: Archaeological and Biological Significance

This is Occasional paper no.4 by Dave Nagorsin and Grant Keddie of the BC Museum, Victoria, and Tanya Luszcz, Biology Cooperative Ed Program U.Vic. Abstract Since 1985, faunal remains of the Vancouver Island marmot have been discovered in four high elevation cave sites: Clayoquot Plateau, Mariner Mountain, Limestone Mountain, and the Golden Hinde. Two sites

Seasonality of Hydroids (Hydrozoa, Cnidaria) from an intertidal pool and adjacent subtidal habitats at Race Rocks, off Vancouver Island, Canada

Anita Brinckmann-Voss Published in Scientia  Marina 1996 ( SCI MAR.,60(1):89-97 ) Advances in Hydroid Biology.  S. Piraino, F. Boero J. Bouillon, P.F.S. Cornelius and J.M. Gilli (eds.) SUMMARY: An assemblage of 27 hydroid species was reported from a tide pool in the lower rocky intertidal zone, and compared with 42 hydroids of the adjacent subtidal

Rhysia fletcheri ( Cnidaria,Hydrozoa, Rhysiidae) a new species of colonial hydroid from Vancouver Island ( B.C. Canada) and the San Juan Archipelago (Washington, U.S.A)

BRINCKMANN-VOSS, A., LICKEY, D. M., and MILLS, C. E. 1993, published in the Can. J. Zool. 71: 401-406. A new species of colonial athecate hydroid, Rhysia fletcheri, is described from Vancouver Island, British Columbia Canada, and from Friday Harbor, Washington, U.S.A. Its relationship to Rhysia autumnalis Brinckmann from the Mediterranean and Rhysia halecii (Hickson and

Katherine Tye ER #116 Management Statement

(This statement is intended for use in conjunction with the descriptive text and map pages supplied in the “Guide to Ecological Reserves in British Columbia”). Features Requiring Special Management Consideration: A small population of the rare and endangered . The orchids are not consistently flowering every year. As many as 100 specimens were observed by

Parker Lake Ecological Reserve Overview, Biological and Physical

hysical: The reserve lies on a flat, boggy lowland within the Alberta Plateau. Low hills rise one or two kilometres to the north and Pouce Creek to the south has cut a channel into the lowland surface . However, the entire reserve is level and boggy with no organized drainage pattern. Four small shallow lakes,