EIGHTH BC PALEONTOLOGICAL SYMPOSIUM

KWAK'WAKA'WAKW MATRILINE AND PATRILINE

The Kwakwaka’wakw are characterized by a particular iconographic promiscuity, a tendency to mobilize a diverse set of visual, material, or performative signs that index their individual standings. There may be various explanations for this. 

The Kwakwaka’wakw are geographically and culturally at the point on the central coast where the strictly matrilineal groups of the north (e.g., Tlingit, Haida, Tsimshian) give way to more patrilineal and less clan/crest-based patterns of descent in the south (Nuu-Chah-Nulth and Coast Salish), and they have long been known as the grand synthesizers of the region. 

Bilateral reckoning of Kwakwaka’wakw descent entails the claiming of crest images and personal prerogatives from both the matriline and patriline, increasing the number of images an individual might legitimately display. 

They developed and maintained through the assimilationist period the most elaborate system of restricted ceremonial performance of the famous ‘‘secret’’ or ‘‘dance’’ societies described by Franz Boas (1897) and Philip Drucker (1940) which is predicated on rather flexible and negotiated hereditary rights to (often multiple) ritual dramas and the accompanying regalia (see Roth 2002:144). 

The Kwakwaka’wakw have long proved remarkably amenable to participating in their own ethnographic representation, from adapting their visual motifs and performances to intercultural contexts of display, to applying the technologies and institutions of modernity to their own modes of cultural production (Glass 2004, 2006)

AMMONITE COQUINA

CASTLE PEAK: CANADIAN ROCKIES

PALEO FIELD TRIP :: TASEKO LAKES

GOAT: CAPRA AEGAGRUS HIRCUS

 

ALBERTASAURUS

PAIX ET TRANQUILITÉ

SOLAR PERFECTION: ENGLISH BAY

MISTER KANE

MISTER KANE

FOSSIL FIELD TRIP BASE CAMP

INSIGHT: ICE CORE LOOKING GLASS

Evidence from the past provides a window into the Earth's future. A sediment core from 400m below the seabed of the Arctic Ocean showed that Fifty-five million years ago, deep in the Eocene, the North Pole was ice-free and enjoying tropical temperatures. It also tells us that the temperature of the ocean was 20C, instead of the coolish –1.5C we see today… a truth that is hard to imagine with all the press surrounding global warming.

The bottom end of that core helped explain the fossils found at Eocene sites around British Columbia, species commonly seen in more tropical environments today. The warmer temperatures seen at McAbee and around the globe were recorded in the core sample and reveal evidence for a global event known at the Palaeocene-Eocene Thermal Maximum. Back in the Eocene, a gigantic emission of greenhouse gases was released into the atmosphere and the global temperature warmed by about 5C.

While the bookends of the geologic time scale slide back and forth a wee bit, the current experts in the geologic community set the limits to be 33.9 +_ 0.1 to 55.8 +_ 0.2 million years ago. The fossil record tells us that this part of British Columbia and much of the Earth was significantly warmer around that time, so warm in fact that we find temperate and tropical plant fossils in areas that now sport plants that prefer much colder climes, or as is the case in the Arctic, snow and ice.

The Okanagan Highlands is an area centred in the Interior of British Columbia, but the term is used in a slightly misleading fashion to describe an arc of Eocene lakebed sites that extend from Smithers in the north, down to the fossil site of Republic Washington. The grouping includes the fossil sites of Driftwood Canyon, Quilchena, Allenby, Tranquille, McAbee, Princeton and Republic. These fossil sites range in time from Early to Middle Eocene, and the fossil they contain give us a snapshot of what was happening in this part of the world because of the varied plant fossils they contain..

While the area around the Interior of British Columbia was affected. McAbee was not as warm as some of the other Middle Eocene sites, a fact inferred by what we see and what is conspicuously missing.

The plant species suggest that McAbee had a more temperate climate, slightly cooler and wetter than other Eocene sites to the south at Princeton, British Columbia and Republic and Chuckanut, Washington. Missing are the tropical Sabal (palm), seen at Princeton and the impressive Ensete (banana) and Zamiaceae (cycad) found at Republic and Chuckanut, Washington.

While we are the likely culprits of much of the warming of the Arctic today, the sediments of McAbee tell us that natural processes operating in the not too distant past have also resulted in significant temperature fluxuations on a world-wide scale.

"LOOK, LOOK, LOOK" A DAY AT THE ZOO

If you are feeling a bit hemmed in from all the cold weather, bundle up and take a trip to the Vancouver Aquarium, Science World or your local museum.

There is nothing more exciting than witnessing the awe on a child's face as they begin to explore the natural world.

If you've got a thing for fossils, remember to check out the ancient critters as well. The Royal BC Museum, Qualicum Beach Museum an Courtenay Museum all have permanent fossil displays. If you are in Vancouver, head on down to Science World to see their T-Rex. There re also many fossil exhibits planned at the new Beatty Biodiversity Museum openig later this year at UBC.

SAINT-RÉMY-DE-PROVENCE

HORNBY ISLAND EASTER EGG HUNT

CIEL

JOHN LEAHY COLLECTION

THE BEST OF SOOKE: TY COLLWYN RETREAT

Heading to Victoria for a jaunt or to the village of Sooke for a bit of fossil collecting?

Ty Collwyn Waterfront Retreat offers private, oceanfront, two bedroom cottages within walking distance from the heart of Sooke, on Vancouver Island. We are located just forty minutes west of Victoria; the capital city of British Columbia, Canada.
Our two cottages share wonderful ocean views of Sooke Harbour and the Juan de Fuca Strait; each with it's own deck and hot tub to soak away stress.

The grounds include a heated indoor pool, coin-operated laundry facilities, private dock, and waterfront with a fire pit, all surrounded by lush trees and an acre of grass area.

When you are not relaxing and enjoying your oceanfront view, take advantage of all that Sooke has to offer. Enjoy a scenic drive to our beautiful West Coast beaches, visit the Sooke Potholes, catch a wave surfing, go ocean kayaking, try a fishing charter, check out the Sooke Museum, walk along the wonderful Whiffin Spit, or travel any of the region's hiking trails on foot, rollerblade, or bicycle. There is so much to do!

Later, you can dine at the world renowned Sooke Harbour House Restaurant, famous Mom's Café, or create your own barbeque feast right on your deck.