Thursday, 8 October 2015
PALM TRUNK MOULD
Sunday, 20 September 2015
ERBENOCHILE ERBENI
Family Odontopleuridae, Odontopleurid trilobite from the Lower Devonian, Emsian, 408 to 393 MYA, Bou Tiskaouine Formation, Hamar l”Aghdad Limestones, Taharajat, Oufaten, Djebel Issoumour
Friday, 28 August 2015
EARLY EXPLORERS ON HORNBY ISLAND
![]() |
| Captain George Vancouver's Commission to Lieutenant |
- The Commission, dated July 10, 1783, appointing him fourth Lieutenant of the HMS Fame (this is the official document confirming a field commission given to him May 7, 1782)
- A letter to James Sykes (a Navy Agent in London) written from the ship Discovery (not the same Discovery used by Cook) while in Nootka Sound near the end of Vancouver’s exploration of the West Coast, October 2, 1794. Vancouver states that they have determined that the Northwest Passage does not exist, which was one of the main goals of his voyage
- A letter to James Sykes written from Vancouver’s home in Petersham, England, after his voyage, October 26, 1797
Saturday, 22 August 2015
Sunday, 2 August 2015
Saturday, 1 August 2015
TRIASSIC PAPER CLAMS FROM PINE PASS NEAR TUMBLER RIDGE
![]() |
| Triassic Paper clams, Pardonet Formation |
Here, in outcrops of the Pardonet Formation, the remains of once-living bivalves called paper clams—or “flat clams”—paint a vivid picture of life in the Late Triassic seas.
During the Triassic, roughly 237–201 million years ago, these delicate-shelled bivalves of the genus Moinotis, specifically Moinotis subcircularis, thrived in shallow marine environments.
Their thin, flattened shells resemble wafer-like sheets, earning them the common name “paper clams.”
Despite their fragile appearance, they were ecologically tough, colonizing vast seafloor regions after the Permian-Triassic mass extinction—Earth’s most catastrophic biodiversity crisis. In the wake of devastation, paper clams became pioneers in new marine ecosystems, spreading widely across the Triassic world.
At Pine Pass, the Pardonet Formation captures this resilience in stone. The strata—composed mainly of silty shales and fine-grained sandstones—represent an ancient seabed deposited along the western margin of Pangea. These rocks are part of the larger Western Canada Sedimentary Basin and are well known for their rich fossil assemblages, including ammonoids, conodonts, and marine reptiles. Yet, among these Triassic relics, it’s the paper clams that often dominate.
A short scramble up the rocky slope near the highway reveals bedding planes glittering with thousands of tiny, overlapping shells. They lie perfectly preserved, their paper-thin forms cemented into the matrix as though frozen in a whisper of time. Each shell records a pulse of ancient life in a warm, shallow sea teeming with invertebrates.
Our field stop at Pine Pass was a spontaneous detour en route to a paleontological conference in nearby Tumbler Ridge—a region equally famed for its dinosaur tracks and marine fossils. What was meant to be a quick roadside break became a fossil feast.
Within minutes, we were crouched among the rocks, gently tracing our fingers over Moinotis subcircularis—delicate, symmetrical, and as hauntingly beautiful as the day they settled on the Triassic seafloor.
Sunday, 26 July 2015
Wednesday, 22 July 2015
Thursday, 16 July 2015
ICHTHYOSAUR EVOLUTION
They were particularly abundant in the later Triassic and early Jurassic periods before being replaced as a premier aquatic predator by another marine reptilian group, the Plesiosauria, in the later Jurassic and Cretaceous periods.
Wednesday, 15 July 2015
KELP FORESTS AND CARBON SINKS
Some pieces stretch for meters, still tangled with small shells and bits of driftwood, while others hold tight, bulbous floats that once kept them buoyant in the underwater forests just offshore.
When the tide recedes, the air fills with the unmistakable scent of iodine and salt—an ancient perfume carried by the sea.
Kelp is a brown alga, part of the group Phaeophyceae, which evolved roughly 150 to 200 million years ago.
While kelp itself doesn’t fossilize easily (it’s soft-bodied and decomposes quickly), its ancient lineage can be traced through molecular and microfossil evidence. The earliest relatives of kelp likely appeared in the Jurassic seas, when dinosaurs ruled the land and the oceans teemed with ammonites.
Microscopic spores and chemical biomarkers in sedimentary rocks tell scientists that brown algae were already photosynthesizing in shallow coastal waters long before the first mammals appeared.
Giant kelp, Macrocystis pyrifera, holds the title for the fastest-growing marine organism on Earth—it can shoot up more than half a meter a day under ideal conditions!These towering underwater forests provide shelter and food for thousands of marine creatures, from tiny snails to sea otters, who wrap themselves in the fronds to sleep without drifting away.
Back when I used to scuba drive a lot around Vancouver Island, they were one of my favourite places to explore as those underwater forests were teeming with life.
If you’re beachcombing in British Columbia, Alaska, or California, you might find bull kelp, Nereocystis luetkeana, recognizable by its long, whip-like stipe and single round float. It’s edible and surprisingly tasty. The blades can be dried and used like seaweed chips, while the bulb can be sliced thin and pickled—an oceanic delicacy with a salty, citrusy crunch.
Other edible seaweeds you might encounter include sugar kelp, Saccharina latissima, which has a slightly sweet flavor, and ribbon kelp, Alaria marginata, often used in soups and salads.
On the foreshore near where I live on Vancouver Island, we have loads of sea lettuce. Sea lettuce, Ulva spp., is one of the ocean’s most vibrant and inviting greens—a delicate, translucent seaweed that looks like bright green tissue paper fluttering in the tide.
![]() |
| Sea Otter in a Kelp Bed |
Its thin, ruffled fronds are only a few cells thick, soft to the touch, and often cling to rocks, shells, or docks in intertidal zones where saltwater and freshwater mingle.
Unlike the giant brown kelps that form towering underwater forests, sea lettuce is part of the green algae group (Chlorophyta), sharing pigments more closely related to land plants.
It grows worldwide in temperate and tropical waters and thrives wherever nutrient-rich water flows—estuaries, tide pools, and shallow bays. When the tide goes out, you might see it draped over rocks like sheets of emerald silk, drying slightly in the sun and releasing a faint, oceanic scent.
Sea lettuce is entirely edible and a favourite among foragers and coastal chefs. Fresh from the sea, it has a mild, slightly salty flavour with a hint of sweetness—similar to spinach or nori. It can be eaten raw in salads, lightly fried until crisp, or dried into flakes and used as a natural salt substitute.
In many coastal cultures, from Ireland to Japan, Ulva has long been part of traditional cuisine. It’s also rich in vitamins A, C, and B12, along with iron and calcium—proof that sea greens can be as nutritious as they are beautiful. When my little sister was living in County Cork, she shared pictures of folk bathing in tubs of icy sea water and seaweed as a briny health spa treatment.
From a scientific perspective, sea lettuce plays an important ecological role. It provides shelter for small marine creatures like snails, shrimp, and juvenile fish, and it helps absorb excess nutrients from the water, which can help reduce harmful algal blooms.
However, when too many nutrients enter the ocean—often from agricultural runoff—sea lettuce can grow explosively, creating dense “green tides” that blanket shorelines.
Its lineage stretches deep into the fossil record as well. While soft-bodied algae like Ulva rarely fossilize, green algal relatives appear in rocks over 1.6 billion years old, making them some of Earth’s earliest photosynthesizers.
Beyond their culinary and ecological roles, kelp forests act as powerful carbon sinks, pulling CO₂ from the atmosphere and storing it in the deep ocean. They also buffer coastlines from storms and provide nurseries for fish populations that support global fisheries.
As you stroll the shoreline and your toes brush against that slippery tangle of golden-brown ribbons, remember—you’re touching the living descendant of an ancient lineage that’s been swaying in Earth’s oceans since the age of dinosaurs—beautiful, ancient and tasty!
Tuesday, 14 July 2015
Monday, 29 June 2015
GULLS ON THE FORESHORE: T'SIK'WI
![]() |
| A gull cries in protest at not getting his share of a meal |

















