Bringing Oregon Natural History to Life Through Plant and Animal Fossils
 
March 9, 2010
 
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Oregon Fossil Guy Trading Depot
Bivalve Fossils (clams) have shells divided on a left-right axis and are
generally hinged together with a single adductor muscle. Here’s a list of
the most common bivalve fossil species on Oregon’s coast and a brief
description of each:
Anadara devincta—Oregon’s most common marine fossil, similar in appearance and shape to the cockles of today (see photo at right). Anadara devincta isan indicator fossil worldwide for Miocene-age formations.
Katherinella angustri—another common clam fossil with a broad,
smooth-patterned shell, often found agatized, or translucent.
Macoma arctata—a thin, flat shell, often having a hole drilled by snails
(which then ate the clam inside).
Chione ensifera—a shell with a cross-hatched pattern, similar to the steamer clams available in restaurants.
Panopea arupta—a very large shell, measuring over four inches across.
Patinopectin/Vertipectin—a large scallop shell, found whole in flat, round
concretions, sometimes split by nature, often held in seawalls.
Common Miocene gastropods making Oregon’s coast their home include:
Gastropods (snails): While clams are the larger and more populous of Oregon’s Miocene marine fossils, gastropods are frequently found, especially inconcretions. For some, the attraction of gastropods results from the artistic 180° twist the shell makes during its growth, called torsion. Most gastropods—herbivores and carnivores—use an armored tongue, or “radula,” as a tool to drill through shells into their meals.
Bruclarkia oregonensis—a squatty shaped shell, accented with delicate
whorls.
Nassarius arnoldi—a shell with short and slender whorls and artistic ribs
Musashia indurata—a very large shell, nearly six inches long, seldom found
whole.
Ficus modesta—a well-rounded shell with a fig-like shape and delicately
lined whorls.
Turritella oregonensis—a shell with high spires, in a tightly curved design,
often found in groups.
Crepidula praerupta—an extinct, androgynous, clawlike snail, which moved incolonies linked together.
Chlorostoma pacificum—a shell with a short, rounded design and a
well-defined whorl.

Calicantharus carlsoni—similar in look to modern whelks, often fossilized
with a Membranipora coat (similar to moss on a tree or lichen on a rock).
Dentalium schencki—sometimes known as a “tusk shell”—look for “white
drinking straws” in brown or gray rocks.
Wood and Bone Fossils:
In addition to abundant marine fossils, Oregon’s coast offers a wide variety
of petrified woods. As ocean currents moved along the shoreline and rivers
ran into the Pacific Ocean, wood species from other regions were deposited
on Oregon’s beaches.
Teredo wood appears as brown to black rocks, usually rounded at the ends
with a “Swiss cheese” look to them. Fossilized casings from the Teredo
marine clam created the pattern when the Teredo, in its larval form, ate its
way through chunks of ancient wood. These colonies of small larvae never
cross each other’s borings, making each piece unique in design and
appearance.
Other petrified woods are light tan to carbonized black, frequently found in
sizes ranging from one inch to two feet across. Look for a dull sheen on wet
rocks with parallel wood grain patterns. Softwood species of pines and some
hardwoods, including alder, myrtlewood, and oak, as well as petrified palm,
are also found on Oregon beaches.
An occasional fossilized leaf impression can be found on or in coastal
rocks, recognizable as elm, alder, and Oregon Grape—Mahonia repens.
Petrified wood pieces are also often found in concretions of rounded
mudstone or hard gray volcanic ashballs. Sometimes split in half by nature,
inside these concretions is often carbonized or fossilized wood that was
once carried downstream from the Cascade Mountains. Crabs are one type ofarthropod found inside concretions when split open—claws, legs, and
occasionally whole crabs.
Another genre of fossil found on Oregon’s coast is mammal bone. Usually
deposited in hardened sandstone, bone is as abundant as Teredo wood and
Anadara shells. Look for light brown or gray rocks with rounded edges and adarker edge or center, which is usually bone.
Careful matrix removal can expose identifiable fossilized bone, including
vertebrae, ribs, jaw bones, joints, and skulls, which may be from
prehistoric whales, dolphins, porpoises, sea lions, or seals.