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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. |
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