Gooseneck Barnacles G. Anderson Gooseneck
barnacles, scientific name Pollicipes polymerus, have the characteristics of the more
common volcano-type barnacles (like the buckshot and Balanus), in that they are also
filter feeders, capable of living rather high in the intertidal, being
hermaphroditic, cross fertilizers, and having numerous planktonic larvae.
They differ in that their bodies are on top of a permanently attached stalk
covered with a thick skin. This stalk is a wonderful
seafood (no guts inside) and tastes much like clam when steamed.
Gooseneck
Barnacle clumps (G. Anderson) They
can live 20 years, or more. As they grow they make new calcareous plates
protecting their bodies. When first secreted, these plates are shiny and
pearlescent. After repeated high tides and battering waves (with sand and
rocks), the pearly shells become pitted and dull.
Gooseneck Barnacle with a new shiny calcium plate
(above left), Gooseneck Barnacle with dull and pitted calcium plates (above
right) G. Anderson It is interesting to look through these masses of
gooseneck barnacles in our tidepools and see newly
secreted shells. This means that the barnacle is happy, healthy and growing. Mussels
Gooseneck Barnacles and Mussels (K. Meldahl) Mussel
showing byssal threads and their attachment pad to
the rock (G. Anderson)
When they are young they can loosen their threads and move
about a bit, but when they are older most of them stay put. They do not
hesitate to grow on top of each other and other species - resulting in
interesting mussel clumps that are themselves a habitat harboring over 100
species of marine organisms. Mussel,
its shells being used as a substrate by Buckshot Barnacles (G. Anderson) Mussels open their shells just a crack at high tide to
feed, which allows them to circulate 2-3 quarts of seawater through their
shells each hour - mucus on their gills traps plankton for their food. When
there is a lot of plankton mussels can grow up to three inches each year and
will overgrow most other species. But they rarely get a chance to live lower
in the intertidal because their main predator, the sea star, consumes them. Studies done by scientists who remove
the sea stars from rocky intertidal areas show that mussels will prevail all
the way to 20 feet below sea level as giant clumps if left unchecked by their
natural predator. Other factors also affect them, like big waves tearing off
clumps, that get too large, or parasites, but it is the sea star that has the
most influence. Aggregating Anemones The aggregating anemone, scientific name Anthopleura elegantissima,
dominates southern California rocky shorelines from the lower part of the middle
tide zone down to the upper part of the low tide zone. Each anemone is round, with a mouth in the middle.
The mouth is surrounded by feeding tentacles that have stinging cells capable
of capturing small crustaceans, fish and anything that happens to touch them
that cannot get away. The tentacles feel sticky to humans, but we are only
feeling their 'sticky' cells. The real stinging cells of the aggregating
anemone cannot penetrate our hands so it is safe to touch them.
Transition
from California Mussels of the Middle Tide Zone to Aggregating Anemones of
the Low Tide Zone (G. Anderson)
Aggregating Anemones with their tentacles pulled
in at low tide (G. Anderson) Food that is gathered by the
tentacles is pulled to the mouth where it is ingested and digested. They are
very simple animals, without a complete digestive tract, and thus there is no
anus. So, ingested material that is not digested (like shells and bones) must
be regurgitated back out the mouth. Sounds rather unpleasant, but this
explains why sometimes the tidepool anemones look
like they are turning inside out. Wayward periwinkle snails, if they have
toppled from their high perch, may be swallowed by these anemones, but the
snail will usually keep its trap door operculum closed until the anemone
tires of its presence. Then, when the anemone spits it out, the periwinkle
snail starts its long trip back up the rock to its preferred (and safe)
Splash Zone. At low tide these anemones pull
in their tentacles and become a lump on the rock. The sides of their bodies
are covered with adhesive structures that attach bits of shell, rock and seaweed.
When closed up at low tide the attached material causes the anemone to look
like a bed of crushed shell, but when you touch it, the anemone (whose body
can be up to 80 percent water) releases water and feels gushy. The bits of
debris probably reflect light to keep the anemone cooler and reduce water
loss at low tide since these critters do not have a protective shell. The
debris could also be dispersing wave action as the tide ebbs and flows each
day. Aggregating
Anemone clone, lower half under water (open) and upper half above water
(closed) pictured above (G. Anderson) An exciting thing happens when two clones meet.
Members of the same clone extend their tentacles at high tide and do not mind
touching members of their own clone … but, should a member of another clone
be touched, they fight until one moves or dies. There are special fighting
tentacles (that are deflated and not visible until a clone war starts) tucked
just under the regular tentacles and the outside of the body. These special
fighting tentacles are called acrorhagi and
during a clone war they are inflated. They look different than the regular
tentacles, being shorter, rounder, and very white. These acrorhagi
are fully illustrated later in this lesson when discussing the starburst
anemone.
Anemone
free area between two aggregating anemone clones (above left), Close up of
anemone free area (above right) (G. Anderson)
|