life on sediment covered shores requires very different adaptations than on rocky shores bc sediments change shape all the time.
nearly all large organisms on sediment-covered shores are called infauna bc they burrow into sediment. also contian large #s of microbial communities, particularly in quiet environments i.e. salt marshes and mud flats
Physical Environment of the Sediment
sediment-covered shores include:
coarse boulder beaches
sand beaches
salt marshes
mud flats
these represent progressively lower-energy environments and are consequently composed of progressively finer sediment. the energy level that a shore experiences is related to the strength of waves and longshore currents
along shores w/ low energy levels, particle size becomes smaller, the sediment slope decreases, and overall sediment stability increases —> sediment in a fine-grained mud flat is more stable than that of a high-energy sandy beach
along high-energy sandy beaches, a large quantity of water from breaking waves rapidly sinks into sand and brings a continual supply of nutrients and oxygen-rich water for animals that live there
supply of oxygen-rich water for the animals that live there
this supply of oxygen also enhances bacterial decomposition of dead tissue
sediment in salt marshes and mud flats is not nearly as rich in oxygen —> decomposition occurs more slowly creating a “rotten egg” smell
Intertidal Zonation
intertidal zone of sediment-covered shore consists of supratidal, high tide, middle tide, and low tide zones which are best developed on steeply sloping, coarse-sand beaches and are less distinct on gentle sloping, fine-sand beaches
on mud flats, the tiny clay-size particles form a deposit with essentially no slope, so zonation is not possible in this protected, low-energy environment
species of animals differ from zone to zone:
intertidal rocky shores, max # of species and greatest biomass found near low tide shoreline and diversity and biomass decrease toward high tide shoreline
Sandy Beaches: Organisms and Their Adaptations
most animals at beach burrow into sand bc there’s no stable fixed surface —> these organisms are less obvious but get a more stable environment where not affected by fluctuations of temp and salinity or threat of drying out
Bivalve Mollusks
bivalve = animal that has two hinged shells i.e. clam or mussel
mollusk = member of phylum Mollusca, characterized by soft body and either internal or external hard CaCO3 shell
bivalve mollusks well adapted to living w/in sediment:
single foot digs into sediment to pull creature down into sand
how deeply a bivalve can bury itself depends on length of its siphons which must reach above sediment surface to pull in water for food and oxygen
indigestible matter forced back out the siphon periodically by quick muscular contractions
Annelid Worms
variety of annelids (worms) = well adapted to sediment life
Ex. lugworm constructs vertical U-shaped burrow, walls strengthened with mucus
worm feeds by extending its snout up into shaft of burrow to loosen sand w/ quick pulsing movements
cone shaped depression forms at surface over head end of the burrow as sand continually slides into burrow and is ingested by the worm
as sand passes through the worm’s digestive tract, the sand''s biofilm is digested, and the processed sand is deposited back at the surface
Crustaceans
crabs, lobsters, shrimps, barnacles = chracterized by segmented body, hard exoskeleton, paired, jointed limbs
Ex. on most sandy beaches, numerous crustaceans called beach hoppers feed on kelp cast up by storm waves or high tides
Ex. sand crabs: move up and down the beach near shorline, burying bodies in sand leaving long curved v-shaped antennae pointing up beach slope
filter food particles from water
Echinoderms
sand stars, heart urchin
sand stars prey on invertebrates that burrow into low-tide region of sandy beaches
well-designed for moving through sediment: smooth back and five tapered legs w/ spines
heart urchins = flatter and elongated
live buried in sand near low tide line
gather sand grains in mouths where biofilm or organic matter that coats sand grains is scraped off and ingested
Meiofauna
meiofauna = small marine organisms that live in the spaces between sediment particles
feed on bacteria attached to surface of sediment particles
Ex. polychaetes, mollusks, arthropods, nematodes
live in sediment from intertidal zone to deep-ocean trenches
Mud Flats: Organisms and Their Adaptations
eelgrass and turtle grass widely distributed in low tide zone of mud flats and adjacent shallow coastal regions
numerous openings at the surface of mud flats attest to large population of bivalve mollusks and other invertebrates
Ex. fiddler crabs dig burrows within mud flats to live in
RECAP
sediment-covered shores including sandy beaches and mud flats have a nintertidal zonation similar to that of rocky shores but also contain many organisms living w/in the sediment (infauna)
CONCEPT CHECK 15.2
(1) Describe how sandy and muddy shores differ in terms of energy level, particle size, sediment stability, and oxygen content.
sandy = higher energy level —> lower sediment stability —> higher oxygen content
muddy = lower energy level —> higher sediment stability —> lower oxygen content
(2) How does the diversity of species on sediment-covered shores compare with that of the rocky shore? Suggest at least one reason why this occurs.
sediment-covered shores = much less species diversity bc they’re composed of unconsolidated materials that often change shape and so require specific adaptations for organisms —> harder for organisms to live here
(3) In which intertidal zone of a steeply sloping, coarse-sand beach would you typically find each of the following organisms: clams, beach hoppers, ghost shrimp, sand crabs, and heart urchins?
clams - low-tide
beach hoppers = high tide
ghost shrimp = low tide
sand crabs = middle tide
heart urchins = middle tide