As the Cellana denticulata is distributed in the upper lower intertidal zone and the mid tide zone it must be able to withstand the upper lower intertidal zone and the mid tide zone as the rocky shore experiences tidal fluctuations (abiotic factor) that occurs in a regular pattern in which the beach has submerged areas and desiccated areas (the niche of the Cellana denticulata) this is an abiotic factor that affects their survival. Tidal fluctuations are when the tide (sea) comes in and submerges areas of the rocky shore while others are exposed. The tide ranges in vertical differences along the rocky shore; from high tide, mid tide to low tide this is called zonation. These are the tides that fluctuate in a regular pattern along the rocky shore and this is mainly due to the gravitation pull of the moon. However the sun also affects the tides but has less gravitational force as the sun is further away from earth. The gravitational pull of the moon is the main cause for tidal fluctuations as the moon has a stronger gravitational pull as it is closer to the earth than the sun, hence the main cause for tidal fluctuations as the gravitational pull from the moon exerted onto earth is greater than the earth. Because the earth is in constant motion of rotation the earth and the moon become closer in distance as the earth is not perfectly round and has uneven surfaces. These uneven surfaces or areas of the earth are closer in distance to the moon and therefore the gravitational pull
The middle shore, or middle tide zone, is submerged by water for approximately half of the cycle. This means that there is the capability to support much more marine vegetation, specifically seaweeds. The organisms found there are more complex and larger in size than further up the shore.[9] The rock pools can provide a suitable habitat for small fish, sea urchins, shrimps and zoo plankton. This area is more diversified than the upper shore.
At day 11 the organisms that are at the highest part of the rock experience the greatest exposure to air because the tide does not get as high during neap tides.
The Tidal zones consist of splash zone, high water neap tide, low water neap tide, high water spring tide, low water spring tide, mid tide level and the splash zone and sub littoral zone. All of these tidal zones can be determined by which indicator organisms/animals are living there. For an example the splash zone is the highest of all zones and the organisms that are generally living there are noddiwinkles. If you spot a lot of honeycomb barnacles and blue-grey periwinkle’s then you are most likely in the high water tide zone and water only covers this zone at high tide. White tube worms are indictor organism the mid tide level zone and is covered by water for half of the day. There’s also the low tide zone which is engulfed in water for the majority of the day expect at low tide, you can determine this zone by finding indicator organisms such as sea squirts. The final tidal zone is the sub literal zone and this is always under water the indictor organism’s living here are brown tubeworms and striped girdled chiton.
The sandy shores of beaches can be considered as a very harsh environment to live in (Ted Klenk, 1999). Survival in such a habitat requires an organism to withstand strong wave and current action, tidal rise and fall, unstable substrate, heavy predation and wide variations in salinity and temperature (The Otter Island Project). Any organism found in this type of harsh environment is specialized and highly adapted (The Otter Island Project).
Red tide is the common name for a large concentration of certain species of dinoflagellates. This event accumulates harmful algal blooms quickly, resulting in discoloration near the surface water. Dense enough algal blooms cause harmful toxins strong enough to affect people and the oceans ecosystem as a whole. Karenia brevis is the most troublesome species of dinoflagellate in the Gulf of Mexico. This species reproduces by asexual cell division, therefore, given the right conditions, the population can rapidly increase in size. K. brevis needs large amounts of the correct nutrients to reproduce at toxic speed. The nutrients responsible for supporting Florida's red tide are nitrogen and phosphorus.
What are the 3 conditions organisms in a tidal pool ecosystem must be able to withstand?
A coastal plain is a low flat surface that is a part of the coast of the Atlantic ocean. This area takes up almost half of the whole state of North Carolina. Here you get all four seasons, and sometimes you can see it snow on the beach while it can also get to 100 degrees The Outer Banks is made of three parts. This includes the Tidewater, Outer banks, and the Inner Coastal Plains. The outer banks is about 175 miles long and consists of many barrier islands. Barrier islands are thin islands separated from shore by sounds. A sound is a narrow, large body of water that separates the two parts of land. Some of the islands include Hattera,Oracoke, and Bodie islands. Though these islands are major vacation spots in North Carolina they include
Dutch expert Henk Ovink once told New Times that “Miami will no longer be a land city, but a city in the sea.” (Weiss, 2015). There has been a rise of 10 inches in sea levels in the 19th century. As of today, the East Coast and Gulf of Mexico of the United States are the two areas that are more prone to sea level rises (Infographic, n.d.). Miami is the fourth-largest population in the world that is susceptible to this predicament. On top of that, it seems that floods are becoming more frequent and more damaging than ever. It is estimated by the end of the century, Miami can get another rise of 6 to 10 feet of water (McKie, 2014). There are clear signs of the tides taking effect in the city. Homes and shops are being surrounded by water in
Geology of major natural system: Overall, in regards to geology, beach dunes are known for typically containing parallel zones of an upper beach area, undulating foredune, transition dune, and lastly a stable dune- which slopes upward and away from the water’s edge (Web World Wonders, n.d.a.). Primarily, all dunes are known to be driven by wave-sand interactions with
The ocean is one of, if not, the largest biome on earth. There are more than one million species of marine life. Covering over 70 percent of the Earth’s surface, the ocean is our planet’s largest habitat, containing 99 percent of the living space on the planet. This area holds the life of nearly 50 percent of all species on Earth. Like lakes, oceans are subdivided into separate zones: intertidal, pelagic, abyssal, and benthic. All four zones have a great diversity of species. The intertidal zone is the region along the shoreline between average low tide and average high tide. In other words, this region goes through cycles of submergence and exposure to air. Animals in this zone must be able to survive the extended periods
Great waves toss and turn with great force. Rushing as they collide with the earth soaking the soft sand. The ocean seemed to be howling as every wave grew as tall as a mountain. Slowly, the water creeps forward, then lazily seeping back in the vast ocean, only to do the same over and over again. The deep sea is a mysterious place where sea creatures lurk beneath the waves. Blue, sparkling water is everywhere you look with no end. The humming waves seem to whisper as if telling me the most confidential secret. You can never really hear them clearly until you dive in deeper and deeper.
The intertidal rocky shore of Caloundra Beach is inhabited by diverse range of biodiversity of animals and plants, many of which have developed high levels of adaptations throughout their existence. The very boundary of marine and terrestrial ecosystem, this environment is subjected to extremes of the physical environment such as temperature, desiccation, wave turbulence as well the ecological interactions that commonly occur in biotic communities (e.g. competition, predation). However Rocky intertidal shores are easily accessible by humans and provide an enjoyable opportunity for passive recreation and for science and environmental education as well.
Littoral drift occurs as incoming waves move toward the beach at an angle, transporting sediment particles to shore at the same angle (swash), while backwash pulls particles straight back into the water. The resulting zig-zag motion moves particles along a shoreline, eventually forming features such as barrier islands, tidal inlets, and spits. (Loved seeing Dauphin Island in the
In the movie The Prince of Tides, the kind of Psychotherapy being portrayed is Psychodynamic. Psychodynamic therapy is a deriving from the psychoanalytic tradition, views individuals as responding to unconscious forces and childhood experiences and seek to enhance self-insight. The therapist in the movie uses the patients brother to find out the root of the patients disturbing Psychodynamic behavior. By doing so she discovers the darkness of the family’s history.
The investigation of these tidal zones showed that most of the organisms are not evenly distributed. The tidal organisms are often hidden in cracks, shades and gullies to prevent them from being dislodged by the wave action or desiccation.