All the sponge parameters measured in our study in between the two discrete depth zones revealed a clear statistical difference and consistently higher values for the shallow location except from the sponge surface area (Median shallow,deep = 85, 152 cm2, respectively) and oscular number per sponge area (Median shallow,deep = 0.04, 024 cm2 respectively). Similar to our study of turbidity in the previous section the parameters given above for the deeper zone was higher for the sponges with lesser pumping rates, but this difference observed to be eminent for the depth comparison (Table 4). The comparative study of shallow and deep locations at the two pristine sites of southern side of Bodrum Peninsula showed that there is a high chance of …show more content…
The most efficient sponge patch at the deep site processed 0.166 cm3 cm-2 s-1 amount of seawater with 23 oscula collectively pumping. These numbers clearly show that C. reniformis specimens possessing few numbered large sized osculas, pump more efficiently than sponges with many small sized oscula. This raises a question in mind; is it better to have single enormous sized oscule or many smaller sized osculas? Our analysis marks out a discrete large sized oscule provides a clear advantage on pumping efficiency to the sponges living in the wave zone, but in the meantime at a cost of maintaining a smaller sized body and perhaps less growth. The sponge specimens living in the deeper zones compensates this disadvantage by spreading through a larger surface and forming many oscular openings.
The shallow pristine site, Meteor Bay is generally protected from wave action, but there are regular storm events throughout the year. Absence of oceanic water currents leaves wave action as the major source of mixing and water movement. A possible advantage for C. reniformis specimens to acquire larger sized oscules might be described with the need of catching desired food particles in a water movement zone affected by wave action. Continuous oscillation of particles in a wave action could make it harder to catch desired particles for a
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).
In 1607 three ships carried more than 100 passengers that found an island and named it Jamestown. But little did they know what terrors lay ahead of them. In 1607 three English ships had traveled through Cheesecake Bay and sailed up to the James river. The three ships than found an island and named it after King James. In the beginning only men came to the island, but after some years women and children began to come to Jamestown as well. Jamestown was not full of animals. Jamestown was full of death and misery for the English. From 1607-1610 many Jamestown colonists had their lives stolen from them due to Indians, lack of food, and disease.
Along the coasts of rocky beaches, an intricate ecological community inhabits the ‘rocky intertidal’ areas. The variety of rocks is home to an array of slimy, squishy, and colorful organisms. This intertidal community is comprised of nine species: three different algae, three stationary filter-feeders, and three mobile consumers. The three algae, Nori Seaweed, Black Pine, and Coral Weed, are the community’s producers and inhabit the bottom of the food chain. The next three species are stationary consumers. They are Mussel, Goose Neck Barnacle, and Acorn Barnacle. Because of their consumer status, they are more competitively dominant than algae. The last three components are the mobile consumers: Whelk, Chiton, and Starfish. They
Only one method of planktonic sampling was used so comparison with another method of sampling cannot be done. It is safe to assume that the most appropriate method of sampling in these areas was previously determined by the lab instructor. Isolation of organisms in the samples was met with some difficulty as there was very little life to be observed. Once isolated however, a general identification was simple with the use of the “quick picks” section of the Marine Invertebrate Zoology Lab Manual. One particular organism isolated from the “T-docks” samples, a foraminiferida, was chosen for scientific drawing (Figure 1).
The Sublittoral is the region of the ocean below the low tide limit and extends all the way to the edge of the continental shelf. This zone is submerged permanently despite the turn of the tides and the intra/interspecific competition for space is extreme. Organisms in this region rarely experience intense sun or air exposure and organisms such as blue
An investigation into the effects of varying seawater concentrations on two marine invertebrates’ osmoregulatory abilities; Carcinus maenas and Arenicola marina.
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.
For millennia, terrestrial plant matter, seeds, and driftwood have travelled across the open oceans with the help of surface currents. Even floating islands, also known as tussocks, floatons, or sudds are common in many Florida lakes and across the world (Mallison, C.T., 2001). These islands have been known to carry exotic plants and vertebrate animals. Floating islands promote trans-ocean dispersal of marine and terrestrial organisms. This increases biodiversity and helps new barren islands thrive. However, in the last five decades, with the growing number of plastics in the marine environment, the dispersal and occurrence of these organisms has increased exceedingly (Gregory, R.M., 2009). This paves the way for invasions by alien and even aggressive invasive species to establish themselves in new ecosystems beyond their native range. A survey done in 2009 reported that over 150 marine species have established themselves due to marine debris stranded on the shores of northern New Zealand. Most of these organisms were identified as crustaceans. Four of those organisms discovered are featured in figure 3. Specimen A shows various crustaceans on unknown plastic, specimen B depicts warm water Indo-Pacific oysters growing on nylon rope, specimen C depicts crustaceans growing on a plastic pellet, and specimen D depicts a bryozoan colony attached
The off-shore marine environment changes intensively with the change in the ocean depth. There are three distinctive zones that can be classified along the depth which is the Epipelagic which extends from the sea surface to a depth of 200 meters, the mesopelagic which extends from a depth of 200 meters to a depth of a 1000 meters and then the Deep sea which extends from a depth of a 1000 meters to the sea floor (Castro & Huber, 2010). The Deep sea can then be divided into a further three zones (Figure 01) Bathypelagic which extends from a depth of a 1000 meters to 4000 meters, Abyssopelagic which extends from a depth of 4000 meters to 6000 meters and then the Hadopelagic which extends which extends from a depth of 6000 meters to the sea floor (Castro & Huber, 2010).
Coastal regions are strongly affected by water motion due to tides and wave energy Graham & Wilcox, 2000; Jonsson et al, 2006; Wolcott, 2007). Jonsson et al. (2006) found that Fucus vesiculosus located on the seaward side
Floras and microbes are additional main biotic mechanisms of many oceanic ecosystems. Microbes act as decomposers for oceanic ecosystems, and they break defunct living matter and transforms it into vitality that is used by other existing organisms in the oceanic ecosystem. Detrivores, which are a type of animal, also eat deceased or putrefying plants and animal matter. Algae, which are autotrophs, appear as the head herbal vivacity and primary producers in oceanic ecosystems. The sunlight transforms the light into energy for nourishment for marine plants. Heat and light are focal abiotic factors discovered in essentially all oceanic ecosystems, consequently oceanic ecosystems has some broaden abiotic mechanisms, comprising viscosity and many more. The power that the bulk of an organism is called buoyancy. The durability of the drive of seawater is called viscosity. These abiotic factors source to the drive of all organisms in oceanic systems. Sunlight pierces the sea exterior only about 65 feet. As there is more salt in the Great Barrier Reef than in other oceanic ecosystems the marine holds less oxygen than the
Rocky Shores are found where the sea meets the land which supports a diverse mix of plants and animals that have adapted to survive in the unique conditions of constant wave action as well as the fall of tides (Ehp.qld. 2016). Most of the ecosystems flora and fauna live in the intertidal zone, between high and low tide (Ehp.qld. 2016). They are exposed to two environments, being crushed by waves and swamped by the sea water, extreme temperatures and salinity, and left unprotected
Germany was suffering under the harsh conditions of the treaty of Versailles, the economic downturn as a result of the Great Depression and the weakness of the Weimar republic all allowed for Adolf Hitler and the Nazi party to gain control of Germany. The Treaty of Versailles made the government of Germany look weak because other countries took land away from Germany. The Germans were paying money to other countries because of all the damage they had done in World War 1. They also had to take the blame for starting World War I and they could only have an army of 100,000 men. Germany suffered a lot in the Great Depression which spiralled Germany in despair. Hitler promised the people that he would bring life back to Germany which meant more money into Germany, more land and he will bring back Germany’s pride. However there were negative aspects to Hitler’s rule.
The coral reef surveyors were instructed to find the best sites that they believed had the most living coral and were thought to be least affected by human activities. This would allow Hodgson to determine if human activities were having an appreciable effect on the supposed pristine coral reefs, which were distant from urban centers. The invertebrate survey was undertaken at two depth intervals of 3m and 10m. Four 0.5 m wide by 20 m long belts were placed on the coral reef. Over a period of 3-5 minutes the observers counted the number of invertebrates found on the belts. The coral survey was performed, by placing four 20 m long belts on the coral substrate. At 0.5 m intervals the substrate on which the belts were lying was examined and recorded.
With the development of medical sciences, mortality and morbidity related to medical treatment and management has reduced. Further effort to reduce this further is an ongoing process (Subhash, 2005). Unforeseen and expected complications and even death do occur during the