Essay about Ecobeaker1

In site one there was a high proportion of very unspherical rocks. According to this the hypothesis is right, in site two there is a lot more smother rocks medium sized and in site 3 there are very small pebbles which are very smooth and spherical. The pebbles get smoother and rounder while it goes downstream. Due to us only taking about 10 rocks our result may have been not right as there were some pebbles which were largely over sized. Most of the other load is dissolved by solution such as limestone and chalk

The second factor, allopatric speciation, occurred between the two rodents’ habitat. This is when a population is divided by a geographic barrier which prevents interbreeding between the two populations. These species are found on two different islands, so the water in between separates the two populations from interacting with one another. Due to this, both species could have developed changes in courtship rituals, developed new traits, and undergone changes to adapt to their environment.

With our observation of the Shawangunk formation, we see a sedimentary rock formation containing a range of grain size. Such sizes range from pebbles (3cm-5cm), fine-grain sand, and medium-grain sand. There is some grading towards the bottom left of the outcrop known as a reverse grading with some small cross beds present (Figure 2). The grading occurs towards a slight part of the outcrop where we see the grading beginning as fine grain sediments and working up to coarser grain. With moderate sorting we see variations of degree of sorting per bed. As the degree of sorting varies as does the sphericity. The sediment bedding is well seen ranging in sizes of +/--20 cm to 40 cm. This outcrop has thick beds as one can see the basic units with cracks in between each (Figure 3). With mostly tabular beds consisting of sub-angular, and sub-rounded sediments, this outcrop also consists of some ventricular beds (Figure 4). When looking at figure 4, we have a small space of a ventricular bed present. This is because the bed comes in, pinches thicker bedding,

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.

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 profile of Pallarenda beach as shown in figure 1 is very typical of a North Queensland, medium energy beach. The lack of organisms present higher up the beach was due to the harsh conditions at low tide. Ghost Crabs, Ocypode quadrata, can survive these areas as a result of their adaptations (The Otter Island Project). The ghost crab burrows during the day and feeds at night to avoid the heat of the day (The Otter Island Project). These crabs can actively take up moisture from damp sand to wet their gills (The Otter Island Project).

This concept is displayed in the inquiry as I will be reviewing the change within the stalactites formation and what the effect is when rainfall is involved.

To confirm my assumption, which is ‘each day has different tide cycle,’ I compare our data to Corte Madera tide table. On Wednesday 19th, Corte Madera Creek has first low tide at 3:37 AM and second low tide at 2:57 pm. The first high tide was at 10:05 am and the next high tide was at 9:22 pm. The tidal coefficient was 67 (middle). The maximum high tide recorded in the tide tables for Corte Madera Creek which is of 7.2 ft and a minimum height of -2.0 ft.

4. Choose one of the geological periods listed in figure 3.8 and find out all you can about it. How are rock formations from that period identified? What are its most characteristic fossils? Where are the best samples of rock from your chosen period?

Questions and charts are from Geoscience Laboratory, 5th ed. (p. 133-150), by T. Freeman, 2009, New York, NY: John Wiley & Sons. Reprinted with permission.

Know the adaptations of organisms found in the tidal pool ecosystem – to do this, match up the following

Using the National Environment Agency website, 2016, the tide information was noted and dates with tides of 0.5m or less are chosen to survey the locations. Low tides are ideal as there will be a higher chance of seeing T. gigas at the shore.

The Supra-littoral zone is one of the harshest terrains for organisms to exist in. The organisms that live in this region are facing problems like gas exchange, desiccation, temperature changes and feeding. It is only covered during storms and extremely high tides and is moistened by the spray of the breaking waves. Organisms are exposed to the drying heat of the sun in the summer and to extreme low temperatures in the winter. Because of these severe conditions, only a few resistant organisms live here. The dominate organisms that reside within this zone are Blue grey Periwinkles. Using Transect lines for over 30m, we evaluated the effects of several factors on this zone, including (1) predation, (2) herbivory, (3) plant—plant competition, (4) plant—animal competition, and (5) physical disturbance from high—energy waves. The interaction having the greatest effect on the structure of this zone was desiccation and high temperatures. However the Blue grey Periwinkle has been specially adapted to the harsh conditions of the dry upper littoral zone. They are able to trap water inside their shell to prevent moisture escaping, and cling to the rock face while the tide is out. As we can see from the abiotic data the temperature at the Supra littoral zone is also very high reaching 25 degrees compared to the other zones reaching only 20 degrees. Furthermore the special adaptations of the Blue Grey Periwinkle allow it to be the most dominant

The cave gudgeon, Milyeringa veritas is a small, eye-less fish that lives in the groundwater aquifers of cape range and barrow island (Exmouth – Jarvis well 136km). It is found in both freshwater caves and seawater anchioline systems, and inhabits the karst wetlands in Miocene limestone. Populations have been found up to 4.3km inland from the coast, and within 150m. Their habitat is affected by marine tides, which determine the distance they will inhabit from the coast, relating to the high and low tides. They have a wide depth range and have been seen swimming in karst windows at the surface, and to depths of 33m. The fish can occur in hyperoxic surface water and suboxic waters beneath the pynocline. The cave gudgeon is only associated with

Another abiotic factor that helps the formations of different zones would be the tidal movement (aerial exposure) effecting the sea life shore community. The tidal zones we found at Siren’s Rocks are the sublittoral zone, low tide, mid tide, high tide and supralittoral zone. These are all on the data recorded by us at the rocky shore we researched.