My pilot study and extended investigation is to be conducted at Hunt's Bay, Gower.

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INTRODUCTION

My pilot study and extended investigation is to be conducted at Hunt's Bay, Gower.

Hunt's Bay or Deep Slade is situated on the Gower Peninsula facing south. The OS (ordinance survey) grid reference of hunt's bay, from a mumbles and south Gower map is 564 868 (see appendix 1). It is a rocky beach. The rocks are made up of carboniferous limestone, a sedimentary rock. We decided that the bedding planes at Hunt's Bay are about 45 degrees from each other, with smooth fronts due to erosion by the sea. This will affect the type and amount of sea life at the beach.

Cliff face

Sea

45 degrees

Aim of Pilot study

The aim of my pilot study is to conduct a transect of Hunt's Bay. From this, I will be able to produce a zonation pattern for the beach, draw a profile of the beach, calculate the exposure rating and discuss the distribution of various organisms found on the beach. This will help me with my extended investigation.

Method for conducting a transect at Hunt's Bay

The method I am going to use to conduct a transect at Hunt's Bay is the Cross-Staff method. (Refer to appendix 2)

Tides

A tide is a periodic rise and fall of all ocean waters, including those of open sea, gulfs and bays. The tide will rise and fall twice approximately every 25 hours, giving two high tides and two low tides daily. Tides are the result from the gravitational attraction of the moon and the sun upon the water and upon the earth itself.

During the periods of new and full moon, when the sun, moon, and earth are directly in line, the moon and sun pull in the same direction. This results in the condition known as spring tides, in which the high tide is higher and the low tide is lower than usual. When the moon is in first or third quarter, however, it is at right angles to the sun relative to the earth and the moon and sun are pulling at right angles to each other. This condition produces neap tides, in which the high tide is lower and the low tide is higher, than normal.

Tides

Spring tides

Neap tides

Tidal range

MHWS (mean high water spring) to MLWS (mean low water spring) in the Bristol Channel covers a rise and fall of 14 metres. Around Gower, including Hunts Bay the range is about 8 metres. It has been highlighted that low water of spring tides occurs between 12.00 and 3.00pm in this area. It takes 6 hours for the tide to come in and 6 hours for the tide to go out. The speed at which the tide covers and uncovers the shore is described as the 'rule of twelve'. In the first hour the tide rises and falls by 1/12th of its range, 2/12th in the second hour, 3/12th in the third hour, 3/12th in the fourth hour, 2/12th in the fifth hour and 1/12th in the sixth hour. Therefore, in the third and fourth hour there is most danger because the water is rising or falling faster.

Zonation pattern

The distribution of organisms on a rocky shore consists of a series of overlapping bands called the zonation pattern. It is a response to the amount of time each part of the shore is immersed in seawater and/or emersed.

The immersion/emersion cycle

The zonation pattern of plant and animal distribution is a response to the frequency and length of period of immersion and emersion, when the tide rises and falls. Immersion and emersion times change depending on the relative positions of the moon and the sun i.e. whether it is a spring or a neap tide. This week at Hunt's Bay (21st-25th September 1998) was a week of spring tides. The week before was a period of neap tides; therefore the organisms at the bottom of the beach were uncovered and exposed to the air. The previous week they remained completely immersed in seawater. At the top of the beach there will be organisms that will be briefly covered this week by the sea. Last week they spent the whole week emersed from seawater.

Environmental conditions during emersion

The most important factors affecting the upper distribution of shore organisms are:

. HEAT

2. DESICCATION

3. STRONG LIGHT (light intensity and u.v light)

Under these conditions all metabolic activities are reduced- feeding, respiration and movement. Toxic products may accumulate and the shore is open to terrestrial predators, for example birds. It is evident that organisms that occupy the upper parts of the shore need to have mechanisms to allow them to resist these factors.

Environmental conditions during immersion

When the tide is in the temperature is cool and stable. There is no worry of water loss (desiccation). The water contains dissolved oxygen, carbon dioxide, and nutrient salts together with organic detritus. Animals can move around easily. Toxic excretory products can be removed from the body. It is possible to release gametes for fertilisation.

The most important factor affecting the lower distribution of shore organisms is:

. THE LEVELS OF LIGHT

The levels of light may fall below the required compensation for photosynthesis. This will limit the lower distribution of some algae. However, different algae have overcome this problem by using different photosynthetic pigments.

The immersion/emersion cycle is affected by a number of modifying factors, the most important of which is:

. Exposure- the size and strength of the waves are the result of wind speed and FETCH i.e. the distance over which the wind and waves travel before hitting the beach. Therefore the exposure rating of the beach is affected by the geographical location of the beach.

Increased exposure will increase the vertical extent of the shore above and below its theoretical limits. The emersion factors associated with the MHWN level of a normal beach will be encountered at MHWS and above on an exposed beach. Zonation patterns will be enclosed by the theoretical limits MHWS and MLWS.

Increased exposure will also change the types of organisms to be found on the beach. The physical force of waves can dislodge organisms, crush them and smash them against the rocks. Therefore, it is likely that exposed beaches will be devoid of plant life because the violent waves and wind would destroy these organisms. It could be argued that an exposed beach would contain fewer animals than a sheltered beach and contain organisms that can survive in the harsh conditions.

2. Topography- this will affect wave action. Rough shallow slopes will dry out less rapidly than steep slopes.

3. Aspect- South-facing beaches will dry out more quickly than north facing beaches. Hunt's Bay faces south. This suggests that this will affect the extent up the beach of the zonation pattern.

4. Time of low water springs- Emersion factors will be at their strongest between 12.00 and 3.00 p.m. during the summer months. Hunt's bay experiences Low water spring tides at this time.

5. Biotic factors- These are the inter-relationship between organisms on the shore, for example:

a. Competition between and within species

b. Predation

c. Overcrowding

d. Grazing

PILOT STUDY

After calculating the exposure rating for Hunt's Bay, I have come to the conclusion that it is a semi-exposed beach to an exposed beach (see appendix 3).

After analysing my zonation pattern for Hunt's Bay (see appendix 4), I am able to describe and explain the distribution of various organisms along the beach. I am also able to draw a profile of Hunt's Bay (see appendix 5).

Distribution of the Littorinid species

The common name for the Littorinid species is periwinkles. There are four main species. These are as follows:

Littorina neritoides (small periwinkle)

Littorina saxatilis (rough periwinkle)

Littorina littorea (edible periwinkle)

Littorina obusata (flat periwinkle)

Distributed at the top of the beach, MHWN to MHWS, is Littorina neritoides. They have no ctenidium but the cavity wall is greatly folded and acts as a lung. They, therefore, do not need water all the time for respiration and this is one reason for their distribution at the top of the beach. Reproduction is via external fertilisation. They release their gametes into the water and so need a high tide. Their main excretory product is uric acid. Littorina neritoides are able to withstand desiccation and are therefore found at the top of the beach in crevices and empty barnacle shells.

Littorina saxatiliis is found on the middle of the beach near to the top, MLWN to MHWN. A ctenidium is present for respiration, but it is much reduced. The cavity wall is much folded. This periwinkle can breathe air. They do not require water all the time for respiration but need more than Littorina neritoides because their ctenidium is reduced and therefore are situated slightly further down the beach than Littorina neritoides. They possess internal fertilisation (viviparous) and the young emerge direct from the parent. This is clearly an adaptation to more of a terrestrial existence and an increased protection for the young. Their main excretory product contains some uric acid crystals, which again suggests that they are adapted to a terrestrial existence. They live in crevices and on stones on upper and upper middle rocky shores, feeding on seaweed.

Found towards the bottom of the beach, MLWN to MLWS, is Littorina littorea. A ctenidium or gill lies in a cavity, which has little folding of the wall for respiration. Reproduction is via external fertilisation and their main excretory product is ammonia, requiring a large volume of water for dilution of toxic material. It is evident that they cannot breathe, reproduce or excrete without the presence of water. Therefore, edible periwinkles are found on rocks, stones and seaweed on the middle and lower parts of rocky shores, feeding on plant debris and algae.

Littorina obtusata is found at the bottom of the beach, MLWS. A ctenidium or gill that lies in a cavity, which has little folding of the wall, is present. During fertilisation eggs are laid (oviparous) in gelatinous on seaweed. Young are shelled and they emerge directly. Their main excretory product is ammonia. Water constitutes 90% of urine whereas urea constitutes 10%. Therefore, water is needed for both respiration and excretion and that is why flat periwinkles are found right at the bottom of the shore, at the intertidal zone, where it feeds on brown seaweed. They are mainly found on sheltered shores and would be washed away on an exposed shore.
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The resistance to desiccation (without water) on the Littorina species after 7 days at 18°C has been investigated. The results are as follows:

SPECIES

% MORTALITY

Littorina littorea

70

Littorina obtusata

80

Littorina saxatilis

8-17

Littorina neritoides

0

This shows that none of the Littorina nertoides died when exposed to the effects of desiccation. It suggests that they be found at the top of the beach, MHWS, because they can survive without water for long periods of time.

This also shows ...

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