Marine Life Society of South Australia Inc.

Newsletter

January 2007   No. 339

“understanding, enjoying & caring for our oceans”

 

Next Meeting

 

This will be the February Meeting and it will be held as usual at the Conservation Centre on the 21st February commencing at 7.30pm. Our guest speaker is member Robert Browne who will be telling us about the Aquariums he has visited all over the world.

 

                                                                             

CONTENTS

Pipefish (Kevin Smith)

What’s hot!?  The Climate Change and Greenhouse

Emissions Reduction Bill 2006  (Robert Browne)

South Australia’s Jetties (Steve Reynolds)

 

 

EDITORIAL

 

I hope you all had a great Christmas and have made some New Year resolutions.

 

Could one of them include the writing of articles for the Newsletter? I am very short of a variety of articles.

 

The Journal has been well received but the next one will be about 40 pages maximum as the printing and download times for the larger Journal caused some problems.

 

The 2007 calendar has almost broken even on the sales front but we still have three boxes to sell or they will be wasted. We are working on the 2008 version now. If you have any really great underwater pictures then please get them to me ASAP.

 

 

Pipefish found in South Australian Waters

 

Kevin Smith gave an excellent talk on the various species of Pipefish found in South Australian waters at our General Meeting in October 2006. Several members missed the talk so Kevin has agreed to let me publish the slides from the talk in a few of our Newsletters.

Of course the additional comments and explanations, questions and video footage cannot be included.

However, I hope this will give you some idea of the identification of the various Pipefish.

Editor

 

 

 



Pipefish

-a presentation to the Marine Life Society of South Australia
18th of October, 2006.

 

Pipefish

         With seahorses, seadragons and pipehorses, pipefish are members of the family Syngnathidae (tail pouch).

         They are generally small and thin with a body possessing bony plates formed into a series of rings.

         Pipefish are sexually dimorphic.

         Female fish deposit eggs into a male’s brood pouch located on the ventral surface of the tail. The young are released alive and live independently of the adults.

         While more than twenty species of pipefish are found in South Australian waters this presentation includes only those encountered by the author.

 

 

Identification

         Identification keys use observable features to distinguish between types.

         Some pipefish are easily recognisable although others may need careful assessment.

         The most useful identification features and methods are:

       raised ridges on the trunk, tail, snout and operculum

       presence or absence of fins and the number of rays on each

       counts of trunk and tail rings, in particular those under the dorsal fin

       snout length relative to head length

 

 

 

 

 

 

Some of the more easily recognisable types:

 

Brushtail Pipefish
Leptoichthys fistularius

 

         Up to 65cm

         large caudal fin

         hovers horizontally in and over Posidonia and Zostera beds.

         often found in groups

 

 

 

 

Brigg’s Crested Pipefish
Histiogamphelus briggsii

 

         Found in sandy areas near the protection of rocks, algae or seagrass but also out in the open.

         Can look very similar to decaying posidonia.

 

 

 

 

 

 

 

Rhino Pipefish
Histiogamphelus cristatus

 

         Also known as Macleay’s Crested Pipefish.

         Has a short head with a very high dorsal snout ridge.

 

 

 

 

What’s hot!?  The Climate Change and Greenhouse Emissions Reduction Bill 2006

 

by Dr Robert Browne, MLSSA Science Officer.

 

What’s hot?, is the planet as one climate record after another gets broken, is the rapid thawing of the Tundra and the Arctic, is the increasing drought cycle in southern Australia as predicted in most greenhouse warming models, is that run away greenhouse effect may already be occurring as the vast deposits of carbon are released from the Tundra, and that climate warming is the greatest threat to biodiversity. 

 

What’s hot? is that a new approach to the value, use, and pollution of the atmosphere is required at an international level. Increasing evidence shows that the prevention of climate warming should be the paramount concern of humanity and that societies could collapse under the stress of a greenhouse world. Recent effects of climate change, including heat waves, droughts, violent storms, and floods will increase in size. These crises will be accompanied by destruction to life and property, loss of agricultural production, and loss of natural habitat – including marine habitat. 

 

The Conservation Council of South Australia’s General Meeting in August addressed ‘Responding to Climate Change. Speakers were Maggie Hine, from the Climate Change Division, Department of the Premier and Cabinet, and Stephanie Williams from the Department of Environment and Heritage. The audience was large and the topic was ‘hot’ and to be legislated in the South Australian ‘Climate Change and Greenhouse Emissions Reduction Bill 2006” found at www.climatechange.sa.gov.au. 

 

This ‘Climate Change and Greenhouse Emissions Reduction Bill 2006 to some extent defines the current state of climate warming and effects legislation to limit climate warming. Urgent measures are required to stop and hopefully reverse the effect of climate warming. However, the legislation fails to address two important issues, 1) it does not seek for the normalization of the atmosphere but only a 60% reduction of 1990 carbon dioxide levels by 2050, and 2) it does not have strong enough incentives for the reduction of emissions from industrial sources or from energy usage.

 

Marine conservationists should encourage the prevention of more climate warming.  The marine environment is highly vulnerable to the effects of climate warming. Predicted effects include sea level rises due to the melting of ice and the expansion of sea water as it warms. This will cause coastal erosion and the loss of remaining coastal estuaries and marshes. Lowered salinity and warming waters will effect oceanic currents and alter the climates of whole regions. Higher air temperatures will cause stratification of the water layers in shallow bays and estuaries thus increasing the chances of dinoflagellate blooms and red tides. Areas of seagrass and other marine species will die from heat stress.

 

In spite of these threats very little has been done to prevent the climate warming crisis and governments have only recently begin to mobilize on the issue. Several countries that are particularly dependent on the profligate use of energy have resisted global agreements to address climate change. Nevertheless, at a global scale evolving policies plan to turning climate change around, through reducing carbon dioxide and methane emissions, and through the fixing and storage of carbon. 

 

Even under the best current scenarios for the amelioration of climate warming the Earth will probably get hotter for fifty to one hundred years before beginning its cooling to normal. Carbon emissions can be reduced by using less carbon based fuels.  The best thing would be to immediately adapt the economy to accommodate only a net fixation of carbon. However, all industries are based on the use of carbon emitting fuel sources including coal, oil and gas. Therefore, the manufacture and maintenance of non-carbon fuel sources themselves result in the short term increase of carbon dioxide, including the mining and processing of ore to yield uranium for nuclear reactors. 

 

We still have some problems with technologies to ameliorate the crisis, but there are also opportunities for improved conservation outcomes. Carbon can be fixed by trees but this method of reducing atmospheric carbon dioxide is limited. As forests mature their net mass of carbon levels out and no more carbon can be absorbed. After this for increase in the amount of net fixed carbon more trees must be planted. The atmosphere already contains the carbon dioxide from previously cleared great forests, and the replanting of these forests is unlikely in the near future. However, there can be great advantages to conservation from the planting of carbon sinks besides carbon fixing. 

 

If areas of low conservation significance are chosen for planting the climate can be moderated by trees, valuable timber produced, and areas for wildlife and recreation provided. Plantation forests could have a certain percentage of their area reserved for wildlife and never harvested, with these areas of high diversity distributed along roads and in recreation areas. This type of habitat matrix could support a very high diversity of plants and animals including endangered species and take pressure of protected areas.

 

To supplement the fixation of carbon by new forests, and to speed up the progress of climate normalization carbon dioxide could fixed by physical or chemical processes. A possible physical process is the deposition of frozen carbon dioxide under the sea floor. Surprisingly, natural deposits of carbon dioxide on the seafloor could be subject to sublimation and then explode to the surface thus releasing carbon dioxide. A chemical process for the removal of carbon dioxide from the atmosphere is its absorption by seawater in the ocean. The absorption of carbon dioxide is already occurring to the extent that some seawater is becoming unsuitable for the maintenance of native life forms, and perhaps should not be relied on as a major carbon sink. 

 

Addressing the problems of global warming through the reduction of carbon dioxide emissions, and creating policies for abatement and adaptation to the effects of climate change on biodiversity were the main aims of the South Australian ‘Climate Change and Greenhouse Emissions Reduction Bill 2006’. At the heart of the legislation is a 60% reduction of the 1990 levels of greenhouse gas emission by 2050. 

 

One widely discussed problem with the ‘Climate Change and Greenhouse Emissions Reduction Bill 2006’ is that there appears to be little incentive for industry to engage in major programs for the reduction of carbon dioxide. The nature of ‘Sectorial Agreements’, a foundation of the policy, was widely discussed at the CCSA meeting. These ‘Sectorial Agreements’ agreements are between a greenhouse gas emitter and the State Government. They state a future emission target for the participant. The basis’ of a secular agreements are; 1) Government representatives and sectors would reach a target for reduced emission, 2) Four year report on progress, and a 3) Review option with prescriptive measures which would be performance based. The agreements can be with a person, industry, or business. The value of the agreements is that they define objectives, strategies, and methods. 

 

Questions are also raised as whether the legislation really addresses the state of the climate crisis. There appears to be an immediate need to stop the emission of carbon dioxide and reverse the past damage, and a target of 60% reduction in carbon dioxide emission over another four decades seems very conservative. For instance the present over usage of oil will prevent many current uses in the near future; the optimistic forecast is a decline to a crunch in less than two decades. Considering the potential costs of climate warming to both society and biodiversity a target of zero net greenhouse emission within a shorter period could be more practical. There is a need for a complete restructuring of the economy and industry to achieve this goal. For instance to reduce the problems of emissions from transport, legislation should encourage urban consolidation and increased use of public transport. Building designs can also be optimized for energy usage. 

 

What is really needed to address the issue of climate change is a major change in culture. The consumer society will have to change to a sustainable society. For to long have a small vested interest group profiting from increasing use of fossil fuels manipulated the world economy, politics, and society for their benefit. They have shown no regard for the destruction of public resources such as the atmosphere which is encouraged by their activities. Marine conservationists must support further efforts by the government to limit the negative ecological effects of these destructive industries and their associated cultures.

 

An important aspect of South Australia’s approach to climate change is the abatement of negative effects and the adapting of ecosystems to probable environmental changes. These include the identification of vulnerable biodiversity assets, building resilience in ecosystems, improving ecological function and connectivity, and protecting terrestrial and coastal habitats form anticipated changes. These goals are limited by a lack of practical information – particularly of vulnerable coastal environments. Besides encouraging the government to directly address the causes of global warming marine conservationists should also encourage projects who’s goal is increasing our knowledge of coastal biodiversity and the monitoring of the effects of climate change.

 

Nevertheless, in spite of the complexities of the issue, the enduring quality of the ‘Climate Change and Greenhouse Emissions Reduction Bill 2006’ will be as a foundation and stepping stone to a general acceptance and implementation of sustainable management. Although there is a clear need for more powerful legislation on climate change, South Australia is already providing a global leader in addressing the problems of climate change.

 

South Australia’s Jetties

by Steve Reynolds

What is a jetty? Where does the name “jetty” come from? Jetties are often called piers, in countries such as England for example. My old English encyclopaedia says that a jetty is “A pier or embankment used to direct or concentrate a current or to shelter a harbour”. This sounds like a breakwater to me.

My Australian Pocket Oxford Dictionary says that a pier is, amongst other things, a “structure running out into the sea and serving as promenade or landing-stage”. The same dictionary says that a jetty is a mole or landing pier (from the French word ‘jettee’). Henry Rymill agreed in 1994 that the word “jetty” is derived from the French word ‘jettee’ which, he said, meant ‘throw out’. My Hugo’s French-English Dictionary says that ‘jeter’ means to ‘throw’. The same dictionary says that ‘jettee’ means pier, jetty or mole.

So what is a mole? My Australian Pocket Oxford Dictionary says that a mole is, amongst other things, a “stone pier or breakwater or causeway” (just like I said about an English jetty or pier).

Michael Atchison’s “Word for Word” in The Advertiser of 10th March 2005 explains that large stone buildings were once described as a ‘pile’. That came from a 14th century word ‘pyle’ which meant ‘castle’ or ‘stronghold’. When we speak of a jetty in Australia we often refer to a wooden structure.

There are lots of jetties along SA’s coastline at present. Many of these are struggling to survive as they battle the elements. According to Ronald Parsons, in his book “Southern Passages” (Wakefield Press, 1998), the Government began to provide little ports with jetties as early as the 1850s. These ports quickly became a part of the transport network with the provision of a jetty. Eventually, most of the ports along the SA coast had jetties built by the Government. By 1910 SA had some 85 government-owned jetties and a few private ones. Many were later demolished when they were no longer required. Many others were broken up by storms.

When I started scuba diving, I became interested in the history of our jetties. I continually seek out snippets of information about them, even about those that no longer exist.

 

EDITHBURGH JETTY

Here’s an interesting thing, in my view. Edithburgh on the Yorke Peninsula has two jetties. The main jetty is situated at a spot called Point De Mole (or De Mole Point). When I read that Point De Mole had been chosen as the site to build a jetty I thought that there must be some kind of mistake. Since a mole is a jetty I thought that either the point was named after the jetty or after an earlier jetty built there. How wrong could I be? The book “South Australia – What’s in a Name?” by Rodney Cockburn says that there is a Point De Mole at Streaky Bay. Captain R Douglas, the Harbour-master, named the point after George E DeMole, a surveyor who accompanied him during his survey of the area in April 1858. DeMole drew the charts of Douglas’s survey. It seems that Point De Mole at Edithburgh is also named after the same surveyor. The booklet “Edithburgh Jetty 125th Anniversary”* by student Jarrod Thompson says that Point de Mole (sic) was named after a SA surveyor, presumably the same one that Streaky Bay’s Point De Mole was named after.

*Not the full title – it has also been called “History of Edithburgh Industry 1873-1998” but the full title appears to be “Souvenir of the Edithburgh Jetty 125th Anniversary 1873-1998 25th and 26th April 1998, History of Edithburgh Industry, Salt – Grain – Gypsum”.

Jarrod’s great, great-grandfather Jacob Staeben (Stehbens?) died at the jetty in 1891 when he was run over by one of the horse teams there. He was just 53 years old at the time of his death.

 

 

Edithburgh jetty in 1988 (Photo by Steve Reynolds)

The Edithburgh jetty was opened in January 1873. It was only 45m long initially but subsequent extensions made it some 175m long and 11.3m wide over some of its length. Edithburgh was declared a port on 15th September 1875. It was, however, closed as a port on 11th January 1973. The top decking of the jetty was covered in concrete in June 1996. As mentioned above, there are two jetties at Edithburgh. The second jetty there is located south of the boat ramp. It was built in the 1890s and it is known as the Fishermen’s Jetty.

 

RAPID BAY JETTY

A jetty was first built at Rapid Bay jetty on the Fleurieu Peninsula in 1867.That jetty was just 48m long. It was washed away during a storm in 1916. The present Rapid Bay jetty was built by BHP during WWII, between 1939 and March 1942. It was built to a length of 487.7m but its length is now officially just 420m (and it has a 224.5m long ‘T’ head at the end).

 

 

Steve Reynolds preparing to dive at Rapid Bay jetty (Photo by Peter Gower)

 

Adelaide Brighton Cement used the jetty for several years until 1998 when it was no longer needed by them. Demolition work was then done on the redundant ship-loading equipment. Within one year of the demolition work, the ‘dolphin’ platforms attached to the ‘T’ head were under threat. A ‘dolphin’, apart from being a friendly marine mammal, is a bollard or mooring post or buoy. There were plans to remove the dolphin platforms from the ‘T’ head for safety reasons. The Scuba Divers Federation of SA was assured that the jetty itself was in good shape and successfully fought for the dolphins to be retained. The jetty has since fallen into a state of disrepair and it was (mostly) closed on Christmas Eve in 2004. The future of the jetty is now uncertain. Diving at the jetty can now only be done by way of either a boat dive or a long swim from the rocky shore.

 

REFERENCES:

“Southern Passages” by Ronald Parsons (Wakefield Press, 1998)

The pamphlet “South Australia’s Yorke Peninsula, Unlocking the secrets – Historic jetties”.

 “Yorke Peninsula . . . A Resident’s Views” by Allan Parsons, second edition 1987, National Library of Australia ISBN 1 86252 059 2.

“A Story of Coobowie, Edithburgh and District” published by the Edithburgh Museum Committee, 1986.

 “South Australia – What’s in a Name? (Historically significant place names) by Rodney Cockburn, Axiom Publishing, 1999. ISBN 0 9592519 1 X.

“Souvenir of the Edithburgh Jetty 125th Anniversary 1873-1998 25th and 26th April 1998, History of Edithburgh Industry, Salt – Grain – Gypsum” by Jarrod Thompson, Edithburgh Museum, 1998. ISBN 0 646 35330 6.

“The Jetties of South Australia – Past and Present” by Neville Collins, published by the author, 2005. ISBN 0-9580482-2-3.

 

 

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