Sarcastic fringehead

The Sarcastic fringehead, Neoclinus blanchardi, is a ferocious fish which has a large mouth and aggressive territorial behavior from which it has been given its common name. When two fringeheads have a territorial battle, they wrestle by pressing their distended mouths against each other, as if they were kissing. This allows them to determine which is the larger fish, which establishes dominance.

They can be up to 30 centimeters (12 in) long, elongate and slender and are mostly scale less with great pectoral fins and reduced pelvic fins. They tend to hide inside shells or crevices. After the female spawns under a rock or in clam burrows the male guards the eggs.

They are found in the Pacific, off the coast of North America, from San Francisco, California, to central Baja California and their depth range is from 3 to 73 meters (9.8 to 240 ft).

Frizzle chickens

 

A Frizzle is a type of chicken with feathers that curl outwards, rather than lying flat as in most chickens. While many consider the Frizzle to be an entirely separate breed, it is not. Chickens from all breeds may have a frizzled appearance. It is a variety within breeds, some with clean legs and others with feathering on the legs.Genetically, the frizzled gene is a dominant trait. As a result of its unusual look, Frizzles are primarily exhibition birds, and are included in the Standard of Perfection.

Frizzle Chickens Background & Appearance.

The Frizzle is thought to have originated in Southern Asia around 300 years ago, but the history is a little sketchy as some Frizzles were documented to have been kept in Europe in the 17th century.

This breed of chicken is generally regarded as an exhibition breed, the bantam variety being much more popular than the larger type. In fact the larger bird was virtually extinct, until a group of breeders set up an intensive program to promote them, they are still considered rare today.

One look at a Frizzle Chicken and you’ll understand how it got it’s name, the strange feathering curls towards the head and is even and as tight as posible. Frizzles are full breasted and have short erect bodies. Large tails and long wings complete the picture.

Frizzles come in a range of colours, the commonest being white, black,blue, buff and silver-grey. Less common colours being columbian, black-red, duckwing, cuckoo, spangle, brown-red, pile and spangle.

Beak colour is denoted by the plumage colour, with some white and some yellow. The curly feathers also get a category either frizzled, over-frizzled or flat-coated.

Caring For Frizzle Chickens.

Frizzles are hardy birds, which develop quickly and can be left to free roam, but if you want to keep them in a run, then ensure you have a top on it or they may escape.

If you live in a particularly wet area, and get a lot of rain, then your frizzles should be kept indoors, as their feather formation doesn’t tolerate  particularly wet weather. You should also make sure your drinkers don’t allow the birds feathers to become wet, as the wet curly feathers become a magnet for dirt and shavings etc.

A great breed for keeping pet chickens, but if you have toddlers, don’t let them run around the pen or your chooks will become nervous.

If you are considering breeding Frizzle Chickens,  then introduce new strains to your girls, as breeding from the same strain year upon year will result in birds with weak and sparse feathers.

Newly hatched chicks appear to be normal feathered when they hatch, but don’t worry, the feathers soon start to grow and curl outwards.

Frizzle Chickens, Egg Laying & Broodiness.

It is worth mentioning at this point, that a lot of breeders and chicken fanciers, don’t recognise frizzles as a breed, (except in the UK where it is a show breed) but a feather type. Therefore a lot of crossbred frizzle strains abound. So dependant on where you get your birds, egg laying and egg colouration can differ quite a lot.

Generally true bred Frizzles lay quite well and produce a cream or tinted medium egg. If your ‘frizzles’ are cross bred with Cochins or Australorps for instance, then the egg laying/colour could follow those breeds. It’s best to check with the breeder you get your chicks or eggs from as to the exact strain.

 

20-Meter Sea Level Rise, Five Million Years Ago

July 21, 2013 — Global warming five million years ago may have caused parts of Antarctica's large ice sheets to melt and sea levels to rise by approximately 20 metres, scientists report today in the journal Nature Geoscience.
The researchers, from Imperial College London, and their academic partners studied mud samples to learn about ancient melting of the East Antarctic ice sheet. They discovered that melting took place repeatedly between five and three million years ago, during a geological period called Pliocene Epoch, which may have caused sea levels to rise approximately ten metres.
Scientists have previously known that the ice sheets of West Antarctica and Greenland partially melted around the same time. The team say that this may have caused sea levels to rise by a total of 20 metres.
The academics say understanding this glacial melting during the Pliocene Epoch may give us insights into how sea levels could rise as a consequence of current global warming. This is because the Pliocene Epoch had carbon dioxide concentrations similar to now and global temperatures comparable to those predicted for the end of this century.
Dr Tina Van De Flierdt, co-author from the Department of Earth Science and Engineering at Imperial College London, says: "The Pliocene Epoch had temperatures that were two or three degrees higher than today and similar atmospheric carbon dioxide levels to today. Our study underlines that these conditions have led to a large loss of ice and significant rises in global sea level in the past. Scientists predict that global temperatures of a similar level may be reached by the end of this century, so it is very important for us to understand what the possible consequences might be."
The East Antarctic ice sheet is the largest ice mass on Earth, roughly the size of Australia. The ice sheet has fluctuated in size since its formation 34 million years ago, but scientists have previously assumed that it had stabilised around 14 million years ago.
The team in today's study were able to determine that the ice sheet had partially melted during this "stable" period by analysing the chemical content of mud in sediments. These were drilled from depths of more than three kilometres below sea level off the coast of Antarctica.
Analysing the mud revealed a chemical fingerprint that enabled the team to trace where it came from on the continent. They discovered that the mud originated from rocks that are currently hidden under the ice sheet. The only way that significant amounts of this mud could have been deposited as sediment in the sea would be if the ice sheet had retreated inland and eroded these rocks, say the team.
The academics suggest that the melting of the ice sheet may have been caused in part by the fact that some of it rests in basins below sea level. This puts the ice in direct contact with seawater and when the ocean warms, as it did during the Pliocene, the ice sheet becomes vulnerable to melting.
Carys Cook, co-author and research postgraduate from the Grantham Institute for Climate Change at Imperial, adds: "Scientists previously considered the East Antarctic ice sheet to be more stable than the much smaller ice sheets in West Antarctica and Greenland, even though very few studies of East Antarctic ice sheet have been carried out. Our work now shows that the East Antarctic ice sheet has been much more sensitive to climate change in the past than previously realised. This finding is important for our understanding of what may happen to the Earth if we do not tackle the effects of climate change."
The next step will see the team analysing sediment samples to determine how quickly the East Antarctic ice sheet melted during the Pliocene. This information could be useful in the future for predicting how quickly the ice sheet could melt as a result of global warming.

 

Source:http://www.sciencedaily.com/releases/2013/07/130721161502.htm