Slider

Science

SCITECH

AMAZING FACTS

NATURE SPACE

Psychology

This dog is standing on thousands of frozen fish!

This dog is standing on thousands of frozen fish!

This dog is standing on thousands of frozen fish

It is assumed that the fish were frightened into shallow waters by whales and the water froze solid before the fish could escape. The local temperature was about -8 C (17 F). Though other fish have been chased into the bay by predators before, this is the first known occurrence of getting trapped in the ice.

As the ice thaws, the fish will probably be scavenged by birds.
Kosmo Elk in water - froze into ICE: This something special sight met Inger Sjøberg on Kosmo lake in Valnesfjord in Fauske municipality in Nordland last week.  - There has probably been a distressing death, she said.  - Photo: Private /
Froze into ICE: This something special sight met Inger Sjøberg on Kosmo lake in Valnesfjord in Fauske municipality in Nordland last week. - There has probably been a distressing death, she said.


Source

Worldwide Amphibian Declines: How big is the problem, what are the causes and what can be done?

Worldwide Amphibian Declines: How big is the problem, what are the causes and what can be done?

I. Introduction

Amphibians, a unique group of vertebrates containing > 7000 known species, are threatened worldwide. A recent assessment of the entire group (iucnredlist.org/amphibians) found that nearly one-third (32%) of the world’s amphibian species are threatened, representing 1,856 species. Amphibians have existed on earth for over 300 million years, yet in just the last two decades there have been an alarming number of extinctions, nearly 168 species are believed to have gone extinct and at least 2,469 (43%) more have populations that are declining. This indicates that the number of extinct and threatened species will probably continue to rise (Stuart et al. 2004).

Amphibian diversity is highest in the tropics and Brazil has the most described species at 932 species. By contrast, the United States is nearly the same size as Brazil but has 297 species (as of Feb 13, 2013).

Click on the image to see a larger version of this map.


II. Map of Global Declines

Declines have occured around the world, the areas that have suffered the most declines include Central America, the Caribbean, and Australia.
Click on the image to see a larger version of this map.



III. Why Are Amphibian Populations Declining?


Clearly, the most important factor leading to amphibian population declines is habitat destruction. When forests are cleared it is no surprise that species that once lived there disappear. What is alarming is that there are many cases where the habitat is protected and amphibians are still disappearing. The causes for recent amphibian declines are many, but an emerging disease called chytridiomycosis and global climate change are thought the be the biggest threats to amphibians. Chytridiomycosis is a disease caused by the fungal chytrid pathogen Batrachochytrium dendrobatidis. This pathogen is associated with the global loss of hundreds of species of amphibians and represents a spectacular loss of biodiversity, some say the worst in recorded history.
In the table below we break down all of the hypothesized factors and the links provide more detailed information for each one. Some factors are obviously shared with other types of endangered species on our planet and are part of to the worldwide biodiversity crisis such as habitat destruction, alteration and fragmentation (Fisher and Shaffer 1996, Davidson et al. 2001, Marsh and Trenham 2001), introduced species (Vredenburg 2004, Kats and Ferrer 2003) andover-exploitation (Jennings and Hayes 1985, Lannoo et al. 1994). For these threats, we have a pretty good understanding of the ecological mechanisms underlying declines (Collins and Storfer 2003). However, amphibians have also declined in relatively ‘pristine’ and protected environments (Wake 1991, Crump et al. 1992, Lips 2000). These more complex and elusive mechanisms include climate change (Pounds et al. 1999, Kiesecker et al. 2001, Carey and Alexander 2003), increased UV-B radiationchemical contaminants (Hayes et al. 2002, Blaustein et al. 2003), emerging infectious diseases (Daszak et al. 2003; see AmphibiaWeb's global distribution map of chytrid) and deformities (or malformations). The underlying mechanisms behind these factors are complex and they may be working synergistically with more straight forward factors, such as habitat destruction and introduced species, to exacerbate declines (Kiesecker et al. 2001, Blaustein and Kiesecker 2002). Researchers are finding that there is not a single overarching cause for global declines, instead all of these factors are threatening amphibian populations and the threat tends to vary depending on the location. If we are going to prevent further extinctions, research must move forward quickly and be used effectively in management by governments and non-governmental organizations around the world.


IV. Factors Involved in Amphibian Declines

Table 1. Probable and confirmed factors causing amphibian declines (modified from Table 1 in Young et al. 2001).
FACTORPROCESS(ES)
Habitat destruction, alteration and FragmentationRoads, introduced species, or other factors separate remaining populations of amphibians from each other.
Introduced SpeciesNon-native species prey on or compete with native amphibians.
Over-ExploitationAmphibians are removed form the wild and sold internationally as food, as pets, or for medicinal and biological supply markets
Climate ChangeAmphibians are extremely sensitive to small changes in temperature and moisture. Changes in global weather patterns (e.g. El Niño events or global warming) can alter breeding behavior, affect reproductive success, decrease immune functions and increase amphibian sensitivity to chemical contaminants.
UV-B RadiationLevels of UV-B radiation in the atmosphere have risen significantly over the past few decades. Researchers have found that UV-B radiation can kill amphibians directly, cause sublethal effects such as slowed growth rates and immune dysfunction, and work synergistically with contaminants, pathogens and climate change.
Chemical ContaminantsChemical stressors (e.g., pesticides, heavy metals, acidification and nitrogen based fertilizers) can have lethal, sublethal, direct or indirect effects on amphibians. These effects may include death, decreased growth rates, developmental and behavioral abnormalities, decreased reproductive success, weakened immune systems and/or hermaphroditism.
DiseaseNew diseases (such as chytridiomycosis) or higher susceptibility to existing diseases leads to deaths of adults and larvae.
DeformitiesThere has been a recent and widespread increase of deformities (or malformations) in natural populations of amphibians; this is now perceived as a major environmental problem.
SynergismsMultiple factors can act together to cause mortality or sublethal effects.


V. Possible Solutions: WHAT CAN BE DONE TO SAVE AMPHIBIANS?


The Global Amphibian Assessment has created an AMPHIBIAN ACTION CONSERVATION PLAN (pdf).

Table 2. Here are some other ways to reverse or ameliorate Amphibian Declines:
SOLUTIONPROCESS(ES)
Captive BreedingCaptive breeding progams for endangered species are being carried out in zoos.
ReintroductionsReintroduction programs place amphibians back into wild habitats in the hope that new populations can be established.
Non-native Species RemovalIntroduced species are being removed where they threaten native species.


VI. Literature Cited

Alford, R. A., and S. J. Richards. 1999. Global amphibian declines: A problem in applied ecology. Pages 133-165 in Annual Review of Ecology and Systematics. Annual Reviews, Palo Alto.
Blaustein, A. R., and J. M. Kiesecker. 2002. Complexity in conservation: Lessons from the global decline of amphibian populations. Ecology Letters 5:597-608.
Blaustein, A. R., J. M. Romansic, J. M. Kiesecker, and A. C. Hatch. 2003. Ultraviolet radiation, toxic chemicals and amphibian population declines. Diversity & Distributions [print] 9:123-140.
Blaustein, A. R., and D. B. Wake. 1990. Declining amphibian populations - a global phenomenon. Trends in Ecology & Evolution 5:203-204.
Carey, C., and M. A. Alexander. 2003. Climate change and amphibian declines: is there a link? Diversity and Distributions 9:111-121.
Collins, J. P., and A. Storfer. 2003. Global amphibian declines: Sorting the hypotheses. Diversity & Distributions [print] 9:89-98.
Crump, M. L., F. R. Hensley, and K. L. Clark. 1992. Apparent decline of the Golden Toad: underground or extinct? Copeia 1992:413-420.
Daszak, P., A. A. Cunningham, and A. D. Hyatt. 2003. Infectious disease and amphibian population declines. Diversity & Distributions [print] 9:141-150.
Davidson, C., H. B. Shaffer, and M. R. Jennings. 2001. Declines of the California red-legged frog: Climate, UV-B, habitat, and pesticides hypotheses. Ecological Applications 11:464-479.
Fisher, R. N., and H. B. Shaffer. 1996. The decline of amphibians in California's Great Central Valley. Conservation Biology 10:1387-1397.
Hayes, T. B., A. Collins, M. Lee, M. Mendoza, N. Noriega, A. A. Stuart, and A. Vonk. 2002. Hermaphroditic, demasculinized frogs after exposure to the herbicide atrazine at low ecologically relevant doses. Proceedings of the National Academy of Sciences of the United States of America 99:5476-5480.
Houlahan, J. E., C. S. Findlay, B. R. Schmidt, A. H. Meyer, and S. L. Kuzmin. 2000. Quantitative evidence for global amphibian population declines. Nature 404:752-755.
Jennings, M. R., and M. P. Hayes. 1985. Pre-1900 overharvest of California [USA] red-legged frogs (Rana aurora draytonii): The inducement for bullfrog (Rana catesbeiana) introduction. Herpetologica 41:94-103.
Kats, L. B., and R. P. Ferrer. 2003. Alien predators and amphibian declines: Review of two decades of science and the transition to conservation. Diversity & Distributions [print] 9:99-110.
Kiesecker, J. M., A. R. Blaustein, and L. K. Belden. 2001. Complex causes of amphibian population declines. Nature 410:681-684.
Lannoo, M. J., K. Lang, T. Waltz, and G. S. Phillips. 1994. An altered amphibian assemblage: Dickinson County, Iowa, 70 years after Frank Blanchard's survey. American Midland Naturalist 131:311-319.
Lips, K. R. 2000. Decline of a tropical amphibian fauna. in 166th National Meeting of the American Association for the Advancement of Science (AAAS) and Science Innovation Exposition., Washington, D.C., USA, February 17-22, 2000.
Marsh, D. M., and P. C. Trenham. 2001. Metapopulation dynamics and amphibian conservation. Conservation Biology 15:40-49.
Pounds, A., M. Fogden, and J. Campbell. 1999. Biological response to climate change on a tropical mountain. Nature 398:611-614.
Stuart, S., Chanson, J. S., Cox, N. A., Young, B. E., Rodrigues, A. S. L., Fishman, D. L. and Waller, R. W. 2004. Status and trends of amphibian declines and extinctions worldwide. - Science 306: 1783-1786.
Vredenburg, V. T. 2004. Reversing introduced species effects: Experimental removal of introduced fish leads to rapid recovery of declining frog. Proceedings of the National Academy of Sciences 101(20):7646-7650.
Wake, D. B. 1991. Declining amphibian populations. Science 253:860.
Young, B. E., K. R. Lips, J. K. Reaser, R. Ibanez, A. W. Salas, J. R. Cedeno, L. A. Coloma, S. Ron, E. La Marca, J. R. Meyer, A. Munoz, F. Bolanos, G. Chaves, and D. Romo. 2001. Population declines and priorities for amphibian conservation in Latin America. Conservation Biology 15:1213-1223.

Source

Literature citations edited by John Wilkinson (johnjwilkinson at hotmail), May 14, 2008.


VII. Recent Scientific Publications

AmphibiaWeb maintains a list of recent scientific publications on amphibian declines and amphibian conservation.This list is compiled and updated monthly by Professor Tim Halliday (formerly DAPTF International Director) (t.r.halliday@open.ac.uk).

Scientists discover giant trench under Antarctic Ice

A massive ancient subglacial trough – deeper than the Grand Canyon - has been discovered by a team of UK experts. The research involved scientists from Newcastle University, the University of Bristol's Glaciology Centre, the British Antarctic Survey and the universities of Edinburgh, Exeter, and York. They charted the Ellsworth Subglacial Highlands – an ancient mountain range buried beneath several kilometres of Antarctic ice - by combining data from satellites and ice-penetrating radars towed behind skidoos and on-board small aircraft.
Antarctica
Credit: Newcastle University
The researchers spent three seasons investigating and mapping the region in West Antarctica, uncovering a massive subglacial valley up to 3 kilometres deep, more than 300 kilometres long and up to 25 kilometres across. In places, the floor of this valley is more than 2000 metres below sea level.
The  and deep valley were carved millions of years ago by a small icefield similar to those of the present-day Antarctic Peninsula, or those of Arctic Canada and Alaska.
Professor Martin Siegert, Professor of Geosciences at the University of Bristol, said: "While the idea of West Antarctic Ice Sheet growth and decay over the past few million years has been discussed for decades, the precise location where the ice sheet may originate from in growth phases, and decay back to in periods of decay, has not been known.
"By looking at the topography beneath the ice sheet using a combination of ice-penetrating radio-echo sounding and satellite imagery, we have revealed a region which possesses classic glacial geomorphic landforms, such as u-shaped valleys and cirques, that could only have been formed by a small ice cap, similar to those seen at present in the Canadian and Russian High Arctic. The region uncovered is, therefore, the site of ice sheet genesis in West Antarctica."
The team's analysis has provided an unprecedented insight into the extent, thickness and behaviour of this ancient icefield, and the configuration and behaviour of the early West Antarctic Ice Sheet. The subglacial landscape shows where and how the West Antarctic Ice Sheet originated and grew. It also provides important clues about the size and shape of the  in West Antarctica in a warmer global climate.
The findings are published in the latest edition of the Geological Society of America Bulletin. The paper's lead author Dr Neil Ross, from Newcastle University, said: "The discovery of this huge trough, and the characterisation of the surrounding mountainous landscape, was incredibly serendipitous.
"We had acquired ice penetrating radar data from both ends of this huge hidden valley, but we had no information to tell us what was in between. Satellite data was used to fill the gap, because despite being covered beneath several kilometres of ice, the valley is so vast that it can be seen from space.
"To me, this just goes to demonstrate how little we still know about the surface of our own planet. The discovery and exploration of hidden, previously-unknown landscapes is still possible and incredibly exciting, even now."
More information: Neil Ross, Tom A. Jordan, Robert G. Bingham, Hugh F.J. Corr, Fausto Ferraccioli, Anne Le Brocq, David M. Rippin, Andrew P. Wright, and Martin J. Siegert. "The Ellsworth Subglacial Highlands: Inception and retreat of the West Antarctic Ice Sheet." Geological Society of America Bulletin, January 2014, v. 126, no. 1-2, p. 3-15, first published on September 19, 2013, DOI: 10.1130/B30794.1

FACED WITH SEA ICE LOSS, EMPEROR PENGUINS ALTER BREEDING TACTICS

Emperor penguin

FACED WITH SEA ICE LOSS,
EMPEROR PENGUINS ALTER BREEDING TACTICS

Confronted with the loss of sea ice in some parts of Antarctica, four colonies of emperor penguins have come up with an innovative breeding strategy to adapt to their changing environment. Using satellite images, an international team of scientists tracked the four colonies from 2008 to 2012. In the first three years, the emperor penguins hatched and incubated eggs in their customary fashion — atop the sea ice that freezes during the Antarctic winter and spring. But in 2011 and 2012, sea ice did not form until a month after the breeding season began. As a result, the emperor penguins — the largest penguin species on earth — did something never before witnessed by scientists: They climbed up the nearly sheer walls of large, floating ice shelves — huge structures, often hundreds of square miles in extent, that flow from land-based glaciers into the sea. In the region of the four colonies, the ice shelf walls reach as high as 100 feet, researchers say. The scientists say the altered breeding behavior could demonstrate how ice-dependent emperor penguins may adapt to life in a warming world.
sea ice, is global warming real, effects of global warming, global warming myth, global warming news, rising sea levels, 
emperor penguin, emperor penguin facts, where do penguins live, pictures of penguins, facts about penguins, penguins,
emperor penguins, polar bears

Magnolia trees

japanese magnolia, magnolia flower, star magnolia, jane magnolia, sweetbay magnolia, magnolia virginiana,
royal star magnolia, magnolia jane, ann magnolia, magnolia soulangiana, magnolia flowers, elizabeth magnolia,
teddy bear magnolia trees,
Magnolias are prized worldwide for their flowers and forms. Growing as large shrubs or trees, they produce showy, fragrant flowers that are white, pink, red, purple or yellow. Some forms are evergreen with glossy and leathery leaves and some evergreen types have buds, stems and undersides of leaves that are covered with attractive gold to copper to brown felt-like hairs. There are more than 200 species of Magnolia native to temperate, subtropical and tropical areas of southeastern Asia, eastern North America, Central America, the Caribbean and parts of South America. Many are now grown worldwide because of their beautiful flowers, shape and form.
How do you know if a magnolia is right for you? Ask the following questions to help determine if you should consider a magnolia -- and if so, where best to plant it:

WHAT KIND OF WINTERS DO YOU HAVE? magnolia tree, trees, palm trees, star magnolia tree, plants, shrubs, 

dogwood shrub, fast growing trees, cherry blossom tree, cherry tree, forsythia, conifers, weeping willow, dogwood,
hydrangea, azaleas, viburnum, hibiscus, camellia, azalea
The easy way to answer this question is to figure out what “zone” you live in. The U.S. is divided into zones by the USDA depending on how cold the winters are. Similar hardiness zone maps are available for AustraliaCanadaChinaEurope, and Japan and many other regions are developing maps.
Magnolias are available for almost any climate, especially if you can provide protection from harsh conditions.

WHAT KIND OF LIGHT DOES YOUR GARDEN RECEIVE?

Magnolias prefer a spot in the garden that receives full sun to light shade. That said, if you live in a particularly warm or dry climate, your magnolia might benefit from a location shaded from the hot afternoon sun. If possible, avoid exposed, windy locations because strong winds can damage large flowers and the typically brittle branches.

WHAT KIND OF SOIL DO YOU HAVE?

Most magnolias grow best in moist, well-drained, slightly acid soils but neutral to slightly alkaline soils are also suitable for growth. Magnolias are adaptable to clay, loam or sand soils, but most grow poorly in wet or poorly drained soils. Well-established plants can be moderately drought tolerant.

WHICH MAGNOLIA IS RIGHT FOR YOU?

So many choices, too small a garden. When you start looking into magnolias, you will want one in every bed! Some magnolias are grown primarily for their flowers, usually in the form of a shrub or small tree. Other magnolias grow to be large shade trees, and yet others are used as evergreen shrubs, trees or hedges. Consult our Magnolia Cultivars Checklist for options and consider visiting one of the gardens listed on this map to get an idea for the kinds of magnolias that are likely to do well in your climate.

WHAT ARE SOME OF THE COMMON TYPES OF MAGNOLIA AVAILABLE AT LOCAL NURSERIES?

Star Magnolia: Those of you living in colder areas may already be familiar with Star Magnolia,Magnolia stellata. This magnolia is one of the best known species because it is very cold hardy (USDA Zones 4-8), widely adaptable and blooms when very small. Star Magnolia is a slow growing, broad spreading, small tree or large shrub, ultimately reaching 15 feet tall or more. Leaves may be 4-8 inches long and up to 3 inches wide. As a deciduous plant, the dark green leaves drop in fall, sometimes turning yellow before falling.
Star Magnolia flowers are 3 to 5 inches in diameter with 12 to 40 petal-like parts called "tepals." The overall effect of the tepals is that of a starburst, hence the name, "Star Magnolia." Flowers are white, although a few cultivars have pinkish flowers. Star Magnolia's characteristics have made it popular as a parent of many hybrids.
Saucer Magnolia: Saucer and other large-flowered hybrid magnolias are deciduous trees known for their spectacular display of flowers appearing before the foliage in late winter and early spring. They are considered some of our most beautiful flowering trees, and some cultivars are hardy into USDA Zone 4 while others are adaptable in warmer Zone 9. These deciduous flowering magnolias generally are considered small trees with slow to moderate growth rates. Smaller cultivars may be grown as large shrubs and some larger trees may eventually grow 40 to 70 feet tall. Tree shape characteristically is upright to rounded when young and becoming rounded or broad-spreading with age. The medium green leaves are oval to circular in shape and vary in size from 3 to 10 inches long and 2 to 10 inches wide. Leaves turn a nondescript yellow to brown before dropping in fall. The trunk has smooth, tan or grey bark and branches exhibit large, fuzzy flower buds.
The fragrant flowers open before the foliage and range in color from white to pink to purple. Often flowers display one color on the outer side of the tepal and a lighter color inside. Many different cultivars or varieties have been selected over the years. Characteristics vary with the cultivar but flowers range from 3 to 12 inches in diameter. Peak bloom usually occurs in early spring; because of this, flowers are sometimes damaged by frosts. Some cultivars produce flowers sporadically through the summer and fall. Reddish fruits sometimes develop in the fall.
Southern Magnolia: Residents of warm temperate climates (USDA Zones 7-9) may be familiar with the Southern Magnolia. This native of southeastern North America was first introduced to Europe in 1731, and quickly became popular because of its glossy evergreen foliage, large beautiful flowers and elegant form. Growing as a small to large evergreen tree, Southern Magnolia also was found to be widely adaptable to different climates, soils, and exposures. Thus, it was the first Magnolia to be planted widely as a street or shade tree and is now grown nearly worldwide wherever suitable climate and soils exist.
Southern Magnolia has glossy, leathery, evergreen, oval-shaped leaves that are 5 to 8 inches or more long and half as wide. The upper leaf surface is dark green and the lower surface is often covered by brown, dense, felt-like hairs. The fragrant white flowers are 8 inches in diameter, appearing in late spring and intermittently throughout the summer. The flowers are followed by reddish, 3- to 5-inch long, oblong-shaped fruits displaying red seeds ripening in late fall. This species is extremely variable in size, shape, habit, growth rate, canopy density, leaf color, and flowering season. This variability has allowed a large number of beautiful cultivars to be selected.
Southern Magnolia is used as a specimen plant, street tree, shade tree, screen or windbreak. This tree also can be grown as an espalier.
Champaca Magnolia: Many magnolias grow in subtropical and tropical climates typical of USDA Zones 10-12 and warmer. Champaca Magnolia is a native of southeastern Asia famous for its extremely fragrant creamy-white, yellow or yellow-orange flowers. The small flowers are produced in large numbers because they form all along the branches and not just at the stem tips as with many other magnolias. Champaca blooms from spring through summer and sporadically flowers in winter. Its fragrance is so beautiful and powerful, it is used to make perfumes.
Champaca Magnolia is often grown in humid subtropical and tropical areas because it is valued for its form as an evergreen tree as well as its floral fragrance. Champaca Magnolia's typical size in the landscape is 30 feet tall and wide, though this tree may grow much larger with time.
Many new magnolias have been discovered in tropical areas of Asia and South America, and these may become more available in the future.

WHAT TIME OF YEAR SHOULD YOU PLANT A MAGNOLIA?

Deciduous magnolias (those that drop their leaves in fall) are best planted when dormant, typically in late fall or winter in warmer climates and early spring in cold climates. Evergreen magnolias are best planted in early spring. For the first 6 to 12 months after planting, both types will benefit from mulch and regular irrigation during warm or dry weather.

WHERE TO GO TO BUY MY MAGNOLIA?

Check with your local retail nursery or garden center. They may know which magnolias grow well in your area and will have these for sale. You may need to look for specialty, rare or new magnolias at "better" garden centers or from an online magnolia nursery. Consult our list of magnolia nurseries for suppliers specializing in this family.

WHAT SHOULD YOU LOOK FOR WHEN SELECTING A MAGNOLIA?

Look for healthy magnolias with evenly spaced branches. A container-grown plant can be slipped out of its pot to inspect the roots. Healthy roots are white, whereas diseased roots are brown to black and often have a sour odor.
Avoid plants with:
  • spotted, discolored or distorted leaves
  • discolored stems
  • broken branches
  • crossing and rubbing branches
  • wounds on the main trunk(s)
  • discolored roots
  • swollen areas on stems or roots (however, note that grafted or budded plants sometimes have swollen areas where the bud or graft was attached; check with nursery personnel to determine if this is the case)
  • many circling roots just inside of the container indicating the plant may be rootbound, making the plant more difficult to establish and often resulting in poor long-term growth and survival.

Top