“Based on the numbers that have been reported, the population seems to be pretty healthy,” Collins says. “I do not think this is something that people should be overly alarmed about,” he adds. “They are not large. Their bell is only about a centimeter. There aren’t any reports of them causing bad stings to swimmers, but the venom has not been specifically studied.”

Image right: The box jellyfish Tripedalia cystophora. (Photo by Jan Bielecki)

With the gradual warming of the oceans a number of marine species from the Caribbean have been observed moving into areas of the southern and mid-Atlantic coasts of the United States. “We’re seeing this happening everywhere all over the planet. Species ranges are changing because of human activities,” Collins says. “In general, it’s another symptom of a changing world.”

Image right: Diagram of a box jellyfish from the paper “First report of the box jellyfish Tripekalia cystophora (Cubozoa: Tripedaliidae) in the continental USA, from Lake Wyman, Boca Radon, Florida” by Evan Orellana and Allen Collins.

Tripedalia cystophora has taken up residence in southern Florida’s red mangroves, which is “a really good habitat for larval fishes,” Collins explains. “So, they could be competing with larval fishes for food, or if the fish larvae are small enough, perhaps even eating them, but they specialize on copepods. This box jellyfish is probably here for good.”

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Moray eel. Moray eels are legendary predators on coral reefs. Note the second set of jaws in the “throat”; these are the gill arches, which are present in all fish. Gill arches support the gills, the major respiratory organ of fish.

Lookdown. Because of its sloped head and the enlarged crest on its skull, the Lookdown appears to “look down” as it swims. These fish often swim in small schools.

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Alligator Pipefish. Pipefish may be thought of as seahorses unfurled. The numerous bony body rings are used to differentiate one species of pipefish from another.

Ox-eyed Oreo. The name Oreosoma (“mountain body”) refers to the cone-shaped bony structures on the underside of this larval specimen. Adults are more elongate, less oval, and covered with scales.

Dhiho’s Seahorse. Just over one inch long, this elegant fish is readily identified as a seahorse by its characteristic head. The body ends in a tail that can curl around and hold on to algae or coral. This species is found only in the waters around Japan.

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Across the Atlantic Ice boldly challenges this old narrative and presents overwhelming evidence for a pre-Clovis occupation of the American continents, and finds virtually no direct evidence that the progenitors of Clovis came from Siberia. Evidence put forth in this new book overwhelmingly indicates southwestern Europe, specifically the Ice Age Solutrean Culture of France and Spain, as the source of the people that developed into the Clovis.

Drawing from original archaeological analysis, paleoclimatic research, and genetic studies, noted archaeologists Dennis J. Stanford, of the Smithsonian’s National Museum of Natural History, and Bruce A. Bradley, associate professor at the University of Exeter, United Kingdom, apply rigorous scholarship to a hypothesis that places the technological antecedents of Clovis in Europe. Their research indicates that the first Americans crossed the Atlantic by boat and arrived earlier than previously thought.

Supplying archaeological and oceanographic evidence to support these assertions, the book dismantles the old paradigms while persuasively linking Clovis technology with the culture of the Solutrean people who occupied France and Spain more than 20,000 years ago.

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Hagfishes, known as slime eels or slime hags, are so named because of the huge amounts of mucus they produce. One disturbed hagfish can fill a 2-gallon bucket with slime in a matter of minutes. The slime makes them virtually inedible.

2

The eyes of the Four-eyed Fish are split in half horizontally, each having two pupils and a retina that is divided into top and bottom sections. It swims with half of its eye out of the water, searching for insects, and the other half looking down into the water.

3

African lungfish enclose themselves in a mud tunnel and, after their lake has dried up, can live for years buried in the mud, breathing air and waiting for the rains to return. The structure of their heart and lungs first tricked scientists into thinking the South American lungfish was a reptile, the African lungfish an amphibian.

4

Anemone fishes live in groups where the two largest fish only are sexually mature, the largest being female and the next largest male. If the female dies, the male changes sex to female and the next largest fish in the group matures to male. If the animated film “Finding Nemo,” had been true to life, Nemo’s dad, Marlin, should have become Nemo’s mother shortly after his original mother was eaten by a barracuda.

5

A few fishes specialize on, or at least supplement their diets with, the eyes of other fishes. A narrow-bodied cichlid in Africa’s Lake Malawi, the Malawi Eyebiter, does not make a good aquarium pet because of its eye-popping activities.

6

Peters Elephantfish is the only fish ever observed playing with objects. In captivity, these fish will repeatedly take a small ball of aluminum foil and carry it to the outflow tube of an aquarium filter so the ball is pushed across the tank by the water current.

7

Most fish are countershaded: darker on top, gradually lighter or silver on their sides and brightest on their bellies. Seen from above, beside or below, this pattern makes them less visible in the water column against the background color of the water.

8

The cusk eels are the world’s deepest living family of fishes. One was netted with a bottom trawl in the Puerto Rico Trench at a depth of 27,500 feet. At such a depth a fish would experience a pressure of  approximately 12,000 pounds per square inch.

9

As they sleep (and fish do sleep), parrotfishes and wrasses secrete a mucous cocoon around themselves at night, perhaps to thwart the highly-developed senses of moray eels and blood-sucking parasitic invertebrates.

10

Menhaden, the fishes the Indians taught the Pilgrims to plant with their corn, today rank as America’s most important fishes. Menhaden oil is used in cosmetics, linoleum, health food supplements, margarine, soap, insecticides and paints. Their pulverized bodies end up as feed for cats, dogs, poultry and pigs.

All fish facts are from the new book Fishes: The Animal Answer Guide, by Bruce Collette, National Systematics Laboratory,  Smithsonian’s National Museum of Natural History; and Gene Helfman, University of Georgia.

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Image right: The hand print of a baby dinosaur from the nesting site in South Africa. (Images courtesy University of the Witwatersrand)

A new study, entitled Oldest known dinosaur nesting site and reproductive biology of the Early Jurassic sauropodomorph Massospondylus and published in the international journal Proceedings of the National Academy of Sciences, was led by Canadian palaeontologist Robert Reisz, a professor of biology at the University of Toronto at Mississauga, and co-authored by Hans-Dieter Sues of the Smithsonian’s National Museum of Natural History; Eric Roberts of James Cook University, Australia; and Adam Yates of the Bernard Price Institute for Paleontological Research.

The study reveals clutches of eggs, many with embryos, as well as tiny dinosaur footprints, providing the oldest known evidence that the hatchlings remained at the nesting site long enough to at least double in size.

The authors say the newly unearthed dinosaur nesting ground is more than 100 million years older than previously known nesting sites.

Image left: A fossil from the nesting site showing seven eggs, some with the embryos exposed.

At least 10 nests have been discovered at several levels at this site, each with up to 34 round eggs in tightly clustered clutches. The distribution of the nests in the sediments indicate that these early dinosaurs returned repeatedly (nesting site fidelity) to this site, and likely assembled in groups (colonial nesting) to lay their eggs, the oldest known evidence of such behavior in the fossil record.

The large size of the mother, at six meters in length, the small size of the eggs, about six to seven centimetrs in diameter, and the highly organized nature of the nest, suggest that the mother may have arranged them carefully after she laid them.

“The eggs, embryos, and nests come from the rocks of a nearly vertical road cut only 25 meters long,” Reisz says. “Even so, we found ten nests, suggesting that there are a lot more nests in the cliff, still covered by tons of rock. We predict that many more nests will be eroded out in time, as natural weathering processes continue.”

Image right: A nest of dinosaur eggs from the South African nesting site.

The fossils were found in sedimentary rocks from the Early Jurassic Period in the Golden Gate Highlands National Park in South Africa. This site has previously yielded the oldest known embryos belonging to Massospondylus, a relative of the giant, long-necked sauropods of the Jurassic and Cretaceous periods.

“This amazing series of 190 million year old nests gives us the first detailed look at dinosaur reproduction early in their evolutionary history, and documents the antiquity of nesting strategies that are only known much later in the dinosaur record,” says Evans.

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Roughly 10 percent of all plant species are orchids, making them the largest plant family on Earth. But habitat loss has rendered many threatened or endangered. This is partly due to their intimate relationship with the soil. Orchids depend entirely on microscopic fungi in the early stages of their lives. Without the nutrients orchids obtain by digesting these host fungi, their seeds often will not germinate and baby orchids will not grow. While researchers have known about the orchid-fungus relationship for years, very little is known about what the fungi need to survive.

Image right and below: Flowers (right) and leaves (below) of the orchid Goodyera pubescens, commonly known as the downy rattlesnake orchid, endangered in Florida. (Photos by Melissa McCormick/SERC)

Biologists based at the Smithsonian Environmental Research Center in Edgewater, Md., launched the first study to find out what helps the fungi flourish and what that means for orchids. Led by Melissa McCormick, the researchers looked at three orchid species, all endangered in one or more U.S. states. After planting orchid seeds in dozens of experimental plots, they also added particular host fungi needed by each orchid to half of the plots. Then they followed the fate of the orchids and fungi in six study sites: three in younger forests (50 to 70 years old) and three in older forests (120 to 150 years old).

Image right and below: Leaf (right)  and flowers (below) of Tipularia discolor, the cranefly orchid, endangered in New York and Massachusetts, and threatened in Michigan and Florida.

After four years they discovered orchid seeds germinated only where the fungi they needed were abundant—not merely present. In the case of one species, Liparis liliifolia (lily-leaved twayblade), seeds germinated only in plots where the team had added fungi. This suggests that this particular orchid could survive in many places, but the fungi they need do not exist in most areas of the forest.

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Image right: These ancient corn cobs date roughly from 6,500-4,000 years ago. A is Proto-Confite Morocho race; B, Confite Chavinense maize race; and C is Proto-Alazan maize race.. (Photo by Tom Dillehay)

Some of the oldest known corncobs, husks, stalks and tassels, dating from 6,700 to 3,000 years ago were found at Paredones and Huaca Prieta, two mound sites on Peru’s arid northern coast. The research group, led by Tom Dillehay from Vanderbilt University and Duccio Bonavia from Peru’s Academia Nacional de la Historia, also found corn microfossils: starch grains and phytoliths. Characteristics of the cobs—the earliest ever discovered in South America—indicate that the sites’ ancient inhabitants ate corn several ways, including popcorn and flour corn. However, corn was still not an important part of their diet.

Image left: Wild forms of Zea mays are called ‘teosinte’. Over time, selective breeding modifies teosinte’s few fruitcases (left) into modern corn’s rows of exposed kernels (right). (Photo courtesy John Doebley.).

“Corn was first domesticated in Mexico nearly 9,000 years ago from a wild grass called teosinte,” Piperno says. “Our results show that only a few thousand years later corn arrived in South America where its evolution into different varieties that are now common in the Andean region began. This evidence further indicates that in many areas corn arrived before pots did and that early experimentation with corn as a food was not dependent on the presence of pottery.”

Understanding the subtle transformations in the characteristics of cobs and kernels that led to the hundreds of maize races known today, as well as where and when each of them developed, is a challenge. Corncobs and kernels were not well preserved in the humid tropical forests between Central and South America, including Panama—the primary dispersal routes for the crop after it first left Mexico about 8,000 years ago.

“These new and unique races of corn may have developed quickly in South America, where there was no chance that they would continue to be pollinated by wild teosinte,” Piperno says. “Because there is so little data available from other places for this time period, the wealth of morphological information about the cobs and other corn remains at this early date is very important for understanding how corn became the crop we know today.”

“Preceramic corn from Pardones and Huaca Prieta, Peru,” Grobman, A., Bonavia, D., Dillehay, T.D., Piperno, D.R., Iriarte, J., Holst, I. 2012. . PNAS early online edition, week of Jan. 16, 2012.

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Image left: A desert tortoise, Gopherus agassizii. (Image by Mike Jones, courtesy Encyclopedia of Life)

“Roads are barriers to dispersal for lots of species and usually it takes many generations to show up in the genetic structure of an animal,” says one of the paper’s co-authors Emily Latch, a postdoctoral researcher at the Smithsonian Conservation Biology Institute’s Center for Conservation and Evolutionary Genetics, and now an assistant professor at the University of Wisconsin-Milwaukee. “Because tortoises have such a long life span, we didn’t think the roads would influence their genetic structure so quickly, but they did.”

The study shows for the first time that recent landscape features such as roads “can have rapid effects on the genetic structure of a localized population and are detectible almost immediately,” in as little as one generation, the scientists report. As a result, the scientists conclude, “Roads may become increasingly important in shaping the evolutionary trajectory of desert tortoise populations.”

For the study, DNA samples were taken from 859 tortoises living in an area of 23,969 acres. “A huge number of samples,” for such a small area, Latch says. Data also was taken on each animal’s sex, location, and location elevation and slope.

Image right: A tortoise in the Mojave Desert. (Image courtesy Wikipedia)

The tortoises were sampled as part of a tortoise relocation effort at Fort Irwin Army Training Center and the animals were located by having people walk map transects in the desert. They picked-up, labeled and took data and DNA samples for every tortoise encountered.

“The adult individuals were initially genotyped to develop a baseline genetic database of translocated and resident tortoises so that family groups hatched after the translocations could be identified to particular parents, and the reproductive success of translocated and resident tortoises compared,” says Smithsonian geneticist Rob Fleischer, head of the Center for Conservation and Evolutionary Genetics and senior author on the paper. “This is important to determine if translocation is really an effective mitigation step. It was serendipity that led to our finding a surprising level of genetic structure.”

Roads may inhibit gene flow in desert tortoises by the reptiles being hit by cars, picked up by travelers, and predation and disease associated with pets released by the roadside. Eroded banks and increased vegetation along desert roads also may provide places for the tortoises to burrow and forage for food, causing them to move along a road rather than to cross it.

The article “Fine-Scale Analysis Reveals Cryptic Landscape Genetic Structure in Desert Tortoises,” by Emily K. Latch, William I. Boarman, Andrew Walde, and Robert C. Fleischer appeared recently in the journal PLoS ONE.

-John Barrat

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Image right: This NASA satellite image, acquired Jan. 7, 2012, shows the recent eruption in the Red Sea that has risen completely above water. Click image to enlarge.

Q: Geologically what is going on in these photographs?

A: The new island visible in the satellite photograph is the top of a giant shield volcano located on the rift axis in the Red Sea where the continental plates of Africa and Arabia are pulling apart. As these massive continental plates pull apart volcanic magma forcibly pushes its way up through the fissure and into the Red Sea. This new island emerged above water atop the shield volcano in a cluster of 10 islands called the Zubair Group. Each island represents a different vent area of the volcano and each one, during thousands of years, has been built up from the shield’s summit area, some 325 feet below sea level.

This video shows the new island erupting in the Red Sea.

The “new” volcano, of which you can see the very top, has probably been erupting episodically underwater for thousands of years. While its above-surface dimensions are roughly 1,739 feet east-to-west and 2,329 feet north-to-south we know the larger submerged shield it sits on is about 12.5 miles across—an edifice whose age is unknown, but the Red Sea may have begun spreading apart about 34 million years ago and the shield volcano could thus be tens of millions of years in the making.

Now that this recently active vent has emerged from the sea to make dry land, the eruption has excited media interest and people have begun to hear about it.

Image right: Satellite images showing the Red Sea region where the volcanic island recently appeared before (top) and after.

Q: What are the dangers of being near this newly forming island?

A: It is not implausible that the edifice could fail and cause a tsunami. The aviation community hasn’t reported big plumes of smoke and ash and the maritime community hasn’t reported a lot of floating pumice. The likelihood is that this eruption is kind of local, not too energetic and of little hazard to marine navigation. Lava is probably being spattered at 164 to 325 feet. Most of its activity has been hidden underwater. Now that it has switched from a submarine eruption to an above water eruption, its style of erupting may change….perhaps to some beautiful spray eruptions.

Keep in mind that this whole region has had many volcanic eruptions in the last five years. In 2007, for example, a sudden eruption on the nearby Island Jebel at Tair killed a number of soldiers stationed there. The process of plate tectonics seems to be going on a little faster, at a quickened rate in this area. Why? We don’t know. The general public needs to be reminded that volcanologists are often in the dark about these processes.

Q: What can we expect to see in the next few months from this volcanic island?

A: The supply of magma supplied by the rift axis seems to be a stop-and-go process and repose of these volcanoes is a lot longer than their eruptive phase. Often in the case of submarine volcanoes they wash away in about a year from ocean currents, wind and storms. Also volcanic islands often sink due to a process we don’t understand very well. A lot of volcanoes on the sea floor are flat topped—as they were sinking, it is as if the waves chopped off their tops–gave them a haircut. So this may happen as well.

Other islands in the group clearly have explosion craters of various sizes so it’s possible that before any sinking or washing away occurs, we could see more energetic explosions. Today’s activity may be as energetic as it will get or it may transition to more effusive behavior as the vent is further sheltered from the sea surface.

There’s a lot more up and down to these submarine volcanoes than meets the eye. They may have quite enigmatic lava flows of 70 to 100 miles but the flows are spread out and over time they built up like a stack of pancakes. They are not formed in a central mound like inland volcanoes are.

(Richard Wunderman is managing editor of the Bulletin of the Global Volcanism Network. To read a just-published report on this new volcanic eruption click this link to the Global Volcanism Program Volcanic Activity Reports and click PDF File.)

Satellite images originally published by NASA Earth Observatory.

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The image shows one of the most active and turbulent regions of star birth in our galaxy, a region called Cygnus X. The choppy cloud of gas and dust lies 4,500 light-years away in the constellation Cygnus the Swan.

Image right: The Cygnus-X star-forming region is located 4,600 light-years from Earth and spans more than 600 light-years. This infrared photograph from the Spitzer Space Telescope reveals more than a thousand protostars in the earliest stages of forming. Light of 3.6 microns is color-coded blue: 4.5-micron light is blue-green; 8.0-micron light is green; and 24-micron light is red.

Cygnus X, which spans an area of the sky larger than 100 full moons, is home to thousands of massive stars, and many more stars around the size of our sun or smaller. Spitzer has captured an infrared view of the entire region, which is bubbling with star formation.

“Spitzer captured the range of activities happening in this violent cloud of stellar birth,” said Joe Hora of the Harvard-Smithsonian Center for Astrophysics, who is the principal investigator of the research. “We see bubbles carved out from massive stars, pillars of new stars, dark filaments lined with stellar embryos and more.”

The majority of stars are thought to form in huge star-forming regions like Cygnus X. Over time, the stars dissipate and migrate away from each other. It’s possible that our sun was once packed tightly together with other, more massive stars in a similarly chaotic, though less extreme, region.

The turbulent star-forming clouds are marked with bubbles, or cavities, which are carved out by radiation and winds from the most massive of stars. Those massive stars tear the cloud material to shreds, terminating the formation of some stars, while triggering the birth of others.

“One of the questions we want to answer is how such a violent process can lead to both the death and birth of new stars,” said Sean Carey, a team member from NASA’s Spitzer Science Center at the California Institute of Technology.

Infrared data from Spitzer is helping to answer questions like these by giving astronomers a window into the dustier parts of the complex. Infrared light travels through dust, whereas visible light is blocked. For example, embryonic stars blanketed by dust pop out in the Spitzer observations. In some cases the young stars are embedded in finger-shaped pillars of dust. In other cases, these stars can be seen lining very dark, snake-like filaments of thick dust.

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