WFS Dinofact: Eotyrannus

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Name:Eotyrannus (Greek for “dawn tyrant”); pronounced EE-oh-tih-RAN-us

Habitat:Woodlands of Western Europe

Historical Period:Early Cretaceous (125-120 million years ago)

Size and Weight:About 15 feet long and 300-500 pounds

Diet:Meat

Distinguishing Characteristics:Small size; relatively long arms with grasping hands

About Eotyrannus

The tiny tyrannosaur Eotyrannus lived during the early Cretaceous period, about 50 million years before more famous relatives like Tyrannosaurus Rex–and, following a common theme in evolution, this dinosaur was much smaller than its giant descendant (the same way the first, mouse-sized mammals of the Mesozoic Era were much smaller than the whales and elephants that evolved from them).

Eotyrannus (Greek for "dawn tyrant")

Eotyrannus (Greek for “dawn tyrant”)

 In fact, the 300- to 500-pound Eotyrannus was so slender and wiry, with relatively long arms and legs and grasping hands, that to the untrained eye it might look more like a raptor; the giveaway is the lack of single, giant claws on each of its hind feet, as sported by the likes of Velociraptor and Deinonychus. (One paleontologist speculates that Eoraptor was actually a non-tyrannosaur theropod closely related to Megaraptor, but this idea is still being digested by the scientific community.)

One of the most remarkable things about Eotyrannus is that its remains were discovered on England’s Isle of Wight–western Europe isn’t exactly famous for its tyrannosaurs! From an evolutionary point of view, however, this makes sense: we know that the earliest tyrannosaurs (like the 25-pound, feathered Dilong) lived a few million years before Eotyrannus in eastern Asia, while the largest tyrannosaurs (like the multi-ton T.

 Rex and Albertosaurus) were indigenous to late Cretaceous North America. One possible scenario is that the very first tyrannosaurs migrated west from Asia, quickly evolving to Eotyrannus-like sizes, and then reached the culmination of their development in North America. (A similar pattern held with horned, frilled dinosaurs, the tiny progenitors of which originated in Asia and then made their way westwards to North America, spawning multi-ton genera like Triceratops.)
Source:www.thoughtco.com
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WFS News: Como Bluff:The Dinosaur Graveyard

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Como Bluff is a long ridge with views of sagebrush prairie for as far as the eye can see. It extends roughly east-west, and is about 10 miles long and 1 mile wide. Geologically, the ridge is one limb of an anticline, formed as a result of the Earth compressing and folding, in association with larger geologic events caused by Rocky Mountain plate tectonics. The northern face of Como Bluff shows the outcrops of the Late Jurassic (145-150 million years ago) Morrison Formation. The Jurassic is a period in the Mesozoic Era (66 to 252 million years ago) better known as the “Age of the Dinosaurs.” At the start of the Jurassic Period, the breakup of Pangaea resulted in Laurasia to the north (which broke up into North America and Eurasia) and Gondwana to the south (which broke into Africa and South America). New oceans flooded the landmasses, with mountains rising on the seafloor, pushing sea levels higher onto the continents. All this water created a rather humid climate and lush subtropical environment, supporting a biologically diverse array of plants and animals. Cycads (palm tree-like foliage) covered the landscape, as well as conifers such as Araucaria and pines. The land was home to large terrestrial species, dinosaurs, with many of these predators at the top of the food chain.

Como Bluff from a distance.

Como Bluff from a distance.

Four types of sauropods were found at Como Bluff. These included the plant-eating Apatosaurus (the correct name for Brontosaurus), Diplodocus, at 90 feet long, Camarasaurus, and Barosaurus. Other large herbivores that inhabited the area during the late Jurassic period included the Stegosaurus (known for its heavy armor), and Camptosaurus, Laosaurus, and Dryosaurus. Carnivores included the Allosaurus, Ceratosaurus, and Ornitholestes.

Many dinosaurs roamed this region we now call Wyoming. Experts say it is a matter of time, place, and climate that prompted dinosaurs to live here. The diversity of plants provided for an abundance of herbivorous, plant-eating dinosaurs. This led to a corresponding abundance of carnivores, the meat-eating dinosaurs. Because so many dinosaur bones were found at Como Bluff, one might consider it the dinosaur capitol of the world, as the dinosaur records show. The discovery of their fossil remains were well preserved in the pastel colored claystones of the Morrison Formation at Como Bluff.

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WFS News:Tick with dinosaur blood found in amber fossil

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REAL LIFE JURASSIC PARK: Tick with dinosaur blood found in amber fossil

REAL LIFE JURASSIC PARK: Tick with dinosaur blood found in amber fossil

In a discovery which is eerily similar to the opening scenes of Jurassic Park, experts found the fossilised blood sucking parasite trapped in amber.

The insect is actually a newly discovered species of tick, which has been called Deinocroton draculi or “Dracula’s terrible tick”, and would have fed on the blood of dinosaurs 100 million years ago.

The tick-encased-amber was discovered on the inside of a tree, and also enclosed was a small feather – which began to evolve on dinosaurs before they eventually evolved into modern day birds.

The University of Oxford calls this the “first direct fossil evidence of ticks parasitising dinosaurs.”

The tick was encased in amber

                                                               The tick was encased in amber

Dr Ricardo Pérez-de la Fuente, a palaeobiologist at Oxford University Museum of Natural History and one of the authors of the study describing the parasites, said: “The fossil record tells us that feathers like the one we have studied were already present on a wide range of theropod dinosaurs.“Although we can’t be sure what kind of dinosaur the tick was feeding on, the mid-Cretaceous age of the Burmese amber confirms that the feather certainly did not belong to a modern bird.”The tick fed on dinosaur blood 100 million years ago                                                          The tick fed on dinosaur blood 100 million years ago

However, it is unlikely scientists will ever be able to know which dinosaur the blood came from.The discovery is also unlikely to lead to a Jurassic Park-style theme park where the ancient beasts roam freely, as scientists are still unable to withdraw DNA from specimens preserved in amber fossil.University of Barcelona researcher Dr Xavier Delclòs said: “Assessing the composition of the blood meal inside the bloated tick is not feasible because, unfortunately, the tick did not become fully immersed in resin and so its contents were altered by mineral deposition.”

Source: Article by Sean Martin, www.express.co.uk

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WFS News: Mongolian microfossils point to the rise of animals on Earth

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A Yale-led research team has discovered a cache of embryo-like microfossils in northern Mongolia that may shed light on questions about the long-ago shift from microbes to animals on Earth.

Called the Khesen Formation, the site is one of the most significant for early Earth fossils since the discovery of the Doushantuo Formation in southern China nearly 20 years ago. The Dousantuo Formation is 600 million years old; the Khesen Formation is younger, at about 540 million years old.

This is an image of assorted microfossils from the Ediacaran Khesen Formation, Mongolia. Each fossil is on the order of 200 microns maximum dimension. Credit: Yale University

This is an image of assorted microfossils from the Ediacaran Khesen Formation, Mongolia. Each fossil is on the order of 200 microns maximum dimension.Credit: Yale University

“Understanding how and when animals evolved has proved very difficult for paleontologists. The discovery of an exceptionally well-preserved fossil assemblage with animal embryo-like fossils gives us a new window onto a critical transition in life’s history,” said Yale graduate student Ross Anderson, first author of a study in the journal Geology.

The new cache of fossils represents eight genera and about 17 species, comprising tens to hundreds of individuals. Many of them are spiny microfossils called acritarchs, which are roughly 100 microns in size — about one-third the thickness of a fingernail.

The Khesen Formation is located to the west of Lake Khuvsgul in northern Mongolia. “This site was of particular interest to us because it had the right type of rocks — phosphorites — that had preserved similar organisms in China,” Anderson said.

The discovery may help scientists confirm a much earlier date for the existence of Earth ecosystems with animals, rather than just microbes. For two decades, researchers have debated the findings at the Doushantuo Formation, with no resolution. If confirmed as animals, these microfossils would represent the oldest animals to be preserved in the geological record.

The other authors of the study are Derek Briggs, Yale’s G. Evelyn Hutchinson Professor of Geology and Geophysics and curator at the Yale Peabody Museum of Natural History; Sean McMahon, a postdoctoral fellow in the Briggs lab; Francis Macdonald of Harvard; and David Jones of Amherst College.

The researchers said the Khesen Formation should provide scientists with additional information for years to come.

“This study is only the tip of the iceberg, as most of the fossils derive from only two samples,” Anderson said. Since the original discovery, the Yale team has worked with Harvard and the Mongolian University of Science and Technology to sample several additional sites within the formation.

  1. Ross P. Anderson, Francis A. Macdonald, David S. Jones, Sean McMahon, Derek E.G. Briggs. Doushantuo-type microfossils from latest Ediacaran phosphorites of northern Mongolia. Geology, 2017; DOI: 10.1130/G39576.1

Yale University. “Mongolian microfossils point to the rise of animals on Earth.” ScienceDaily

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WFS News: Ancient dolphin species Urkudelphis chawpipacha discovered.

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A new dolphin species likely from the Oligocene was discovered and described in Ecuador, according to a study published December 20, 2017 in the open-access journal PLOS ONE by Yoshihiro Tanaka from the Osaka Museum of Natural History, Japan, and colleagues.

Many marine fossils described in previous research have been from long-recognized temperate regions such as South Carolina, off the coast of Oregon, Hokkaido and New Zealand. Few equatorial and polar fossils are currently known.

Skull, Urkudelphis chawpipacha MO-1 (holotype) in right lateral view. Credit: Tanaka et al (2017)

Skull, Urkudelphis chawpipacha MO-1 (holotype) in right lateral view.Credit: Tanaka et al (2017)

While in the tropical region of Santa Elena Province, Ecuador, the authors of this study found a small dolphin skull, which they identified as representing a new species, Urkudelphis chawpipacha, based on facial features. The dolphin skull had a bone crest front and center on its face, above the eye sockets. This species stands apart from other Oligocene dolphins with its shorter and wider frontal bones located near the top of the head and the parallel-sided posterior part of its jaw. The authors also conducted a phylogenetic analysis which revealed that the new species may be the ancestor of the nearly-extinct Platanistoidea, or river dolphin, and may have lived during the Oligocene era.

The fossil is one of the few fossil dolphins from the equator, and is a reminder that Oligocene cetaceans may have ranged widely in tropical waters.

This study was supported by an UPSE project IN-P5-2016-1 for equipment at UPSE, and YT thanks support of a trip to Ecuador. This work has also been supported by the Agencia Estatal de Investigación (AEI) from Spain and the European Regional Development Fund of the European Union (CGL2016-76431-P) and the project CGL2015-68333 (MINECO/FEDER, UE).

  1. Yoshihiro Tanaka, Juan Abella, Gabriel Aguirre-Fernández, Maria Gregori, R. Ewan Fordyce. A new tropical Oligocene dolphin from Montañita/Olón, Santa Elena, Ecuador. PLOS ONE, 2017; 12 (12): e0188380 DOI: 10.1371/journal.pone.0188380
PLOS. “Ancient dolphin species Urkudelphis chawpipacha discovered in Ecuador: Small dolphin skull may have belonged to river dolphin ancestor from the Oligocene.” ScienceDaily. ScienceDaily, 22 December 2017. <www.sciencedaily.com/releases/2017/12/171222090340.htm>.
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WFS News: Habelia optata, A 508-million-year-old sea predator

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Paleontologists at the University of Toronto (U of T) and the Royal Ontario Museum (ROM) in Toronto have entirely revisited a tiny yet exceptionally fierce ancient sea creature called Habelia optata that has confounded scientists since it was first discovered more than a century ago.

General anatomy of Habelia optata, morphs A (d-g) and B (a-c, h). a ROMIP 64357. b USNM 139209 (inset is (h)). c ROMIP 64358. d ROMIP 64359. e Close-up of the mandibles on the counterpart of (d) (wet specimen). f Close-up of the distal telson piece in (g) (wet specimen). g Holotype USNM 57693 (inset is (f)). h Close-up on cephalic ornamentation akin to trilobite prosopon in (b). All pictures taken under cross-polarized light. For abbreviations, see Methods. Scale bars: (a), 4 mm; (b), 3 mm; (c, d, g), 2 mm; (e, f, h), 1 mm

General anatomy of Habelia optata, morphs A (d-g) and B (a-c, h). a ROMIP 64357. b USNM 139209 (inset is (h)). c ROMIP 64358. d ROMIP 64359. e Close-up of the mandibles on the counterpart of (d) (wet specimen). f Close-up of the distal telson piece in (g) (wet specimen). g Holotype USNM 57693 (inset is (f)). h Close-up on cephalic ornamentation akin to trilobite prosopon in (b). All pictures taken under cross-polarized light. For abbreviations, see Methods. Scale bars: (a), 4 mm; (b), 3 mm; (c, d, g), 2 mm; (e, f, h), 1 mm

The research by lead author Cédric Aria, recent graduate of the PhD program in the department of ecology & evolutionary biology in the Faculty of Arts & Science at U of T, and co-author Jean-Bernard Caron, senior curator of invertebrate palaeontology at the ROM and an associate professor in the departments of ecology & evolutionary biology and Earth sciences at U of T, is published today in BMC Evolutionary Biology.

Approximately 2 cm in length with a tail as long as the rest of its body, the long-extinct Habelia optata belongs to the group of invertebrate animals called arthropods, which also includes such familiar creatures as spiders, insects, lobsters and crabs. It lived during the middle Cambrian period approximately 508 million years ago and comes from the renowned Burgess Shale fossil deposit in British Columbia. Habelia optata was part of the “Cambrian explosion,” a period of rapid evolutionary change when most major animal groups first emerged in the fossil record.

Anatomical and morphological details of Habelia optata, morphs A (b, d, f, n) and B (a, e, g, i, l, m). a USNM 139209, close-up of anterior cephalic area, showing intermediary appendage. b USNM 268931, cephalon, showing superimposed insertion of endopods on gnathobases; star points to insertion of anterior endopods. c ROMIP 64357, close-up of fourth cephalic exopodial branch, distal portion showing slender podomeres; arrow points to trident of setae at podomere junction. d ROMIP 64358, close-up of anteriormost region, showing mouth opening and first anterior pairs of gnathobases. e ROMIP 64360, close-up of teeth on masticatory margin of gnathobase; note heavy concentration of carbon in teeth. f Close-up of teeth on masticatory margin of posterior gnathobase on same specimen as in D, showing stronger carbon content in dental edge. g ROMIP 64364, specimen preserved in ventral aspect, close-up of anterior region showing labrum, eyes and appendages; star marks attachment of fifth spinose endopod; arrow points at ornamental spine of cephalic pleura; insets as indicated. h ROMIP 64362, close-up of posterior trunk exopods. i ROMIP 64363, close-up of anterior right cephalic region, dorsal view showing labrum and appendages; arrows point to overprint of gnathobases underneath cephalon. j, k ROMIP 64364. j Close-up of distal portion of cephalic endopod, showing “platform” with setal brushes. k Close-up of terminal claw; arrows point to teeth on inner margin of claw. l USNM 144907, close-up of cephalic gnathobases; arrows point to dentate margins of opposing gnathobases. m ROMIP 64357, close-up on anterior left cephalic region, showing appendages; arrow points to anterior insertion of fourth cephalic endopod. n ROMIP 64359, close-up of cephalic appendages showing insertion of endopods on gnathobases; star marks attachment of fourth cephalic endopod on its gnathobase. c-f, j and k are SEM images; all other are stereomicroscope images of dry specimens under cross-polarized lighting. For abbreviations, see Methods. Scale bars: (a, g, h, i, l, n), 1 mm; (b, m), 0.5 mm; (c, d, k), 200 μm; (e), 100 μm; (f), 50 μm; (j), 500 μm

Anatomical and morphological details of Habelia optata, morphs A (b, d, f, n) and B (a, e, g, i, l, m). a USNM 139209, close-up of anterior cephalic area, showing intermediary appendage. b USNM 268931, cephalon, showing superimposed insertion of endopods on gnathobases; star points to insertion of anterior endopods. c ROMIP 64357, close-up of fourth cephalic exopodial branch, distal portion showing slender podomeres; arrow points to trident of setae at podomere junction. d ROMIP 64358, close-up of anteriormost region, showing mouth opening and first anterior pairs of gnathobases. e ROMIP 64360, close-up of teeth on masticatory margin of gnathobase; note heavy concentration of carbon in teeth. f Close-up of teeth on masticatory margin of posterior gnathobase on same specimen as in D, showing stronger carbon content in dental edge. g ROMIP 64364, specimen preserved in ventral aspect, close-up of anterior region showing labrum, eyes and appendages; star marks attachment of fifth spinose endopod; arrow points at ornamental spine of cephalic pleura; insets as indicated. h ROMIP 64362, close-up of posterior trunk exopods. i ROMIP 64363, close-up of anterior right cephalic region, dorsal view showing labrum and appendages; arrows point to overprint of gnathobases underneath cephalon. j, k ROMIP 64364. j Close-up of distal portion of cephalic endopod, showing “platform” with setal brushes. k Close-up of terminal claw; arrows point to teeth on inner margin of claw. l USNM 144907, close-up of cephalic gnathobases; arrows point to dentate margins of opposing gnathobases. m ROMIP 64357, close-up on anterior left cephalic region, showing appendages; arrow points to anterior insertion of fourth cephalic endopod. n ROMIP 64359, close-up of cephalic appendages showing insertion of endopods on gnathobases; star marks attachment of fourth cephalic endopod on its gnathobase. c-f, j and k are SEM images; all other are stereomicroscope images of dry specimens under cross-polarized lighting. For abbreviations, see Methods. Scale bars: (a, g, h, i, l, n), 1 mm; (b, m), 0.5 mm; (c, d, k), 200 μm; (e), 100 μm; (f), 50 μm; (j), 500 μm

Like all arthropods, Habelia optata features a segmented body with external skeleton and jointed limbs. What remained unclear for decades, however, was the main sub-group of arthropods to which Habelia belonged. Early studies had mentioned mandibulates — a hyperdiverse lineage whose members possess antennae and a pair of specialized appendages known as mandibles, usually used to grasp, squeeze and crush their food. But Habelia was later left as one of the typically unresolved arthropods of the Burgess Shale.

The new analysis by the U of T-ROM researchers suggests that Habelia optata was instead a close relative of the ancestor of all chelicerates, the other sub-group of arthropods living today, named for the presence of appendages called chelicerae in front of the mouth and used to cut food. This is mostly due to the overall anatomy of the head in Habelia, and the presence of two small chelicerae-like appendages revealed in these fossils.

Diagrammatic reconstruction of Habelia optata, morph A. a Ventral view of the cephalon. Right “intermediary” appendage removed to show gnathobase morphology. b Lateral view. c Dorsal view. d Isolated biramous thoracic limb in frontal, lateral and posterior views (left to right). For abbreviations, see Methods. Line drawings courtesy of Joanna Liang © Royal Ontario Museum

Diagrammatic reconstruction of Habelia optata, morph A. a Ventral view of the cephalon. Right “intermediary” appendage removed to show gnathobase morphology. b Lateral view. c Dorsal view. d Isolated biramous thoracic limb in frontal, lateral and posterior views (left to right). For abbreviations, see Methods. Line drawings courtesy of Joanna Liang © Royal Ontario Museum

Habelia now shows in great detail the body architecture from which chelicerates emerged, which allows us to solve some long-standing questions,” said Aria, who is now a post-doctoral researcher at the Nanjing Institute of Geology and Palaeontology, in China. “We can now explain why, for instance, horseshoe crabs have a reduced pair of limbs — the chilaria — at the back of their heads. Those are relics of fully-formed appendages, as chelicerates seem to originally have had heads with no less than seven pairs of limbs.”

Aria and Caron analyzed 41 specimens in total, the majority of which are new specimens acquired by ROM-led fieldwork parties to the Burgess Shale.

The research illustrates that the well-armoured body of Habelia optata, covered in a multitude of different spines, was divided into head, thorax and post-thorax, all bearing different types of appendages. The thorax displays five pairs of walking legs, while the post-thorax houses rounded appendages likely used in respiration.

Artistic reconstruction of Habelia optata. Courtesy of Joanna Liang © Royal Ontario Museum

Artistic reconstruction of Habelia optata. Courtesy of Joanna Liang © Royal Ontario Museum

“Scorpions and the now-extinct sea scorpions are also chelicerates with bodies divided into three distinct regions,” Aria explained. “We think that these regions broadly correspond to those of Habelia. But a major difference is that scorpions and sea scorpions, like all chelicerates, literally ‘walk on their heads,’ while Habelia still had walking appendages in its thorax.”

The researchers argue that this difference in anatomy allowed Habelia to evolve an especially complex head that makes this fossil species even more peculiar compared to known chelicerates. The head of Habelia contained a series of five appendages made of a large plate with teeth for mastication, a leg-like branch with stiff bristle-like spines for grasping, and an elongate, slender branch modified as a sensory or tactile appendage.

“This complex apparatus of appendages and jaws made Habelia an exceptionally fierce predator for its size,” said Aria. “It was likely both very mobile and efficient in tearing apart its preys.”

The surprising outcome of this study, despite the evolutionary relationship of Habelia with chelicerates, is that these unusual characteristics led instead the researchers to compare the head of Habelia with that of mandibulates from a functional perspective. Thus, the peculiar sensory branches may have been used in a similar fashion as mandibulates use antennae. Also, the overlapping plate-like appendages in the middle series of five are shown to open and close parallel to the underside of the head — much as they do in mandibulates, especially those that feed on animals with hardened carapaces.

Lastly, a seventh pair of appendages at the back of the head seems to have fulfilled a function similar to that of “maxillipeds” — appendages in mandibulates that assist with the other head limbs in the processing of food. This broad correspondence in function rather than in evolutionary origin is called “convergence.”

“From an evolutionary point of view, Habelia is close to the point of divergence between chelicerates and mandibulates,” Aria said. “But its similarities with mandibulates are secondary modifications of features that were in part already chelicerate in nature. This suggests that chelicerates originated from species with a high structural variability.”

The researchers conclude from the outstanding head structure, as well as from well-developed walking legs, that Habelia optata and its relatives were active predators of the Cambrian sea floors, hunting for small shelly sea creatures, such as small trilobites — arthropods with hard, mineralized exoskeletons that were already very diverse and abundant during Cambrian times.

“This builds onto the importance of carapaces and shells for evolutionary change during the Cambrian explosion, and expands our understanding of ecosystems at this time, showing another level of predator-prey relationship and its determining impact on the rise of arthropods as we know them today,” said Caron, who was Aria’s PhD supervisor when the bulk of this research was completed.

“The appearance and spread of animals with shells are considered to be one of the defining characteristics of the Cambrian explosion, and Habelia contributes to illustrate how important this ecological factor was for the early diversification of chelicerates and arthropods in general.”

  1. Cédric Aria, Jean-Bernard Caron. Mandibulate convergence in an armoured Cambrian stem chelicerate. BMC Evolutionary Biology, 2017; 17 (1) DOI: 10.1186/s12862-017-1088-7
  2. University of Toronto. “A 508-million-year-old sea predator with a ‘jackknife’ head: Oldest close parent of spiders, scorpions and horseshoe crabs evolved sophisticated head to hunt and eat small shelly animals.” ScienceDaily. ScienceDaily, 22 December 2017. <www.sciencedaily.com/releases/2017/12/171222090334.htm>.

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WFS News: Origins of photosynthesis in plants dated to 1.25 billion years ago

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The world’s oldest algae fossils are a billion years old, according to a new analysis by earth scientists at McGill University. Based on this finding, the researchers also estimate that the basis for photosynthesis in today’s plants was set in place 1.25 billion years ago.

The study, published in the journal Geology, could resolve a long-standing mystery over the age of the fossilized algae, Bangiomorpha pubescens, which were first discovered in rocks in Arctic Canada in 1990. The microscopic organism is believed to be the oldest known direct ancestor of modern plants and animals, but its age was only poorly dated, with estimates placing it somewhere between 720 million and 1.2 billion years.

The Angmaat Formation above Tremblay Sound on the Baffin Island coast. Bangiomorpha pubescens fossils occur in this roughly 500-meter thick rock formation. Credit: Timothy Gibson

The Angmaat Formation above Tremblay Sound on the Baffin Island coast. Bangiomorpha pubescens fossils occur in this roughly 500-meter thick rock formation.
Credit: Timothy Gibson

The new findings also add to recent evidence that an interval of Earth’s history often referred to as the Boring Billion may not have been so boring, after all. From 1.8 to 0.8 billion years ago, archaea, bacteria and a handful of complex organisms that have since gone extinct milled about the planet’s oceans, with little biological or environmental change to show for it. Or so it seemed. In fact, that era may have set the stage for the proliferation of more complex life forms that culminated 541 million years ago with the so-called Cambrian Explosion.

“Evidence is beginning to build to suggest that Earth’s biosphere and its environment in the latter portion of the ‘Boring Billion’ may actually have been more dynamic than previously thought,” says McGill PhD student Timothy Gibson, lead author of the new study.

Pinpointing the fossils’ age

To pinpoint the fossils’ age, the researchers pitched camp in a rugged area of remote Baffin Island, where Bangiomorpha pubescens fossils have been found There,despite the occasional August blizzard and tent-collapsing winds, they collected samples of black shale from rock layers that sandwiched the rock unit containing fossils of the alga. Using the Rhenium-Osmium (or Re-Os) dating technique, applied increasingly to sedimentary rocks in recent years, they determined that the rocks are 1.047 billion years old.

“That’s 150 million years younger than commonly held estimates, and confirms that this fossil is spectacular,” says Galen Halverson, senior author of the study and an associate professor in McGill’s Department of Earth and Planetary Sciences. “This will enable scientists to make more precise assessments of the early evolution of eukaryotes,” the celled organisms that include plants and animals.

Because Bangiomorpha pubescens is nearly identical to modern red algae, scientists have previously determined that the ancient alga, like green plants, used sunlight to synthesize nutrients from carbon dioxide and water. Scientists have also established that the chloroplast, the structure in plant cells that is the site of photosynthesis, was created when a eukaryote long ago engulfed a simple bacterium that was photosynthetic. The eukaryote then managed to pass that DNA along to its descendants, including the plants and trees that produce most of the world’s biomass today.

Origins of the chloroplast

Once the researchers had gauged the fossils’ age at 1.047 billion years, they plugged that figure into a “molecular clock,” a computer model used to calculate evolutionary events based on rates of genetic mutations. Their conclusion: the chloroplast must have been incorporated into eukaryotes roughly 1.25 billion years ago.

“We expect and hope that other scientists will plug this age for Bangiomorpha pubescens into their own molecular clocks to calculate the timing of important evolutionary events and test our results,” Gibson says. “If other scientists envision a better way to calculate when the chloroplast emerged, the scientific community will eventually decide which estimate seems more reasonable and find new ways to test it.”

  1. Timothy M. Gibson, Patrick M. Shih, Vivien M. Cumming, Woodward W. Fischer, Peter W. Crockford, Malcolm S.W. Hodgskiss, Sarah Wörndle, Robert A. Creaser, Robert H. Rainbird, Thomas M. Skulski, Galen P. Halverson. Precise age of Bangiomorpha pubescens dates the origin of eukaryotic photosynthesis. Geology, 2017; DOI: 10.1130/G39829.1
McGill University. “Origins of photosynthesis in plants dated to 1.25 billion years ago: Maybe the ‘Boring Billion’ wasn’t so boring, after all.” ScienceDaily. ScienceDaily, 20 December 2017. <www.sciencedaily.com/releases/2017/12/171220122032.htm>.
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WFS News: Treasure trove of highly detailed fossils uncovered

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A team of researchers from Uppsala University have uncovered a hidden diversity of microscopic animal fossils from over half a billion years ago lurking in rocks from the northern tip of Greenland.

The ‘Cambrian explosion’ of animal diversity beginning ~541 million years ago is a defining episode in the history of life. This was a time when the seas first teemed with animal life, and the first recognisably ‘modern’ ecosystems began to take shape.

Current accounts of this explosion in animal diversity rely heavily on records from fossilised shells and other hard parts, since these structures are the most likely to survive as fossils.

Microscopic animal fossils. From left; the oldest known pterobranch hemichordate; teeth from a priapulid, a sediment dwelling predatory worm; the carapace of a tiny arthropod. Credit: Slater, Willman, Budd and Peel

Microscopic animal fossils. From left; the oldest known pterobranch hemichordate; teeth from a priapulid, a sediment dwelling predatory worm; the carapace of a tiny arthropod.
Credit: Slater, Willman, Budd and Peel

However, since most marine animals are ‘soft-bodied’ this represents only a small fraction of the total diversity.

Rare sites of exceptional fossilisation, like the world-famous Burgess Shale, have revolutionised palaeontologists understanding of ‘soft-bodied’ Cambrian life. Because of the special conditions of fossilisation at these localities, organisms that did not produce hard mineralized shells or skeletons are also preserved. Such sites offer a rare glimpse into the true diversity of these ancient seas, which were filled with a dazzling array of soft and squishy predatory worms and arthropods (the group containing modern crustaceans and insects).

One of the oldest of these truly exceptional fossil bonanzas is the Sirius Passet site in the far north of Greenland. Unfortunately, during their long history, the rocks at Sirius Passet have been heated up and baked to high temperatures as the northern margin of Greenland smashed into various tectonic plates and buried these rocks deep beneath the surface.

All this heating has boiled away the delicate organic remains that once formed the fossils of soft bodied animals at Sirius Passet, leaving only faint impressions of their remains.

Not far to the south of Sirius Passet, the rocks have escaped the worst effects of this heating. A team of palaeontologists from Uppsala (Ben Slater, Sebastian Willman, Graham Budd and John Peel) used a low-manipulation acid extraction procedure to dissolve some of these less intensively cooked mudrocks. To their astonishment, this simple preparation technique revealed a wealth of previously unknown microscopic animal fossils preserved in spectacular detail.

Most of the fossils were less than a millimetre long and had to be studied under the microscope. Fossils at the nearby Sirius Passet site typically preserve much larger animals, so the new finds fill an important gap in our knowledge of the small-scale animals that probably made up the majority of these ecosystems. Among the discoveries were the tiny spines and teeth of priapulid worms — small hook shaped structures that allowed these worms to efficiently burrow through the sediments and capture prey. Other finds included the tough outer cuticles and defensive spines of various arthropods, and perhaps most surprisingly, microscopic fragments of the oldest known pterobranch hemichordates — an obscure group of tube-dwelling filter feeders that are distant relatives of the vertebrates. This group became very diverse after the Cambrian Period and are among some of the most commonly found fossils in rocks from younger deposits, but were entirely unknown from the early Cambrian. This new source of fossils will also help palaeontologists to better understand the famously difficult to interpret fossils at the nearby Sirius Passet site, where the flattened animal fossils are usually complete, but missing crucial microscopic details.

‘The sheer abundance of these miniature animal fossils means that we have only begun to scratch the surface of this overlooked resource, but it is already clear that this discovery will help to reshape our view of the non-shelly animals that crawled and swam among the early Cambrian seas more than half a billion years ago,’ says Sebastian Willman, researcher at the Department of Earth Sciences, Uppsala University.

  1. Ben J. Slater, Sebastian Willman, Graham E. Budd, John S. Peel. Widespread preservation of small carbonaceous fossils (SCFs) in the early Cambrian of North Greenland. Geology, 2017; DOI: 10.1130/G39788.1
Uppsala University. “Treasure trove of highly detailed fossils uncovered.” ScienceDaily. ScienceDaily, 19 December 2017. <www.sciencedaily.com/releases/2017/12/171219093415.htm>.
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WFS News: 3.5 billion-year-old fossil is oldest ever sign of life identified by scientists

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In a nearly 3.5 billion-year-old piece of rock from Western Australia, scientists have identified the oldest life forms ever known.The evidence consists of cylindrical and thread-like shapes thought to be fossilised microbes from the early days of life on Earth.

 New analysis has confirmed that a rock taken from a formation in Western Australia contains the oldest fossils ever discovered UW-Madison

New analysis has confirmed that a rock taken from a formation in Western Australia contains the oldest fossils ever discovered UW-Madison

The “microfossils” have been known for over two decades, but they have been the subject of considerable controversy within the scientific community.

 Critics have suggested the fossils, which are invisible to the naked eye, are just unusual shapes in the rock and not evidence of life at all.

Now, work led by Professor William Schopf, the palaeobiologist who first described the specimens in 1993, has put the matter to rest.

“I think it’s settled,” said Professor Schopf, who is based at the University of California, Los Angeles.

Together with a team of collaborators, Professor Schopf analysed the carbon composition of the ancient rock to find out the ratios of different carbon isotopes – that is, different types of carbon.

They found the ratios corresponded with the microbe-like structures in the rock.

“The differences in carbon isotope ratios correlate with their shapes,” said Professor John Valley, a researcher at the University of Wisconsin-Madison who co-led the study with Professor Schopf.

“If they’re not biological there is no reason for such a correlation.”

The technique for analysing these tiny fossils took the scientists 10 years to develop, and involves grinding down the original sample to carefully reveal the delicate fossils inside.

Source:News By Josh Gabbatiss Science Correspondent,http://www.independent.co.uk.

 Citation: SIMS analyses of the oldest known assemblage of microfossils document their taxon-correlated carbon isotope compositions PNAS 2017 ; published ahead of print December 18, 2017

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WFS News: Chemical tipping point of magma determines explosive potential of volcanoes

@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev

This is bubbly magma in laboratory used as starting material for the viscosity experiments. Credit: Danilo Di Genova

   This is bubbly magma in laboratory used as starting material for the viscosity experiments.
                                                              Credit: Danilo Di Genova

Volcanic eruptions are the most spectacular expression of the processes acting in the interior of any active planet. Effusive eruptions consist of a gentle and steady flow of lava on the surface, while explosive eruptions are violent phenomena that can eject hot materials up to several kilometres into the atmosphere.

The transition between these eruptions represents one of the most dangerous natural hazards.

Understanding the mechanisms governing such transition has inspired countless studies in Earth Sciences over the last decades.

In a new study led by Dr Danilo Di Genova, from the University of Bristol’s School of Earth Sciences, an international team of scientists provide evidence, for the first time, that a subtle tipping point of the chemistry of magmas clearly separates effusive from explosive eruptions worldwide.

Moreover, they demonstrate that variabilities at the nanoscale of magmas can dramatically increase the explosive potential of volcanoes.

Dr Di Genova said: “The new experimental data, thermodynamic modelling and analysis of compositional data from the global volcanic record we presented in our study provide combined evidence for a sudden discontinuity in the flow behaviour of rhyolitic magmas that guides whether a volcano erupts effusively or explosively.

“The identified flow-discontinuity can be crossed by small compositional changes in rhyolitic magmas and can be induced by crystallisation, assimilation, magma replenishment or mixing.

“Composition-induced flow behaviour variations may also originate from changes in magmas intrinsic parameters such as temperature, pressure or oxygen fugacity.”

These can result in revitalization of a previously “locked” magma chamber via chemical fluidification or may hinder efficient degassing and lead to increased explosive potential via chemical “stiffening” of a magma.

Furthermore, the study showed how the sudden precipitation of iron-bearing nanocrystals, which have been recently found in volcanic rocks, can increase the explosive potential of a magma via both depletion of iron in the melt structure and providing nucleation points for gas bubbles which drive explosive eruption.

  1. D. Di Genova, S. Kolzenburg, S. Wiesmaier, E. Dallanave, D. R. Neuville, K. U. Hess, D. B. Dingwell. A compositional tipping point governing the mobilization and eruption style of rhyolitic magma. Nature, 2017; 552 (7684): 235 DOI: 10.1038/nature24488
University of Bristol. “Chemical tipping point of magma determines explosive potential of volcanoes.” ScienceDaily. ScienceDaily, 13 December 2017. <www.sciencedaily.com/releases/2017/12/171213143510.htm>.
@WFS,World Fossil Society,Riffin T Sajeev,Russel T Sajeev