Mostrando postagens com marcador Período Cretáceo. Mostrar todas as postagens
Mostrando postagens com marcador Período Cretáceo. Mostrar todas as postagens

segunda-feira, 21 de novembro de 2022

Como era o Brasil há 100 milhões de anos

Como era o Brasil há 100 milhões de anos Estudo estabelece a cronologia de eventos tectônicos e climáticos nas bacias sedimentares Bauru, Sanfranciscana e dos Parecis, na região Centro-Sul do país (imagem: Wikimedia Commons)

Como era o Brasil há 100 milhões de anos

Novembro de 2022

O mais recente trabalho que procura atar três peças basilares desse quebra-cabeça colossal, as três bacias geológicas que sustentam a porção Centro-Sul do território brasileiro, acaba de ser publicado no Journal of South American Sciences. Um de seus autores é o geólogo Alessandro Batezelli, do Instituto de Geociências da Universidade Estadual de Campinas (Unicamp). O projeto teve o apoio da Fapesp.

O foco do estudo de Batezelli são as bacias sedimentares do Centro-Sul do Brasil, com destaque para as bacias Bauru, Sanfranciscana e dos Parecis. Entender o modo como os eventos tectônicos e climáticos interagiram em cada uma delas no tempo e no espaço ajuda a estabelecer uma sequência cronológica.

A descoberta daqueles eventos não foi obra de Batezelli e do geógrafo Francisco Sergio Bernardes Ladeira, o coautor do trabalho. Mas é a sua pesquisa, assim como a de outros profissionais, que nos permite tecer um esboço do drama geológico que se desenrolou no Centro-Sul brasileiro entre 135 e 60 milhões de anos atrás.

A ruptura de Gondwana

No período Jurássico, entre 201 e 145 milhões de anos atrás, a América do Sul e a África encontravam-se unidas. Ficavam bem no meio do antigo megacontinente Gondwana. As correntes de ar saturadas de umidade do antigo oceano Pantalássico não tinham força para atingir o distante centro de Gondwana. Daí a formação de um imenso deserto, o deserto Botucatu. É o mesmo processo que se vê hoje na Ásia Central, cujo clima desértico se deve à sua grande distância dos oceanos.

Quase não há fósseis preservados do Jurássico no Brasil. Explicações, para tanto, seriam o clima inóspito do deserto e também a difícil preservação de fósseis num ambiente de dunas. No entanto, o deserto Botucatu não era desabitado. Até agora, foram achadas apenas algumas pegadas fossilizadas de mamíferos e de répteis.

Há 140 milhões de anos, a América do Sul e a África começaram a se separar para dar início à abertura do Atlântico Sul. “O fenômeno que provocou a ruptura de Gondwana foi o surgimento de fraturas profundas na crosta terrestre”, diz Batezelli. Por essas fraturas começou a extravasar magma do interior do planeta em quantidades descomunais. À medida que as fendas iam se alargando, e os continentes se afastando, mais lava extravasava, num processo contínuo e muito prolongado, que perdurou de 137,4 a 128,7 milhões de anos atrás.

O epicentro desta megaerupção vulcânica, “ou mais apropriadamente um megaextravasamento basáltico, conhecido como Província Vulcânica Paraná-Etendeka,” como observa o geólogo, foi o Sudeste e o Sul do Brasil, que se encontravam ligados às terras da atual Namíbia, na África.

A Província Vulcânica Paraná-Etendeka foi formada a partir de diversas fendas, ou megavulcões, os maiores de que se têm notícia. Não eram vulcões explosivos, como os que estamos acostumados a ver. “Não havia erupções explosivas. As fendas jorravam continuamente”, diz Batezelli. “Daqui até a África havia fendas através das quais a lava extravasou sobre uma área gigantesca e por um período muito prolongado.” Através daquelas fendas transbordaram 2,3 milhões de km3 de lava, que cobriram totalmente 1,5 milhão de km2 – equivalente a cobrir o Estado do Amazonas, o maior do país, com uma camada de lava de 1,5 km de altura.

A origem do aquífero Guarani

Toda essa lava enterrou as antigas dunas do deserto Botucatu e foi-se acumulando em camadas sucessivas até erigir a Serra Geral, que cobre os Estados do Paraná, Santa Catarina e o norte do Rio Grande do Sul – além do leste paraguaio e o norte da Argentina. Sua areia foi cozinhada a uma temperatura de 1.200 graus centígrados e prensada pelo peso do magma. A areia acabou virando arenito, uma rocha bastante porosa que tem a propriedade de armazenar a água da chuva que é absorvida pelo solo.

No caso das dunas do deserto Botucatu, elas deram origem ao aquífero Guarani, um dos maiores reservatórios subterrâneos de água doce do planeta, enterrado sob o chão do Centro-Sudoeste do Brasil. O aquífero Guarani comporta 37 mil km3 de água, equivalente a 1,6 vez o volume do maior lago do planeta, o Baikal, na Sibéria.

“Nas regiões onde as dunas entraram em contato direto com a lava, houve um aumento de temperatura tão grande que os sedimentos foram literalmente cozidos, formando um arenito mais duro e impermeável, que é usado hoje nas calçadas de mosaico português”, diz Batezelli. Já a lava resfriada formou basalto, e este, desgastado por cem milhões de anos de erosão, deu origem à terra roxa, o solo fértil que alavancou no século XIX as lavouras de café em São Paulo e no Paraná.

Um novo deserto

Há 128,7 milhões de anos, quando os extravasamentos de magma findaram, aquele gigantesco acúmulo de rocha vulcânica fez com que parte do Sudeste brasileiro sofresse um abatimento sob seu próprio peso, o que criou na superfície uma nova bacia sedimentar, a Bacia Bauru. E sobre esta bacia formou-se um novo deserto de dunas, porém menor que o anterior.

O Atlântico Sul mal começara a abrir. Ainda nem era um braço de mar, no máximo uma depressão alagada para onde convergiam os rios, os sedimentos e a erosão de dois continentes. Ou seja, as águas de Pantalassa – o oceano que rodeava a Pangeia – ainda estavam longínquas, assim como sua brisa úmida. Para acabar com as condições de secura do Centro-Sul do Brasil, seria preciso aguardar outros 60 milhões de anos, quando o Atlântico Sul, embora com menos da metade da abertura atual, pôde amenizar o clima.

De qualquer forma, aquela depressão que lentamente se alargava um par de centímetros por ano já ia se fazendo sentir no clima. O novo deserto de dunas, agora denominado Grupo Caiuá, não era tão grande como o antigo deserto Botucatu, afirma Batezelli. Era árido, mas pontilhado aqui e ali por oásis infestados de várias espécies de crocodilos terrestres, parentes extintos dos crocodilianos atuais.

Aqueles crocodilos viviam em terra firme, tinham patas longas e andavam como lobos. Os paleontólogos já descreveram mais de uma dúzia de espécies. A mais famosa é o famigerado baurusuchus, uma fera predadora. Mas havia também formas bizarras, com chifres ou com uma carapaça semelhante à dos tatus, como a do armadillosuchus, e até um crocodilo herbívoro, o esfagessauro.

As dunas do Caiuá existiram entre 125 e 100 milhões de anos atrás, quando cederam lugar a uma nova paisagem formada por rios e lagos. “O clima se tornou muito mais ameno, similar ao semiárido da Caatinga nordestina”, diz Batezelli. Essa nova depressão recebeu sedimentos que hoje pertencem ao Grupo Bauru, que existiu entre 80 e 60 milhões de anos atrás.

Aí sim os titanossauros proliferaram. A maioria das espécies brasileiras é dessa fase. Seus fósseis homenageiam o nome das cidades mineiras e paulistas próximas das quais foram encontrados, como uberabatitan e baurutitan.

A Bacia Sanfranciscana

Concomitante a estes 60 milhões de anos de transformações na Bacia Bauru, “mais para o norte, na Bacia Sanfranciscana, ocorreram fenômenos muito parecidos, embora sem serem os mesmo”, salienta Batezelli. A Bacia Sanfranciscana engloba o oeste de Minas Gerais, Goiás, Tocantins e o oeste da Bahia, estendendo-se até o sul do Piauí.

Durante o Cretáceo inferior, na Bacia Sanfranciscana se desenvolveram campos de dunas eólicas. Dezenas de milhões de anos depois, já no Cretáceo superior, também aconteceu vulcanismo. “Bem no limite entre as bacias Bauru e Sanfranciscana se formaram diversos vulcões”, revela Batezelli pautado em sua pesquisa. “Eles apresentaram um extravasamento bem menor do que o vulcanismo que deu origem à Serra Geral, porém foram responsáveis por formar uma região mais elevada entre as Bacias Bauru e Sanfranciscana. Foi como se a crosta inchasse por causa do calor das intrusões magmáticas.”

Seu relevo é perceptível até hoje, nas crateras no interior das quais estão as cidades de Araxá, Tapira e Poços de Caldas. “As grandes jazidas de nióbio assim como outras riquezas minerais do sudeste de Minas Gerais estão relacionadas a este vulcanismo.”

O vulcanismo na Bacia Sanfranciscana ocorreu há menos de 100 milhões de anos atrás. A maior parte da lava que extravasou desses vulcões avançou sobre as dunas.

A evolução da Bacia dos Parecis é semelhante ao ocorrido nas bacias Bauru e Sanfranciscana. Ainda no período Jurássico superior, ocorreu um vulcanismo modesto nos Parecis. Há 145 milhões de anos atrás, já no Cretáceo superior, formaram-se rios e lagos na região compreendida entre o norte do Mato Grosso e o oeste de Rondônia. Com o passar do tempo o clima foi se tornando mais árido e o cenário paisagístico se transformou num campo de dunas.

Em resumo, e comparando os cenários das três bacias sedimentares, conclui-se que do Cretáceo inferior ao Cretáceo superior, um período de mais de 60 milhões de anos, houve um deslocamento dos desertos de dunas no território brasileiro das direções sudeste para noroeste.

Das dunas eólicas aos rios e lagos

Durante o Cretáceo inferior, a região Sudeste era dominada por uma paisagem desértica formada por dunas eólicas. Já no Cretáceo superior, a maior parte da região Sudeste passou a ter uma paisagem constituída por rios e lagos, enquanto que desertos de dunas surgiram no norte de Minas, em Goiás, Tocantins, Matogrosso e Rondônia. “Isso demonstra que, com o passar do tempo, houve uma diminuição nas condições de umidade de sul/sudeste para o centro-oeste/norte do Brasil”, revela Batezelli.

Todo o drama geológico descrito acima se desenrolou em paralelo ao alargamento do Atlântico Sul. Suas brisas que cresciam em volume e intensidade semeavam cada vez mais umidade na porção sudeste do continente.

Esse era o cenário dominante quando da extinção em massa do fim do Cretáceo, há 65 milhões, que deu fim aos dinossauros. Esse legado geológico, geográfico e climático formou o novo meio ambiente no qual os mamíferos da era Cenozoica puderam se adaptar. Mas esta é uma outra história.

O artigo Stratigraphic framework and evolution of the Cretaceous continental sequences of the Bauru, Sanfranciscana, and Parecis basins, Brazil, de Betezelli e Ladeira, publicado no Journal of South American Earth Sciences, pode ser lido em http://www.sciencedirect.com/science/article/pii/S0895981115300857

quarta-feira, 30 de maio de 2018

Cretaceous Period: Animals, Plants & Extinction Event


Cretaceous Period: Animals, Plants & Extinction Event
Tyrannosaurus rex is part of the carnivorous groups of dinosaurs that, according to new research, maintained a stable level of biodiversity leading up to the mass extinction at the end of the Cretaceous.
Credit: AMNH/J. Brougham
The Cretaceous Period was the last and longest segment of the Mesozoic Era. It lasted approximately 79 million years, from the minor extinction event that closed the Jurassic Period about 145.5 million years ago to the Cretaceous-Paleogene (K-Pg) extinction event dated at 65.5 million years ago.
In the early Cretaceous, the continents were in very different positions than they are today. Sections of the supercontinent Pangaea were drifting apart. The Tethys Ocean still separated the northern Laurasia continent from southern Gondwana. The North and South Atlantic were still closed, although the Central Atlantic had begun to open up in the late Jurassic Period. By the middle of the period, ocean levels were much higher; most of the landmass we are familiar with was underwater. By the end of the period, the continents were much closer to modern configuration. Africa and South America had assumed their distinctive shapes; but India had not yet collided with Asia and Australia was still part of Antarctica.
Parts of supercontinent Pangaea eventually drifted apart to become the continents we know today.
Parts of supercontinent Pangaea eventually drifted apart to become the continents we know today.
Credit: USGS
One of the hallmarks of the Cretaceous Period was the development and radiation of the flowering plants. The oldest angiosperm fossil that has been found to date is Archaefructus liaoningensis, found by Ge Sun and David Dilcher in China. It seems to have been most similar to the modern black pepper plant and is thought to be at least 122 million years old.

It used to be thought that the pollinating insects, such as bees and wasps, evolved at about the same time as the angiosperms. It was frequently cited as an example of co-evolution. New research, however, indicates that insect pollination was probably well established before the first flowers. While the oldest bee fossil was trapped in its amber prison only about 80 million years ago, evidence has been found that bee- or wasp-like insects built hive-like nests in what is now called the Petrified Forest in Arizona.

These nests, found by Stephen Hasiotis and his team from the University of Colorado, are at least 207 million years old. It is now thought that competition for insect attention probably facilitated the relatively rapid success and diversification of the flowering plants. As diverse flower forms lured insects to pollinate them, insects adapted to differing ways of gathering nectar and moving pollen thus setting up the intricate co-evolutionary systems we are familiar with today.
There is limited evidence that dinosaurs ate angiosperms. Two dinosaur coprolites (fossilized excrements) discovered in Utah contain fragments of angiosperm wood, according to an unpublished study presented at the 2015 Society of Vertebrate Paleontology annual meeting. This finding, as well as others, including an Early Cretaceous ankylosaur that had fossilized angiosperm fruit in its gut, suggests that some paleo-beasts ate flowering plants.
Moreover, the shape of some teeth from Cretaceous animals suggests that the herbivores grazed on leaves and twigs, said Betsy Kruk, a volunteer researcher at the Field Museum of Natural History in Chicago.
During the Cretaceous Period, more ancient birds took flight, joining the pterosaurs in the air. The origin of flight is debated by many experts. In the “trees down” theory, it is thought that small reptiles may have evolved flight from gliding behaviors. In the “ground up” hypothesis flight may have evolved from the ability of small theropods to leap high to grasp prey. Feathers probably evolved from early body coverings whose primary function, at least at first, was thermoregulation.

About the size of a crow, Confuciusornis is the earliest known bird to have a true beak. It lived about 10 to 15 million years after Archaeopteryx, but like its early ancestor, it still had clawed fingers. Males were typically larger than females and sported long, narrow tail feathers that they may have used to attract mates. Some scientists question whether Confuciusornis was a direct ancestor of modern birds. They propose instead that it was a cousin that early on went its own separate way.
About the size of a crow, Confuciusornis is the earliest known bird to have a true beak. It lived about 10 to 15 million years after Archaeopteryx, but like its early ancestor, it still had clawed fingers. Males were typically larger than females and sported long, narrow tail feathers that they may have used to attract mates. Some scientists question whether Confuciusornis was a direct ancestor of modern birds. They propose instead that it was a cousin that early on went its own separate way.
Credit: Eduard Solà Vázquez
At any rate it is clear that avians were highly successful and became widely diversified during the Cretaceous. Confuciusornis (125 million to 140 million years ago) was a crow-size bird with a modern beak, but enormous claws at the tips of the wings. Iberomesornis, a contemporary, only the size of a sparrow, was capable of flight and was probably an insectivore. [Image Gallery: Avian Ancestors: Dinosaurs That Learned to Fly]

By the end of the Jurassic, some of the large sauropods, such as Apatosaurus and Diplodocus, went extinct. But other giant sauropods, including the titanosaurs, flourished, especially toward the end of the Cretaceous, Kruk said.
Large herds of herbivorous ornithischians also thrived during the Cretaceous, such as Iguanodon (a genus that includes duck-billed dinosaurs, also known as hadrosaurs), Ankylosaurus and the ceratopsians. Theropods, including Tyrannosaurus rex, continued as apex predators until the end of the Cretaceous.
About 65.5 million years ago, nearly all large vertebrates and many tropical invertebrates became extinct in what was clearly a geological, climatic and biological event with worldwide consequences. Geologists call it the K-Pg extinction event because it marks the boundary between the Cretaceous and Paleogene periods. The event was formally known as the Cretaceous-Tertiary (K-T) event, but the International Commission on Stratigraphy, which sets standards and boundaries for the geologic time scale, now discourages the use of the term Tertiary. The "K" is from the German word for Cretaceous, Kreide.
In 1979, a geologist who was studying rock layers between the Cretaceous and Paleogene periods spotted a thin layer of grey clay separating the two eras. Other scientists found this grey layer all over the world, and tests showed that it contained high concentrations of iridium, an element that is rare on Earth, but common in most meteorites, Kruk said in a class she co-taught on Coursera.org.
Also within this layer are indications of “shocked quartz” and tiny glass-like globes called tektites that form when rock is suddenly vaporized then immediately cooled, as happens when an extraterrestrial object strikes the Earth with great force.

The Chicxulub (CHEEK-sheh-loob) crater in the Yucatan dates precisely to this time. The crater site is more than 110 miles (180 kilometers) in diameter and chemical analysis shows that the sedimentary rock of the area was melted and mixed together by temperatures consistent with the blast impact of an asteroid about 6 miles (10 km) across striking the Earth at this point.
When the asteroid collided with Earth, its impact triggered shockwaves, massive tsunamis and sent a large cloud of hot rock and dust into the atmosphere, Kruk said. As the super-heated debris fell back to Earth, they started forest fires and increased temperatures.

"This rain of hot dust raised global temperatures for hours after the impact, and cooked alive animals that were too large to seek shelter," Kruk said in the class. "Small animals that could shelter underground, underwater, or perhaps in caves or large tree trunks, may have been able to survive this initial heat blast."
Tiny fragments likely stayed in the atmosphere, possibly blocking part of the sun's ray for months or years. With less sunlight, plants and the animals dependent on them would have died, Kruk said. Furthermore, the reduced sunlight would have lowered global temperatures, impairing large active animals with high-energy needs, she said.
"Smaller, omnivorous terrestrial animals, like mammals, lizards, turtles, or birds, may have been able to survive as scavengers feeding on the carcasses of dead dinosaurs, fungi, roots and decaying plant matter, while smaller animals with lower metabolisms were best able to wait the disaster out," Kruk said.
There is also evidence that a series of huge volcanic eruptions at the Deccan traps, located along the tectonic border between India and Asia, began just before the K-Pg event boundary. It is likely that these regional catastrophes combined to precipitate a mass extinction.
The world was a warmer place during the Cretaceous period. The poles were cooler than the lower latitudes, but "overall things were warmer," Kruk told Live Science. Fossils of tropical plants and ferns support this idea, she said.
Animals lived all over, even in colder areas. For instance, Hadrosaurus fossils dating to the Late Cretaceous were uncovered in Alaska.
When the asteroid hit, the world likely experienced so-called "nuclear winter," when particles blocked many of the sun's rays from hitting Earth.
Additional resources
Additional reporting by Staff Writer Laura Geggel. Follow her on Twitter @LauraGeggel. Follow Live Science @livescience, Facebook & Google+

https://www.livescience.com/29231-cretaceous-period.html 

sábado, 3 de março de 2018

 Cretaceous collagen: Can molecular paleontology glean soft tissue from dinosaurs?

Mary Schweitzer, of North Carolina State University, and her colleagues first reported the discovery of soft tissue in a Tyrannosaurus rex femur in 2005. The vial contains a sample of the bone. Credit: both: ©Science.

Mary Schweitzer, of North Carolina State University, and her colleagues first reported the discovery of soft tissue in a Tyrannosaurus rex femur in 2005. The vial contains a sample of the bone. Credit: both: ©Science.

In the early 1990s, “Jurassic Park” hatched a wild idea: that dinosaurs could be reincarnated using tiny amounts of preserved DNA. In the bestselling books and blockbuster movies, the premise hinged on extracting fragments of dinosaur DNA from ancient blood-sucking insects preserved in amber, filling in the genetic gaps with snippets of modern amphibian DNA and hatching the engineered dinosaurs out of ostrich eggs. In reality, however, while many amazing things have been found in fossilized tree sap, DNA isn’t one of them.

“Jurassic Park” fans saw a glimmer of hope in 2005, when a team of molecular paleontologists led by Mary Schweitzer of North Carolina State University reported finding soft tissue preserved inside a 68-million-year-old Tyrannosaurus rex femur. DNA is notoriously delicate, and dinosaur DNA itself has not been found — a possibility Schweitzer calls extremely unlikely since the oldest DNA recovered to date is less than a million years old and nonavian dinosaurs died out 66 million years ago. However, in the decade since that initial find, Schweitzer’s team has unearthed mounting evidence that soft tissues, such as blood vessels, collagen and other proteins, whose long, folded chains of amino acids make them much more robust than DNA, can survive more than 66 million years of degradation.

If 68-million-year-old dinosaur soft tissue can really be recovered — a claim that has been met with much skepticism — it may help paleontologists answer some long-standing questions about dinosaur physiology, such as whether the behemoths were cold- or warm-blooded. The existence of ancient preserved soft tissues would also change how we think about fossilization and the handling and storing of fossils: After all, if soft tissue can be recovered from ancient fossils, we need to be more careful in how we extract and preserve them. Living, roaring tyrannosaurs may not be the future, but perhaps molecular paleontology is.

An Accidental Find

Schweitzer working in a lab at Montana State University. Her team has found evidence for soft tissues in about one-third of the several dozen dinosaur specimens they have studied. Credit: Kelly Gorham, Montana State University. Schweitzer working in a lab at Montana State University. Her team has found evidence for soft tissues in about one-third of the several dozen dinosaur specimens they have studied. Credit: Kelly Gorham, Montana State University.
 
 
The young field of molecular paleontology was thrust into the international spotlight in 2005 when Schweitzer’s team announced in Science their discovery of T. rex soft tissue. The tissues were found by accident: After some broken femur fragments were dissolved in a weak acid solution, a scrap of oddly stretchy material was left over.

Under a microscope, the scrap showed what appeared to be bifurcating blood vessels, cellular structures similar to those found in bone cells of modern animals, as well as fibrous bone matrix tissue and small, round red structures resembling red blood cells. The 68-million-year-old tissue had all the hallmarks of collagen — the main component of connective tissue and one of the most abundant proteins in living animals. “When I first saw [the tissues], my first thought was, ‘Those aren’t supposed to be there.’ Back then, I didn’t think soft-tissue preservation was possible either,” Schweitzer says.
Credit: K. Cantner, AGI. Credit: K. Cantner, AGI.
As far as biomolecules go, collagen is tough, but nobody thought it could be that tough. The oldest nondinosaur collagen recovered to date came from a 3.5-million-year-old camel fossil found in the high Arctic of Canada. The unique geochemical conditions required for long-term preservation of proteins like collagen are still unknown. In fact, the process of fossilization in general remains somewhat mysterious, in part because the rigors of geologic time are impossible to reproduce in the lab. In conventional fossils, just hard parts such as bones, teeth and shells remain; soft parts are typically lost to predation or decay before being fossilized.

In exceptional cases, such as the fossils of the Burgess Shale in British Columbia, delicate soft-tissue structures, such as gills or stomach contents, are mineralized and preserved as rock, but what Schweitzer found was even stranger: actual soft tissue that had somehow escaped scavengers, rotting and the ravages of time for 68 million years.


“Living bone is made up of minerals plus organic matter,” Schweitzer says. After death, as the organics, such as collagen, degrade, they leave behind voids in the bone at the molecular level. During fossilization, those voids fill with minerals, which help preserve the bone for millions of years as a fossil. “The leaving of the organics is part of what allows the fossil to form,” she says. “But in reality, this textbook process of fossilization doesn’t explain all the various modes of fossilization we see, some of which we have no idea about how they happen.”

Repeatable Results

Many dinosaur fossils have been found in Montana, including the 68-million-year-old T. rex and an 80-million-year-old Brachylophosaurus canadensis in which Schweitzer’s team identified collagen, blood vessels, hemoglobin, the proteins actin and myosin, and molecules called histones that help package DNA. Credit: Mary Schweitzer. Many dinosaur fossils have been found in Montana, including the 68-million-year-old T. rex and an 80-million-year-old Brachylophosaurus canadensis in which Schweitzer’s team identified collagen, blood vessels, hemoglobin, the proteins actin and myosin, and molecules called histones that help package DNA. Credit: Mary Schweitzer.
 
Since their initial discovery in 2005, Schweitzer’s team has published dozens of studies identifying collagen, blood vessels, hemoglobin, the proteins actin and myosin, and molecules called histones that help package DNA, in the 68-million-year-old T. rex and in an 80-million-year-old hadrosaur, both found in Montana.

When identifying unusual tissues, Schweitzer starts with high-resolution light microscopy to examine samples for evidence of deep age: If tissues are actually many millions of years old, certain levels of damage are expected. “Does it look altered from a living tissue? Is it possible these are original molecules?” Schweitzer asks. Then, she turns to antibodies, which recognize and bind to certain types of proteins present in a sample. “Antibodies are extremely specific. If I can get a signal, then it justifies the added expense and destruction of [the sample required for] mass spectrometry sequencing,” she says. Mass spectrometry is the definitive method used to identify and characterize both modern and ancient proteins.

The team’s most recent study, published this year in the Journal of Proteome Research, revisited collagen they recovered from the hadrosaur. In a 2009 study, Schweitzer’s team identified three fragments, or peptides, from Type 1 collagen. Peptides are made up of amino acids — the building blocks of protein — and each of the fragments was about 15 amino acids long. As read by a mass spectrometer, the three fragments appeared to be similar to collagen 1 peptides found in living reptiles. For the 2017 study, the team worked with new samples from the same hadrosaur and used updated extraction methods and more sensitive mass spectrometry to identify eight peptides: six new and two that matched the 2009 fragments. The new fragments were found to line up most closely with collagen found in modern birds — the surviving dinosaurs.
The dinosaur bone at the base of the rock in the center of the image was found by Schweitzer’s team in Montana. Credit: Mary Schweitzer. The dinosaur bone at the base of the rock in the center of the image was found by Schweitzer’s team in Montana. Credit: Mary Schweitzer.
 
“This latest study is an effort to show that our data are repeatable,” Schweitzer says. “Everything was different, except for the source dinosaur. We worked in a different lab, with different instruments, using different extraction buffers and different analytical tools, and we still got the same sequences.”
Ideally, other groups would also validate the findings, but not many places are equipped to study such ancient proteins, says Elena Schroeter, a postdoctoral researcher at North Carolina State University and lead author of the 2017 study. “An important step in the scientific process is replication of data in other labs. That’s been one of our major problems: This is high-risk research, it’s hard to get funding, and it is very expensive,” she says. “You need to be able to dedicate a lab exclusively to ancient proteins to keep everything isolated, to avoid the possibility of cross-contamination, and not many places are set up for that.”

The new study is “the most convincing evidence I’ve seen yet that these proteins really are from dinosaurs,” says Enrico Cappellini, a professor of paleoproteomics at the Natural History Museum of Denmark in Copenhagen. “[Schweitzer’s] lab is very careful about contamination,” he says. “They’re doing everything right in keeping the ancient stuff totally separate from modern stuff. My inclination is that their data are authentic, but there’s still room for improvement. I can understand why many of my colleagues are not yet convinced.”
Bone cell (left) and red blood cells (right). The brown cells (in focus) are surrounded by a white fibrous matrix from the B. canadensis specimen that Schweitzer’s team studied. Credit: both: courtesy of Mary Schweitzer. Bone cell (left) and red blood cells (right). The brown cells (in focus) are surrounded by a white fibrous matrix from the B. canadensis specimen that Schweitzer’s team studied. Credit: both: courtesy of Mary Schweitzer.
 
Cappellini says he would like to see the extraction procedure simplified. Schweitzer’s technique “has a lot of steps, and with each step, you get a loss of peptides. With a less convoluted procedure, they might be able to recover a higher number [of peptides] and other labs might be able to follow the technique,” he says.

One of the most vocal critics has been Matthew Collins, a biochemist at the University of York in England who specializes in recovering ancient proteins. “Mary Schweitzer is either doing something very right or she’s doing something very wrong,” Collins says. At this point, the most convincing data would come out of an independent lab, he says. “I would be really happy if other labs could replicate [Schweitzer’s] data. [My lab has] tried and we’ve been unsuccessful. So far, they’re the only ones who have been able to do this.”

Much of the criticism from Collins and others involves questions about contamination, either from bacterial biofilms that invaded the fossil long ago and produced the soft-tissue-like materials, or from modern contaminants introduced in the lab. In May, Michael Buckley of the University of Manchester in England and his colleagues published a study in Proceedings of the Royal Society B that highlights the difficulties of discriminating dinosaur proteins from modern cross-contaminants. Buckley and his team extracted collagen from modern ostrich bone and identified protein sequences identical to those found by Schweitzer’s team in the hadrosaur in their January study and the tyrannosaur in the original 2005 study. The findings were “a bit suspicious,” Cappellini says. They mean “that either 80-million-year-old dinosaur proteins are identical to those found in modern ostriches or that [Schweitzer’s] lab was contaminated with ostrich proteins.”
Schweitzer’s team recovered soft tissue from a B. canadensis fossil found in Montana. Credit: Pedro Salas. Schweitzer’s team recovered soft tissue from a B. canadensis fossil found in Montana. Credit: Pedro Salas.
 
Schweitzer says it’s understandable that some of the hadrosaur proteins will be identical to those found in modern ostriches — because collagen is known to be a highly conserved molecule across a diverse array of species. Dinosaurs and their modern relatives — birds — could share some of the same protein sequences, she says. “Many molecules are conserved across species, over millions of years. They work, so they remain unchanged by evolution.” In fact, she says, some amount of sequence overlap would be expected, so the similarities between the hadrosaur and ostrich peptides don’t mean there was contamination in her team’s samples.

The limited availability of established protein sequences is one of the big challenges in this field, she says. “We are dealing with the limitations of an emerging discipline. When you have a 66-million-year-old protein, what do you compare it to?” Currently, Schweitzer’s team has to settle for comparing protein sequences to those of extant bracketing species such as birds and crocodiles. “But the databases are very limited for creatures that are not mammals. These animals [ostriches and crocodiles] were not represented in existing databases until we put them there. ”

Preserved by Iron?

Field emission scanning electron microscope images of demineralized ostrich bone matrix (left) versus B. canadensis bone matrix (right). Both show osteocytes (bone cells). Some of the ostrich proteins are identical to the B. canadensis proteins. Credit: both: courtesy of Mary Schweitzer. Field emission scanning electron microscope images of demineralized ostrich bone matrix (left) 
versus B. canadensis bone matrix (right). Both show osteocytes (bone cells). Some of the ostrich proteins are identical to the B. canadensis proteins. Credit: both: courtesy of Mary Schweitzer.
Schweitzer and her colleagues feel they have demonstrated that contamination isn’t undermining their sensational findings, but they have not yet figured out how ancient tissues can persist for millions of years. “That’s the million-dollar question. How on Earth is this possible?” says Tim Cleland, a molecular biologist at the Smithsonian’s Museum Conservation Institute in Washington, D.C., who has co-authored papers with Schweitzer, including the 2017 study.

“I have yet to hear a plausible explanation for how soft tissues can be preserved for this long,” Collins says, citing the huge leap of time from 3.5 million years to more than 66 million years. “The more I understand about it, the more difficult it is to believe it can happen,” he says. “There may be something very special about these fossils, but for me they’re defying basic chemistry and physics. I’d like to see better comprehension of what happens when proteins decay and how decay might be suspended indefinitely.”

In 2013, Schweitzer’s team offered a hypothesis: The preservative could be iron. Tissues from both the tyrannosaur and the hadrosaur they studied were found to be chock-full of iron nanoparticles. Iron is abundant in living organisms, especially in the blood, where it makes up part of the oxygen-transport protein hemoglobin. Iron is notoriously bioreactive, so much so that organisms must take biochemical precautions to prevent excess iron from causing tissue damage. But while iron can be detrimental to living tissues, it can act like a preservative in dead tissues, Schweitzer says.
“When a dinosaur dies, it has a boatload of iron in its blood and muscles. And when that iron is released into the carcass, it goes about cross-linking like crazy, tying proteins and cell membranes in knots, basically acting a lot like formaldehyde,” she says. Tissues treated with formaldehyde can sit in a jar on a shelf for decades, but decay is only delayed, not arrested. To demonstrate iron’s preservative capabilities, Schweitzer extracted blood vessels from modern ostrich bones and treated them with iron-rich hemoglobin. “The control [samples turned to] mush in three days, but the vessels exposed to hemoglobin are still sitting on a shelf in my lab at room temperature six years later,” she says. Collins says he remains skeptical. “Iron may slow down the decay process but it’s not clear how it could be arrested altogether,” he says.

Finding and Storing Soft Tissue

 The internal conditions of a carcass play a role in the initial stages of tissue preservation, but the external environment is crucial for fossilization. “Every fossil has its own unique geochemical environment,” Schroeter says. And while paleontologists have a good idea where they should look for dinosaur fossils — in Mesozoic sedimentary rocks, usually in hot, dry places such as eastern Montana and northeastern Utah — they’re still figuring out what conditions are more likely to support fossils with pres The internal conditions of a carcass play a role in the initial stages of tissue preservation, but the external environment is crucial for fossilization. “Every fossil has its own unique geochemical environment,” Schroeter says. And while paleontologists have a good idea where they should look for dinosaur fossils — in Mesozoic sedimentary rocks, usually in hot, dry places such as eastern Montana and northeastern Utah — they’re still figuring out what conditions are more likely to support fossils with preserved soft tissues and how much might exist. “It’s an open question, how much of this [soft-tissue] material is out there,” Cleland says. Soft tissue in dinosaur fossils is rarely found, but that may be because “people rarely look” for it, Schroeter says. Credit: K. Cantner, AGI; inset figures modified from Schweitzer et al., Proceedings of the Royal Academy B, 2006.
 
It may be more common than we realize, Schweitzer adds. Her team has found evidence for soft tissue in about a third of the several dozen specimens they have studied. “We will probably find more if we look more,” she says.

Schweitzer’s team has been working on formulating a profile of burial environments that seem to be conducive to protein preservation. “Fossils that are found in sandstone seem to have better preservation than those that come from shale or claystone, but we don’t really know why that is yet,” Cleland says. “The only thing we know for sure is that the carcass needs to be buried very quickly after death.” The dinosaurs that Schweitzer’s team has worked with have been found partially articulated — a sign that the carcasses were not pulled apart by scavengers.
“You have to be pretty lucky to find a well-preserved dinosaur bone, let alone a whole dinosaur,” Schroeter says. “There’s a huge range of preservation out there. Some fossils have perfect histological structure and look just like pristine bone in terms of their microstructure, while other fossils look just like rocks.”

Once fossilized materials are removed from the ground, whatever equilibrium they were in can be disrupted. In an effort to preserve any remaining soft tissues and prevent contamination, Schweitzer’s team has developed a new approach to excavating and handling fossils. “It’s best to keep the fossils in the sediment they were in until you get them into a controlled lab setting,” Schweitzer says, even though this sometimes results in massively jacketed fossils that are a logistical nightmare to transport. “We can remove the fossil wearing gloves, without using any glues, using sterile instruments and containers in an isolated lab.”
To preserve soft tissue and prevent contamination, Schweitzer’s team wraps dinosaur fossils in massive plaster jackets and transports them — however cumbersome they are — back to the lab, where researchers can remove the fossil using sterile gloves, instruments and containers. Credit: Ken Lacovara. To preserve soft tissue and prevent contamination, Schweitzer’s team wraps dinosaur fossils in massive plaster jackets and transports them — however cumbersome they are — back to the lab, where researchers can remove the fossil using sterile gloves, instruments and containers. Credit: Ken Lacovara.
 
Then, instead of being stored in museum drawers where they might be contaminated, the fossils are kept in sterile glass jars, in special cabinets isolated from other fossils or modern samples, in a room far removed from other specimens. The team is also developing better techniques for storing these samples long term. “Technology gets better and more sensitive by leaps and bounds all the time,” Cleland says. “We want these samples to be around in [a decade] and even longer.”

Constructive Results From Destructive Sampling

Testing for proteins requires destructive sampling, in which bits of the fossils are inevitably destroyed. “Plenty of curators aren’t big fans of destructive sampling,” Schroeter says. “I’d really like to test more specimens, but it can be hard to get people to let you grind up their fossils.”
Paleontology has long relied on scant clues gleaned from bones turned to stone, and the possibility of introducing molecular techniques into the field is tantalizing to some researchers. “Part of the power of molecular paleontology is the ability to look at dinosaurs from a different angle,” Schroeter says. “Morphology can get you pretty far, but there are a lot of things that bones can’t tell you.”
Even skeptics agree that molecular paleontology has great potential. “If soft-tissue preservation is possible, it would open vast areas of the fossil record to molecular analysis,” Collins says. “Honestly, I really hope [Schweitzer] is right.”
Many scientists are loathe to allow even tiny pieces of fossil, like this piece of rib from a Lufengosaurus, a sauropod, to be destroyed — a necessary process for molecular paleontology. Credit: Lee et al., Nature Communications, 2017.Many scientists are loathe to allow even tiny pieces of fossil, like this piece of rib from a Lufengosaurus, a sauropod, to be destroyed — a necessary process for molecular paleontology. Credit: Lee et al., Nature Communications, 2017.
A molecular approach could answer long-standing questions about the physiology of dinosaurs, such as how they regulated body temperature, how their cardiovascular systems were able to support such large creatures, and how they grew and reproduced, as well as resolve how various species were related to one another, how they spread around the planet, and how some lines evolved into birds. But the field has a long way to go.

One of the biggest hurdles is the difficulty of proving endogeneity — that the proteins recovered come from a dinosaur and not a bacterial or modern source (see sidebar, page 45). “When you are testing fossils, it is critical to use multiple methods to examine and reexamine, test and retest different aspects of the molecules we think we’re recovering,” Schweitzer says. “To get the field moving forward, we need to come to a consensus on which methods are the most efficient, and which methods can tell us the most with the least amount of [sample] destruction.”

Other teams have developed methods of testing for ancient preserved proteins that don’t require destructive sampling, but the methods’ reliability is uncertain and they provide limited information about samples. For example, Yao-Chang Lee of the National Synchrotron Radiation Research Center and National Central University in Taiwan and colleagues published a study in Nature Communications this year in which they claim to have recovered collagen from a 195-million-year-old long-necked Lufengosaurus. The researchers described using nondestructive infrared spectroscopy to identify the protein. But there’s a flaw with this method, Cappellini says. “With this technique, you can see a chemical signature of what might be a protein, but it’s not a clear fingerprint like you get with mass spectrometry.” And that’s just not good enough, he says. “On controversial samples this ancient, it’s necessary to have unquestionable evidence.”

The Future Could Be Molecular

Recep Avci (standing) and Jahson Suo look at images of soft tissue from dinosaurs under a microscope. Credit: Kelly Gorham, Montana State University. Recep Avci (standing) and Jahson Suo look at images of soft tissue from dinosaurs under a microscope. Credit: Kelly Gorham, Montana State University.
 
After weathering years of controversy, Schroeter says she is beginning to feel like a mouse running endlessly on a wheel: “Some of us in Mary’s lab feel like we’re stuck continuously arguing that these proteins can persist, even though we’ve shown repeatedly that they do,” she says. “We want to get beyond these same arguments and focus on what we can learn from these tissues.”

Schweitzer says she chooses to respond to her critics by working harder. “The doubters push me to do everything the best I can do it,” she says. “I want to make this work last for the ages.” Neither Schweitzer nor Schroeter are holding their breath for a single piece of evidence that will satisfy their critics once and for all. “When making a scientific argument ... you want a bunch of different lines of evidence that all point toward the same thing,” Schroeter says.
Whether it’s finding blood vessels from hadrosaurs, like this Saurolophus (right), or determining the colors of feathers on dinosaurs like the Jiangxisaurus (left), researchers hope molecular paleontology can reveal many long-kept dinosaur secrets. Credit: right: L. Xing and Y. Liu, PLOS ONE, CC BY 2.5; above: Danny Cicchetti, CC BY 3.0. Whether it’s finding blood vessels from hadrosaurs, like this Saurolophus (right), or determining the colors of feathers on dinosaurs like the Jiangxisaurus (left), researchers hope molecular paleontology can reveal many long-kept dinosaur secrets. Credit: right: L. Xing and Y. Liu, PLOS ONE, CC BY 2.5; above: Danny Cicchetti, CC BY 3.0.
 
Interest in the field is growing, but the number of labs set up for this kind of work remains limited, Schroeter says. “Paleontology has always been a little slow on the uptake in adopting new technology, but as more young people get interested, they’ll bring their tech savvy,” she says. “To be competitive, you have to constantly be thinking of new questions, new approaches, new ideas. This is how we’re going to raise the bar for paleontology.”

Can preserved proteins reveal paint-by-numbers plumage?

Fossil feathers highlight one of the biggest challenges for molecular paleontology: proving that structures or tissues are endogenous and not modern or bacterial contamination. Left: Transmission electron microscopy image of a brown chicken feather, used as a modern control for fossil feathers. Right: Fossilized feather of Gansus yumenensis. Credit: left: Alison Moyer; right: Becky Kirkland. Fossil feathers highlight one of the biggest challenges for molecular paleontology: proving that structures or tissues are endogenous and not modern or bacterial contamination. Left: Transmission electron microscopy image of a brown chicken feather, used as a modern control for fossil feathers. Right: Fossilized feather of Gansus yumenensis. Credit: left: Alison Moyer; right: Becky Kirkland.
Some of the most compelling dinosaur fossils are those found with clearly defined feathers. Feathers may seem fragile and unlikely to be preserved, but in fact they’re composed of durable keratin, one of the toughest natural proteins. Additionally, some fossil feathers unearthed are speckled with tiny black dots, which, according to different studies, could be remnants of either bacteria or melanosomes. Melanosomes are organelles that produce and store melanin, the main source of pigment in feathers. If melanosomes are indeed preserved in some ancient fossils, they could reveal information about dinosaur coloration and plumage — and represent further evidence of preserved proteins in dinosaurs.

Fossil feathers highlight one of the biggest challenges for molecular paleontology: proving that structures or tissues are endogenous and not modern or bacterial contamination. Melanosomes “are identical in size and shape to bacteria,” and “both bacteria and melanosomes can be present in the same microscopic viewing field,” says Alison Moyer, a molecular biologist at Drexel University in Pennsylvania. That means scientists “can’t assume that structures are melanosomes and then use that data to make further assumptions about the animal’s appearance and lifestyle.” The good news, she says, is that researchers have the capability to identify melanosomes; the bad news is that the technique is complicated, time-consuming and expensive.

In modern bird feathers, melanosomes are encased in keratin. In 2016, Yanhong Pan of the Chinese Academy of Sciences and colleagues published a study in Proceedings of the National Academy of Sciences in which they differentiated melanosomes encased in keratin from similar looking bacteria. “That should be the gold standard for melanosome studies,” says Johan Lindgren, a molecular paleontologist at Lund University in Sweden. “But too often people skip that step and go straight to coloration.” For molecular paleontology to move forward with confidence, more standards are needed, Lindgren says. “The field is so new that we haven’t developed common standards that all scientists use,” he says. “Each research team has their own standards, which can range from simply looking at the morphology to full-blown molecular comparisons.”
The stronger the standards, the better the evidence will be, says Mary Schweitzer, a molecular paleontologist at North Carolina State University. People accept that scientists can recover proteins when they relate to color but not that scientists can recover proteins when it relates to soft tissues, like collagen, she adds. It “highlights the unequal application of standards.”
As to whether we’ll ever have a complete picture of dinosaur plumage in full color, Lindgren says, “never say never.” However, melanin is only one factor determining coloration, with other pigments and structurally derived colors — those generated by microscopic surface structures that create iridescent colors — also playing a role. “It’s hard to know how much information can be preserved,” he says. “True dinosaur coloration may be lost to time.”

Mary Caperton Morton

Mary Caperton Morton
Morton (https://theblondecoyote.com/) is a freelance science and travel writer based in Big Sky, Mont., and an EARTH roving correspondent.
Monday, October 16, 2017 - 06:00

Mary Caperton Morton

Mary Caperton Morton
Morton (https://theblondecoyote.com/) is a freelance science and travel writer based in Big Sky, Mont., and an EARTH roving correspondent.

quinta-feira, 16 de julho de 2015

 PALEONTOLOGIA DE VERTEBRADOS

[Paleontology • 2015] Zhenyuanlong suni • A Large, Short-armed, Winged Dromaeosaurid (Dinosauria: Theropoda) from the Early Cretaceous of China and Its Implications for Feather Evolution

Zhenyuanlong suni  Lü & Brusatte, 2015
The famous ‘feathered dinosaurs’ from the Early Cretaceous of Liaoning Province, northeastern China, include several dromaeosaurids, which are among the closest relatives of birds. Most of these are small-bodied taxa with long arms and broad wings comprised of vaned feathers, but a single specimen (the holotype of Tianyuraptor) belongs to a much larger individual with reduced forelimbs, which unfortunately lacks any preserved integument. We describe a new specimen of large-bodied, short-armed Liaoning dromaeosaurid, which we designate as a new genus and species, Zhenyuanlong suni. The integument is well preserved and provides the first evidence of feather morphologies and distribution in a short-armed (and probably non-volant) dromaeosaurid, indicating that these rare and aberrant taxa had large wings consisting of pennaceous feathers on the arms and long pennaceous feathers on the tail very similar to their smaller and longer-armed relatives, but potentially lacked vaned feathers on the legs. Zhenyuanlong adds yet more diversity to the Liaoning dromaeosaurid fauna, helps further reveal a distinct short-armed bauplan among dromaeosaurids, and illuminates previously-unrecognized homoplasy that complicates dromaeosaurid phylogeny and suggests that the Liaoning taxa may not have formed their own clade.
An artist’s impression of the new short-armed and winged feathered dinosaur Zhenyuanlong suni found in China and from the early Cretaceous period (125m years ago).
illustration: Chuang Zhao || doi: 10.1038/srep11775
Figure 1: The holotype of the large-bodied, short-armed Liaoning dromaeosaurid Zhenyuanlong suni gen et. sp. nov. (JPM-0008).
Systematic palaeontology
Dinosauria Owen 1842. 
Saurischia Seeley 1887. 
Theropoda Marsh 1881. 
Coelurosauria Huene 1914. 
Maniraptora Gauthier 1986. 
Dromaeosauridae Matthew and Brown 1922. 

Zhenyuanlong suni gen. et sp. nov.
Etymology: Long”, from the Chinese Pinyin, means dragon. The generic and specific names are in honor of Mr. Zhenyuan Sun, who secured the specimen for study.
Holotype: A nearly complete skeleton with skull and lower jaws preserved (JPM-0008), curated at the Jinzhou Paleontlogical museum. It is likely a sub-adult, as neural arches and centra are not fused in some anterior dorsal vertebrae and the sacral vertebrae, and the anterior sacral vertebrae are not completely fused to each other. The individual is fairly mature, however, as the more posterior sacrals are fused to each other and the neural arches and centra of the cervical vertebra, caudal vertebrae, and some dorsal vertebrae are fused.
Type Locality and Horizon: Sihedang of Jianchang County, Liaoning Province; Yixian Formation
Figure 4: The integument of the large-bodied, short-armed Liaoning dromaeosaurid Zhenyuanlong suni gen et. sp. nov. (JPM-0008).
(A) overview of the skeleton with regions of integument indicated with grey highlight; (B) proximal tail; (C) left forearm; (D) right forearm; (E) closeup of coverts on right forearm.
Figure 5: Phylogenetic relationships of Zhenyuanlong suni among dromaeosaurid theropods.
Junchang Lü and Stephen L. Brusatte. 2015. A Large, Short-armed, Winged Dromaeosaurid (Dinosauria: Theropoda) from the Early Cretaceous of China and Its Implications for Feather Evolution. Scientific Reports. 5, 11775 doi: 10.1038/srep11775

Paleo Profile: Zhenyuanlong suni http://on.natgeo.com/1f7Bw3q via @ngphenomena
Zhenyuanlong suni: biggest ever winged dinosaur is found in China http://gu.com/p/4ayjn/stw

quinta-feira, 7 de maio de 2015

[PaleoOrnithology • 2015]

Archaeornithura meemannae • The Oldest Record of Ornithuromorpha from the early Cretaceous of China


Archaeornithura meemannae
Wang, Zheng, O’Connor, Lloyd, Wang, Wang, Zhang & Zhou. 2015

A reconstruction of the oldest ornithuromorph, Archaeornithura meemannae, a specialized wading bird from the Early Cretaceous of China.
illustration: Zongda Zhang | doi: 10.1038/ncomms7987
Ornithuromorpha is the most inclusive clade containing extant birds but not the Mesozoic Enantiornithes. The early evolutionary history of this avian clade has been advanced with recent discoveries from Cretaceous deposits, indicating that Ornithuromorpha and Enantiornithes are the two major avian groups in Mesozoic. Here we report on a new ornithuromorph bird, Archaeornithura meemannae gen. et sp. nov., from the second oldest avian-bearing deposits (130.7 Ma) in the world. The new taxon is referable to the Hongshanornithidae and constitutes the oldest record of the Ornithuromorpha. However, A. meemannae shows few primitive features relative to younger hongshanornithids and is deeply nested within the Hongshanornithidae, suggesting that this clade is already well established. The new discovery extends the record of Ornithuromorpha by five to six million years, which in turn pushes back the divergence times of early avian lingeages into the Early Cretaceous.
Systematic paleontology
Aves 
Ornithothoraces 
Ornithuromorpha 
Hongshanornithidae
Archaeornithura meemannae gen. et sp. nov.
 Type genus. Hongshanornis, Zhou and Zhang.
 Etymology. The generic name is derived from Greek ‘Archae’ and ‘ornithura’, meaning ‘ancient ornithuromorph’. The specific name is in honour of Dr Meemann Chang for her continuous support of the study of the Jehol Biota.

 Holotype. An articulated partial skeleton with feathers (STM7-145), housed at the Tianyu Natural History Museum of Shandong (STM), China (Fig. 1).
Figure 1: Holotype of Archaeornithura meemannae gen. et sp. nov., STM7-145.
Figure 5: Cladogram showing the systematic position of Archaeornithura meemannae among Mesozoic birds.


 Min Wang, Xiaoting Zheng, Jingmai K. O’Connor, Graeme T. Lloyd, Xiaoli Wang, Yan Wang, Xiaomei Zhang & Zhonghe Zhou. 2015. The Oldest Record of Ornithuromorpha from the early Cretaceous of China. Nature Communications. 6, Article number: 6987 doi: 10.1038/ncomms7987

Remains of oldest known relative of modern birds discovered in China http://gu.com/p/485kx/stw @IanSample
Scientists find the oldest ever relative of modern birds http://wpo.st/yQtF0 @RachelFeltman