Mostrando postagens com marcador Anomalocaris. Mostrar todas as postagens
Mostrando postagens com marcador Anomalocaris. Mostrar todas as postagens

quinta-feira, 3 de dezembro de 2020

 Um dos primeiros euartrópodes cambrianos com apêndices raptoriais semelhantes aos do radiodonte

 

Resolver a evolução inicial dos euartrópodes é um dos problemas mais desafiadores na evolução dos metazoários. Fósseis do período cambriano excepcionalmente preservados contribuíram com dados paleontológicos importantes para decifrar esse processo evolutivo3,4. Estudos filogenéticos resolveram o Radiodonta (também conhecido como anomalocaridídeos) como o grupo mais próximo de todos os euartrópodes que possuem apêndices frontais no segundo segmento da cabeça (Deuteropoda). 

 

No entanto, as inter-relações entre os principais grupos de euartrópodes cambrianos permanecem disputadas, o que impede nossa compreensão da lacuna evolutiva entre Radiodonta e Deuteropoda. Aqui, descrevemos Kylinxia zhangi gen. et. sp. nov., um euartrópode da biota chinesa do início do Cambriano Chengjiang. Kylinxia possui não apenas características deuterópodes como um escudo de cabeça fundido, um tronco totalmente artrodizado e endopoditos articulados, mas também cinco olhos (como em Opabinia), bem como apêndices frontais raptoriais semelhantes a radiodonte. 

Nossa reconstrução filogenética recupera Kylinxia como um táxon de transição que faz a ponte entre Radiodonta e Deuteropoda. Os deuterópodes mais basais são recuperados como uma linhagem parafilética que apresenta apêndices frontais raptoriais plesiomórficos e inclui Kylinxia, ​​megacheirans, panqueliceratos, euartrópodes bivalves de ‘grande apêndice’ e isoxidas. Esta topologia filogenética apóia a ideia de que os apêndices frontais do radiodonte e megacheiran são homólogos, que as quelíceras de Chelicerata se originaram de grandes apêndices megacheiranos e que as antenas sensoriais em Mandibulata derivaram de formas raptoriais ancestrais. 

Kylinxia, ​​portanto, fornece insights importantes sobre as relações filogenéticas entre os primeiros euartrópodes, as transformações evolutivas e disparidade dos apêndices frontais e a origem de inovações evolutivas cruciais neste clado.

quarta-feira, 19 de junho de 2019

Fóssil Gigante Trilobita Encontrado na Austrália

Giant Trilobite Fossil Found on Australia
Um espécime de Redlichia rex do Emu Bay Shale, Kangaroo Island, Austrália. Crédito da imagem: Holmes et al, Uma impressão artística de Redlichia rex no fundo do mar Cambriano. Crédito da imagem: Katrina Kenny.

Paleontólogos desenterraram fósseis de uma espécie gigante de trilobita que habitou as águas australianas há aproximadamente 500 milhões de anos (período Cambriano).

Fósseis de uma nova espécie gigante do extinto grupo de criaturas marinhas chamado trilobites foram encontrados na Ilha Kangaroo, no sul da Austrália.

A descoberta está acrescentando informações importantes ao nosso conhecimento da "explosão" cambriana, o maior evento de diversificação na história da vida na Terra, quando quase todos os grupos de animais apareceram repentinamente há mais de meio bilhão de anos.

Os trilobitas, que têm esqueletos duros, calcificados e parecidos com armaduras, estão relacionados a crustáceos e insetos modernos.  
 
Eles são um dos grupos de animais fósseis mais bem sucedidos, sobrevivendo por cerca de 270 milhões de anos (521 a 252 milhões de anos atrás). Por causa de sua abundância no registro fóssil, eles são considerados um grupo modelo para entender este período evolutivo.

"Decidimos nomear esta nova espécie de trilobita Redlichia rex (semelhante ao Tyrannosaurus rex ) por causa de seu tamanho gigante, bem como suas pernas formidáveis ​​com espinhos usados ​​para triturar e triturar alimentos - que podem ter sido outros trilobitas", diz James. Holmes, estudante de doutorado na Escola de Ciências Biológicas da Universidade de Adelaide, que liderou a pesquisa.


A preservação de "partes moles" de trilobite, como as antenas e as pernas, é extremamente rara. A nova espécie foi descoberta no Emu Bay Shale na Ilha Kangaroo, um depósito de renome mundial famoso por este tipo de preservação. As descobertas foram publicadas no Journal of Systematic Palaeontology por uma equipe de cientistas da Universidade de Adelaide, do South Australian Museum e da University of New England.

A nova espécie tem cerca de 500 milhões de anos e é o maior trilobita cambriano descoberto na Austrália. Cresceu para cerca de 30 cm de comprimento, o que é quase o dobro do tamanho de outros trilobitas australianos de idade semelhante.

"Curiosamente, os espécimes trilobita do Emu Bay Shale - incluindo Redlichia rex - exibem lesões que foram causadas por predadores esmagadores de conchas", disse o autor sênior do estudo, professor associado Diego García-Bellido, da Universidade de Adelaide e do South Australian Museum. .

"Também há grandes espécimes de poo fossilizados (ou coprólitos) contendo fragmentos de trilobita neste depósito fóssil. O tamanho grande de espécimes feridos de Redlichia rex e coprólitos associados sugere que tanto predadores muito maiores estavam atacando Redlichia rex , como Anomalocaris - um criatura de camarão ainda maior - ou que a nova espécie tinha tendências canibais. "

Um dos principais impulsionadores da explosão Cambriana foi provavelmente uma "corrida armamentista" entre predadores e presas, com cada um desenvolvendo medidas mais eficazes de defesa (como a evolução das conchas) e ataques.

"O tamanho total e as pernas esmagadoras de Redlichia rex são uma consequência provável da corrida armamentista que ocorreu neste momento", diz James Holmes. "Este trilobita gigante era provavelmente o terror de criaturas menores no fundo do mar Cambriano."

Espécimes de Redlichia rex e outros fósseis de Emu Bay Shale estão atualmente em exposição no South Australian Museum.



A história acima é baseada em materiais fornecidos pela Universidade de Adelaide

segunda-feira, 15 de outubro de 2018

Período Cambriano: Fatos e Informações


Cambrian Period: Facts & Information
Trilobites were the dominant species during the Cambrian Period, 540 to 490 million years ago.
Credit: Bill Frische | Shutterstock
O Período Cambriano é o primeiro período de tempo geológico da Era Paleozóica (o “tempo da vida antiga”). Este período durou cerca de 53 milhões de anos e marcou uma explosão dramática de mudanças evolutivas na vida na Terra, conhecida como a "Explosão Cambriana". Entre os animais que evoluíram durante esse período, estavam os cordados - animais com cordas nervosas dorsais; braquiópodes encorpados, que se assemelhavam a amêijoas; e artrópodes - ancestrais de aranhas, insetos e crustáceos.

Though there is some scientific debate about what fossil strata should mark the beginning of the period, the International Geological Congress places the lower boundary of the period at 543 million years ago with the first appearance in the fossil record of worms that made horizontal burrows. The end of the Cambrian Period is marked by evidence in the fossil record of a mass extinction event about 490 million years ago. The Cambrian Period was followed by the Ordovician Period.
The period gets its name from Cambria, the Roman name for Wales, where Adam Sedgwick, one of the pioneers of geology, studied rock strata. Charles Darwin was one of his students. (Sedgwick, however, never accepted Darwin's theory of evolution and natural selection.)
In the early Cambrian, Earth was generally cold but was gradually warming as the glaciers of the late Proterozoic Eon receded. Tectonic evidence suggests that the single supercontinent Rodinia broke apart and by the early to mid-Cambrian there were two continents. Gondwana, near the South Pole, was a supercontinent that later formed much of the land area of modern Africa, Australia, South America, Antarctica and parts of Asia. Laurentia, nearer the equator, was composed of landmasses that currently make up much of North America and part of Europe. Increased coastal area and flooding due to glacial retreat created more shallow sea environments.
A fossilized <i>Spartobranchus tenuis</i> from the Burgess shale in Canada. The animal contains features of modern acorn worms and modern tube worms called pterobranches.
A fossilized Spartobranchus tenuis from the Burgess shale in Canada. The animal contains features of modern acorn worms and modern tube worms called pterobranches.
Credit: JB Caron
At this point, no life yet existed on land; all life was aquatic. Very early in the Cambrian the sea floor was covered by a “mat” of microbial life above a thick layer of oxygen-free mud. The first multicellular life forms had evolved in the late Proterozoic to “graze” on the microbes. These multicellular organisms were the first to show evidence of a bilateral body plan. These near-microscopic “worms” began to burrow, mixing and oxygenating the mud of the ocean floor. During this time, dissolved oxygen was increasing in the water because of the presence of cyanobacteria. The first animals to develop calcium carbonate exoskeletons built coral reefs. [Image Gallery: Cambrian Creatures: Primitive Sea Life]

The middle of the Cambrian Period began with an extinction event. Many of the reef-building organisms died out, as well as the most primitive trilobites. One hypothesis suggests that this was due to a temporary depletion of oxygen caused by an upwelling of cooler water from deep ocean areas. This upwelling eventually resulted in a variety of marine environments ranging from the deep ocean to the shallow coastal zones. Scientists hypothesize that this increase in available ecological niches set the stage for the abrupt radiation in life forms commonly called the “Cambrian Explosion.”
Scientists find some of the best specimens for the “evolutionary experiments” of the Cambrian Period in the fossil beds of the Sirius Passet formation in Greenland; Chenjiang, China; and the Burgess Shale of British Columbia. These formations are remarkable because the conditions of fossilization led to impressions of both hard and soft body parts and the most complete records of the varieties of organisms alive in the Cambrian Period.
The Sirius Passet formation has fossils estimated to be from the early Cambrian Period. Arthropods are the most abundant, although the groups are not as diverse as those found in the later Burgess Shale formation.

The Sirius Passet has the first fossil indications of complex predator/prey relationships. For example, Halkieria were slug-shaped animals with shell caps at either end. The rest of the body was covered in smaller armor plates over a soft snail-like “foot.” It is unclear whether they are more closely related to the annelids, such as modern-day earthworms and leeches, or are a primitive mollusk. Some specimens have been found in curled up defensive postures like modern pill bugs. Predator/prey relationships provide intensive selection pressures that lead to rapid speciation and evolutionary change.
The fearsome meter-long super-predator Anomalocaris.
The fearsome meter-long super-predator Anomalocaris.
Credit: Katrina Kenny & University of Adelaide
Burgess Shale fossils are from the late Cambrian. Diversity had increased dramatically. There are at least 12 species of trilobite in the Burgess Shale; whereas in the Sirius Passet, there are only two. 

It is clear that representatives of every animal phylum, excepting only the Bryozoa, existed by this time.
The largest predator was Anomalocaris, a free-swimming animal that undulated through the water by flexing its lobed body. It had true compound eyes and two claw-tipped appendages in front of its mouth. It was the largest most fearsome predator of the Cambrian Period, but did not survive into the Ordovician. 

The earliest known chordate animal, the Pikaia, was about 1.5 inches (4 centimeters) long. Pikaia had a nerve cord that was visible as a ridge starting behind its head and extending almost to the tip of the body. The fine detail preserved in the Burgess Shale clearly shows that Pikaia had the segmented muscle structure of later chordates and vertebrates. Haikouichythes, thought by some to be the earliest jawless fish, were also found in the Burgess Shale.

A mass extinction event closed the Cambrian Period. Early Ordovician sediments found in South America are of glacial origin. James F. Miller of Southwest Missouri State University suggests that glaciers and a colder climate may have been the cause of the mass extinction of the fauna that evolved in the warm Cambrian oceans. Glacial ice would have also locked up much of the free ocean water, reducing both the oxygen in the water and the area available for shallow water species.

Time periods
Precambrian: Facts About the Beginning of Time
Paleozoic Era: Facts & Information
Mesozoic Era: Age of the Dinosaurs
Cenozoic Era: Facts About Climate, Animals & Plants
Dinosaurs

terça-feira, 12 de junho de 2018

This Claw-Faced Sea Monster Was Literally Born to Kill


This Claw-Faced Sea Monster Was Literally Born to Kill
An artist's rendering shows a baby (foreground) and adult Lyrarapax unguispinus hunting the Cambrian seas like the creepy predators they were.
Credit: Science China Press
If you could dip your head into the oceans of Earth as they appeared 500 million years ago, you might see what looked like a spiny, disembodied claw cruising through the depths while trying to stuff an unfortunate piece of prey into its circular, fang-filled mouth. If you were lucky, you might even see a teeny-tiny baby claw bobbing along behind it.

A team of paleontologists from China, Australia and Germany has discovered one such baby claw fossilized in a piece of 518-million-year-old shale in Yunnan, China. The talon-shaped critter is actually a juvenile arthropod from the ancient predator Lyrarapax unguispinus, which hunted Earth's oceans during the Cambrian period (roughly 540 million to 490 million years ago).

Measuring a wee 18 millimeters, or 0.7 inches, long (about the diameter of a penny), the little tyke is the smallest complete L. unguispinus fossil ever discovered. And, according to a new study published June 1 in the journal National Science Review, this little baby was born to kill. [See Images of Bizarre Creatures from the Cambrian Period]

"Its adult-like morphology — especially the fully developed frontal appendages and [mouth] — indicates that L. unguispinus was a well-equipped predator at an early developmental stage," the researchers wrote in their new study.

The baby killer's built-in hunting gear provides further evidence that the spurt of biodiversity seen during the Cambrian explosion may have been driven partially by the sheer number of predators popping up throughout the seas.
As an arthropod, L. unguispinus is an ancient ancestor of today's spiders, scorpions and crustaceans, but — terrifyingly — it could grow to be more than 3.2 feet (1 meter) long. These colossal creepy-crawlers were among the world's earliest apex predators and were well equipped for the job, the researchers wrote.

Every L. unguispinus — even newborn babies, it seems — had a hard, claw-shaped raptorial (or grasping) appendage at the front of its head, which it used to capture and manipulate prey, the researchers wrote. To envision how these raptorial claws looked, see the modern arthropod known as the vinegarroon (so named for the twin streams of vinegar-like spray it shoots out of its bum when threatened).

Once an L. unguispinus caught you in its claws, the next stop on your tour of terror would probably be its toothy mouth. L. unguispinus belongs to a group of arthropods called Radiodonta, the researchers wrote, which translates to "radiating teeth." Radiodontans are characterized (as you might guess) by their circular mouths, filled with 360 degrees of serrated chompers.

The fact that even newborn radiodontans were born with developed teeth and claws could be evidence that species that first appeared during the Cambrian explosion faced tremendous competition with each other, the researchers wrote. This would give predators a strong incentive to evolve quickly, and ruthlessly.

"The predatory lifestyles of certain radiodontan offspring adds further tiering complexity to Cambrian marine food webs, and would have likely placed extra selective pressures on animal communities," the researchers wrote. "Intense predation occurring on all scales during the early phase of animal evolution was undoubtedly a critical driver behind the morphological and ecological innovations arising throughout the Cambrian."

In other words, the Cambrian period was literally a baby-eat-baby world. Let's all be thankful our squishy human babies don't have to face the same challenge.

sexta-feira, 27 de maio de 2011

Cambrian super-predators grew large in arms race

Metre-long anomalocaridids survived millions of years later than was thought.
beastThe giant Ordovician anomalocaridids were probably similar to this Cambrian Laggania.Esben Horn
 
The Cambrian Period's most ferocious predator clung to life for 30 million years longer than was previously thought. Fossils from Morocco show that sea creatures known as anomalocaridids survived long after they had been understood to have gone extinct, and their bodies grew to lengths in excess of one metre.
"Anomalocaridids are always depicted as these fierce horrible predators, ripping up things and tearing them apart — and no doubt some of them were," says Peter Van Roy, a palaeontologist at Yale University in New Haven Connecticut, who describes the findings today in Nature1, with his colleague Derek Briggs. The creatures were thought to have died out by the end of the Cambrian Period, about 500 million years ago, but "this discovery shows that anomalocaridids persisted for a lot longer and were still very successful predators at the top of the food chain".

Although the latest fossils were unearthed in North Africa and the imposing invertebrates are known to have prowled oceans worldwide, anomalocaridids are inextricably linked with the Burgess Shale, a rock formation in western Canada that contains the fossils that helped to define the Cambrian explosion — a time when strange-looking marine animals proliferated.
Anomalocaridids are bizarre even by Cambrian standards. From the late nineteenth century onwards, fossils of various body parts from the creatures were discovered separately, and attributed to ancient relatives of shrimp, sea cucumbers, jellyfish and arthropods. Only in 1985 did Briggs and a colleague realize that these bits and pieces belonged to a single kind of animal, with two tentacle-like appendages at its head, a flat, segmented body and a mouth shaped like a pineapple ring with teeth projecting towards the centre. They named it Anomalocaris2.

Fossil discoveries have since revealed that anomalocaridids came in diverse shapes and sizes — from Hurdia victoria, with its triangular carapace, to Schinderhannes bartelsi, with its long, pointed tail — and lived in the areas that are now Europe, the United States, Australia and China. But ancient relatives of sea scorpions and nautiluses that emerged in the Ordovician Period (490 million–440 million years ago) were suspected to have out-competed the anomalocaridids, causing them to die out, says Van Roy.
In 2008, however, an amateur collector, Mohammed Ben Said Ben Moula, discovered specimens that looked like anomalocaridids, Van Roy says. But it wasn't until 2009, when the researchers took a trip to the Fezouata rock formation in southeast Morocco, that they realized just what Ben Moula had discovered.
The rocks were from the early Ordovician Period, about 488 million–472 million years old — much younger than any in which such fossils had previously been found. "It was quite an indescribable moment when you're putting these things together and suddenly you realize this is an anomalocaridid," says Van Roy.

Beast of the deep

One formation contained the splayed-out, headless body of a beast more than a metre long — nearly twice as large as any of its Cambrian brethren — and more than three times the size of even the largest of the other fossilized species from the same rocks.
None of those other hard-bodied fossils from Fezouata showed the tell-tale marks of an attack from an anomalocaridid's strange mouth, so Van Roy thinks that the one-metre monsters probably hunted soft-bodied invertebrates. Their victims may have been ensnared by the anomalocaridid's giant appendages and then delivered to its mouth.
Jan Bergström, a palaeontologist at the Swedish Museum of Natural History in Stockholm, says that the presence of anomalocaridids in the Ordovician is "surprising news".
Allison Daley, a palaeontologist at the Natural History Museum in London, says that it is difficult to know what caused the extinction of anomalocaridids, but she is still willing to pin the blame on competition from other marine predators, albeit later ones than had been thought — such as cephalopods that emerged during the Ordovician.
The giant bodies of the Fezouata anomalocaridids, Daley speculates, could be the result of an ecological arms race with the emerging predators — one that the Cambrian-era monsters lost. "I doubt there was a period of happy coexistence between the anomalocaridids and newly evolving Ordovician predators," she says. 
  • References

    1. Van Roy, P. & Briggs, D. E. G. Nature 473, 510-513 (2011). | Article |
    2. Whittington, H. B. & Briggs, D. E. G. Phil. Trans. R. Soc. Lond. B 309, 569-609 (1985). | Article | ISI |