Najash rionegrina, a snake with legs

It’s a busy time for transitional fossil news—first they find a fishapod, and now we’ve got a Cretaceous snake with legs and a pelvis. One’s in the process of gaining legs, the other is in the early stages of losing them.

Najash rionegrina was discovered in a terrestrial fossil deposit in Argentina, which is important in the ongoing debate about whether snakes evolved from marine or terrestrial ancestors. The specimen isn’t entirely complete (but enough material is present to unambiguously identify it as a snake), consisting of a partial skull and a section of trunk. It has a sacrum! It has a pelvic girdle! It has hindlimbs, with femora, fibulae, and tibiae! It’s a definitive snake with legs, and it’s the oldest snake yet found.

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Tiktaalik makes another gap

Paleontologists have uncovered yet another specimen in the lineage leading to modern tetrapods, creating more gaps that will need to be filled. It’s a Sisyphean job, working as an evolutionist.

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This creature is called Tiktaalik roseae, and it was discovered in a project that was specifically launched to find a predicted intermediate form between a distinctly fish-like organism, Panderichthys, and the distinctly tetrapod-like organisms, Acanthostega and Ichthyostega. From the review article by Ahlberg and Clack, we get this summary of Tiktaalik‘s importance:

First, it demonstrates the predictive capacity of palaeontology. The Nunavut field project had the express aim of finding an intermediate between Panderichthys and tetrapods, by searching in sediments from the most probable environment (rivers) and time (early Late Devonian). Second, Tiktaalik adds enormously to our understanding of the fish-tetrapod transition because of its position on the tree and the combination of characters it displays.

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Taphonomy of fossilized embryos

There are these fossilized embryos from the Ediacaran, approximately 570 million years ago, that have been uncovered in the Doushantuo formation in China. I’ve mentioned them before, and as you can see below, they are genuinely spectacular.

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Parapandorina raphospissa

But, you know, I work with comparable fresh embryos all the time, and I can tell you that they are incredibly fragile—it’s easy to damage them and watch them pop (that’s a 2.3MB Quicktime movie), and dead embryos die and decay with amazing speed, minutes to hours. Dead cells release enzymes that trigger a process called autolysis that digests the embryo from within, and any bacteria in the neighborhood—and there are always bacteria around—descend on the tasty corpse and can turn it into a puddle of goo in almost no time at all. It makes a fellow wonder how these fossils could have formed, and what kind of conditions protect the cells from complete destruction before they were mineralized. Another concern is what kinds of embryos are favored by whatever the process is—is there a bias in the preservation?

Now Raff et al. have done a study in experimental taphonomy, the study of the conditions and processes by which organisms are fossilized, and have come up with a couple of answers for me. Short version: the conditions for rapid preservation are fairly easy to generate, but there is a bias in which stages can be reliably preserved.

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Lamprey skeletons

Bone is a sophisticated substance, much more than just a rock-like mineral in an interesting shape. It’s a living tissue, invested with cells dedicated to continually remodeling the mineral matrix. That matrix is also an intricate material, threaded with fibers of a protein, type II collagen, that give it a much greater toughness—it’s like fiberglass, a relatively brittle substance given resilience and strength with tough threads woven within it. Bone is also significantly linked to cartilage, both in development and evolution, with earlier forms having a cartilaginous skeleton that is replaced by bone. In us vertebrates, cartilage also contains threads of collagen running through it.

These three elements—collagen, cartilage, and bone—present an interesting evolutionary puzzle. Collagen is common to the matrices of both vertebrate cartilage and bone, yet the most primitive fishes, the jawless lampreys and hagfish, have been reported to lack that particular form of collagen, suggesting that the collagen fibers are a derived innovation in chordate history. New work, though, has shown that there’s a mistaken assumption in there: lampreys do have type II collagen! This discovery clarifies our understanding of the evolution of the chordate skeleton.

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Jurassic beaver

Say hello to Castorocauda lutrasimilis, a primitive mammalioform from the middle Jurassic—164 million years ago. Despite its great age, it has evidence of fur and guard hairs still preserved in the fossil, and was rather large for its time. It’s estimated to have weighed about 500g (about a pound) and was over 400mm (over a foot) long in life, and as you can see from the reconstruction, shows signs of being aquatic. In size and lifestyle, it probably resembled the modern platypus.

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I’m redundant-who needs a blogger?

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There’s a lovely article in this week’s Nature documenting a transitional stage in tetrapod evolution (you know, those forms the creationists like to say don’t exist), and a) Nature provides a publicly accessible review of the finding, and b) the primary author is already a weblogger! Perhaps there will come a day when I’m obsolete and willl just have to turn my hand to blogging about what I had for lunch.

For an extra super-duper dose of delicious comeuppance, though, take a look at this thread on the Panda’s Thumb. I wrote about Panderichthys, and a creationist (“Ghost of Paley”) comes along to mangle the phylogeny and make wild negative assertions about the validity of interpretations of fossils based on work from the Ahlberg lab…when Martin Brazeau of the Ahlberg lab and author of this new paper shows up to straighten him out.

And for my next trick, let me introduce you to Marshall McLuhan…

Brazeau MD, Ahlberg PE (2006) Tetrapod-like middle ear architecture in a Devonian fish. Nature 439:318-321.

Orsten fossils

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Bredocaris admirabilis

Ooooh, there’s a gorgeous gallery of Orsten fossils online. These are some very pretty SEMs of tiny Cambrian animals, preserved in a kind of rock called Orsten, or stinkstone (apparently, the high sulfur content of the rock makes it smell awful). What are Orsten fossils?

Orsten fossils in the strict sense are spectacular minute secondarily phosphatised (apatitic) fossils, among them many Crustacea of different evolutionary levels, but also other arthropods and nemathelminths. The largest fragments we have do not exceed two mm. Orsten-type fossils, on the other hand, have the great advantage in being three-dimensionally preserved with all surface structures in place and thus easier to interpret than any other fossil material. Orsten fossils are preserved virtually as if they were just critical-point dried extant organisms. Details observable range down to less than 1 µm, and include pores, sensilla and minute secondary bristles on filter setae and denticles. Orsten fossils also give an insight of meiofaunal benthic life at small scale, including preservation larval stages, and hence a life zone inhabited by the earliest metazoan elements of the food chain.

It’s a good browse over there. I think it’s useful to remember that the majority of the fauna of the world both extant and half a billion years ago is and was tiny and unfamiliar.