Tag Archives: Paleontology

Ida the Fossil Primate

You probably know that there is a new primate fossil, nicknamed “Ida,” and that there is quite a buzz about it.

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Darwinius masillae, aka Ida

ResearchBlogging.org
Ida comes from fossil deposits in Germany, and was originally excavated in two different parts by private collectors, and only recently rejoined and recognized for the amazing fossil it is. This is considered to be a new genus, and is named Darwinius masillae

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…holotype skeleton in right lateral view…

Ida is a 47 million year old adapid primate of outstanding, unprecedented state of preservation that seems to have some very interesting and possibly unexpected features that could shed light on the evolutionary relationships among the extinct primates. But before we get to that, we need to cover some background on primates, extinct and otherwise.

The first thing you need to know is that order of living primates can be divided into two groups: the suborders Strepsirrhini and the Haplorrhini.

Strepsirrhini includes the lemurs of Madagascar, and the lorises, pottos and galagos of Africa and Asia. In other words, Strepsirrhini are the Prosimians, more or less.

The Haplorrhini include the old world monkeys and the new world monkeys, and the apes, as well as this one strange group called the Tarsiers (which used to be in the Prosimians, which has caused some confusion.) The Haplorrhini are the “Anthropoid primates,” more or less.

Based on morphology and DNA and so on, it is believed that these two groups diverged from one another perhaps as far back as 80 million years ago (Murphy et al 2009). Subsequent to that time, the different smaller groups of primates (old world vs. new world monkeys, for instance) diversified.

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Artist reconstruction

Now, here is a basic problem that plagues primate evolutionary research. If you look at all the features that make a primate a primate (as opposed, say, to a tree shrew or some other mammal) using only living species, you get a workable set of features. If you take standard lemurs and, say, Old World Monkeys and you make a set of distinctions between those two groups, you get a reasonable set of criteria to distinguish among them. But, when you either add in Tarsiers (or some other primate groups) or start looking at fossils that are tens of millions of years old, it starts to get tricky. It becomes difficult to distinguish between convergence and common ancestry for certain traits. In other words, it is hard to tell if two traits are the same in two groups because the common ancestor of those groups had the trait and the specimens you are looking at both inherited this, or if the two lineages independently evolved the same trait.

“How likely is that to happen?” you may be asking yourself. Answer: Under some conditions, very very unlikely. Under other conditions, very likely. Let me explain.

Imagine we wanted to do a phylogeny of sedans. Once a line of car develops a square-back or pickup design, we eliminate it from our analysis. Sedans only. At the same time, some other research team is analyzing “powered vehicles” …. things that go with engines. This would include cars, trucks, boats, trains, and space ships. Even though both lineages may have been around for about the same amount of time, the sedan lineage would be much more prone to convergence because all sedans are almost exactly the same length, width, and height, have almost exactly the same number of seats, the same method for driving (like, auto vs. one stick) and so on, compared to the vehicles in the second study. The comparisons across vehicles that can carry nine tons of gravel, vehicles that can go under water, and vehicles that can fly are going to result in only the most trivial and easily exposed convergences.

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Radiograph

Same with primates. At many important levels, all primates are the same. Compared to carnivores, all primates have almost the same pattern of teeth … there are very few variants on tooth pattern among all the primates that exist today, but many many variants for the carnivores. Even body size is fairly restricted for primates. Yes, there are a few whopping big ones, but compared to the elephants or the hyracoidea, not so much. With only a few exceptions, primates live in moist to wet heavily vegetated environments. Compare this to antelope, who have water-dependent and water-independent species. And so on.

Perhaps because of this limited range of variation, or perhaps causing this limiting range, is the simple fact that morpholgically all primates are primitive. So there is not some group of primates where the radius and ulna are fused, and a different group where they are not. All primates have unfused radius and ulna. There are not primates with vs. without some kind of grasping hand (I simplify slightly here). All primates have the same number of fingers and toes. In comparison, for instance, carnivores have varying numbers of toes and different patterns of bone fusions among them.

So that is the background. If you are going to look at ancient fossils, you’ve got a very conservative set of lineages so a) you’ll always recognize a primate, quite easily, when you see one and b) convergence will haunt you for your entire life if you are a paleo-primatologist.

For various reasons, especially the item noted above about the moist heavily vegetated habitats, but also the sparseness on the landscape and lightly built skeletons, primates make lousy fossils. There are very few places in the world where we have primate fossils, and they are much restricted in geographical space and time range. In short, the primate fossil record sucks. The primate fossil record is mostly teeth, and the teeth look all the same. All the work I’ve done in the primate fossil record has been in the Miocene, and that is not so bad. There are better conditions: You get some real fossils, even postcranial (body) bones, sometimes. But the pre-Miocene record is really scary.

Paleontologically, primates are anatomically ambiguous ghosts.

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As a juvenile, Ida has both deciduous (“baby”) teeth and adult teeth. More teeth = more data.

Within the fossil record, there are probably four or five sets of fossils that represent groups different from living primates, but most “crown” fossils can be placed into two major groups: The adapids and the omomyids. If either of these two groups could be linked to later, living primates, this would have to be done using a number of physical characteristics of the bone … there is not much chance of finding ancient DNA in these very old fossils.

This part of the fossil primate record includes the Adapoidea, including the widespread Adapids and some other fossil groups, but no living forms, and the Tarsioidea, which includes the fossil Omomyids, some other fossil forms, and the living Tarsius. The Adapids and Omomyids date mainly to the Eocene about 55 to 34 million years ago. Note that this is well after the Haplorrhini-Strepsirrhini split. Over the years, various groups of primatologists have attempted to link either of these groups to the major living groups of primates.

One subgroup of the Adapoidea is the Cercamoniinae, identified in the 1970s by one of the present paper’s authors, Philip Gingerich. This group exhibits a few traits that seem to link it with the living Haplorrhini (monkeys and apes). For example modern monkeys often have a premolar that is shaped a certain way to “hone” the canine. This is a bit unusual, and is a marker for this kind of modern primate. Something that looks like such a tooth appears, more or less, among the Cercamoniinae. This sort of connection (and other factors) has led some (Gingerich included) to link the Adapoidea in general to the modern anthropoid primates (monkeys and apes). Others disagree.

The fossil being reported now, Ida, is grouped by the authors into the Cercamoniinae. If that phylogenetic conclusion ends up being verified by further study, this excellent, well preserved fossil will be an important touchstone in interpreting early anthropoid (non-lemur) primate evolution and behavioral ecology.

The phylogenetic argument that is being made in this paper is admittedly preliminary (more work is promised on this) but so far it is very tricky and is likely to remain tricky. The structure of the prior arguments that links either of the two main fossil groups to either of the two main living groups has always been tenuous. The reason for this, as I’ve alluded to above, is that those two fossil groups fall about half way in time between the present and the original split of these groups, and there are not enough fossils between 80 and 55 million years ago to understand the details of that early split. Then, there are not enough fossils from about 34 million years ago to recent times to understand this later period during which the modern forms arose. While more work will be done on the phylogenetic relationships, considering that the contemporary fossils …. the old fossils roughly of the same age as “Ida” … are mostly teeth, and tens of millions of years separates Ida from the modern forms, I do not expect much more in the way of a resolution until more fossils like Ida, but of different species, are found.

Getting away from phylogeny, let’s have a look at other aspects of this fossil. This is a remarkably well preserved specimen. The animal probably died from volcanic gas (like C02) and fell into the water, and was slowly buried in fine sediment. Once encapsulated, the body began to rot, and the slime layer that started out as the animals’ flesh, skin, and fur approximated the outer surface of the body and was preserved in the fine sediment as well. The sediments in which this fossil is preserved are compressed, so the entire skeleton is uniformly crushed, slightly, but everywhere, affecting every bone. In order to visualize and measure the specimen, fancy 3D imaging and image processing techniques were applied.

The animal was a juvenile female and weighted between 385 and 580 grams, and would have grown up to be about 660 grams by one estimate, or a whopping 1600 or 1700 grams by another estimate. Since the larger estimate is based on molar size, which in turn can be secondarily influenced by adaptations to diet, I’d go with the lower estimate. Indeed, using the brute force method of holding the fossil up to full scale pictures of living primates to find one that matches, the estimated adult body size is about 845 to 892 grams.

The contents of the digestive track were preserved (that is extraordinary) and include leaves and fruit. There are no insect remains in the gut.

You are going to hear more about this fossil, as more analysis is done. I have two meta-remarks to make about this finding. First, there was a lot of hype about how this fossil is a “missing link” and so on and so forth. That was overdone. But equally overdone is the reaction to the hype. Almost every blog post or other secondary report I’ve seen on this has talked almost as much … or more … about the hype than about the fossil. Second, please note that this find was reported in PLoS ONE, an open access on line journal. This means that you can see the report yourself, look at all the cool pictures, and try if you must to slog through the highly technical text. This is big for Open Access publishing.

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~ ~ ~ ~ ~ ~ ~ ~ ~ ~

Franzen, J., Gingerich, P., Habersetzer, J., Hurum, J., von Koenigswald, W., & Smith, B. (2009). Complete Primate Skeleton from the Middle Eocene of Messel in Germany: Morphology and Paleobiology PLoS ONE, 4 (5) DOI: 10.1371/journal.pone.0005723

Murphy, W., Pringle, T., Crider, T., Springer, M., & Miller, W. (2007). Using genomic data to unravel the root of the placental mammal phylogeny Genome Research, 17 (4), 413-421 DOI: 10.1101/gr.5918807

There is a LOT of blogospheric and media coverage on this find. I was going to provide a list of links and then realized that there is only one good way to do this … I’m sending you here, to A Blog Around the Clock. Bora has every single link.

All of the images used above come from the original on line article.

Extinction of the Old, Evolution of the New: What really happened to the dinosaurs?

ResearchBlogging.orgMany years ago, a sudden event occurred that changed everything. Or at least, that is what we think now. But in truth, the event took longer than many today believe, and many of the specific details, the exact order of events, the actual meaning of each detail, are not fully understood. Indeed, in the process of describing this event today, we find considerable disagreement, or at least, it is clear that one person’s version is different than another’s. I’d be happy to give you my version of it. What qualifies me to do that? Well, for one thing, I was there when it happened…
Continue reading Extinction of the Old, Evolution of the New: What really happened to the dinosaurs?

A 300 million year old fish brain …

ResearchBlogging.org … has been found. Inside the fish’s skull, in fact. This is from a chimaeroid fish, which today are fairly rare but during the Carboniferoius were quite common and diverse. There are really two aspects of this find that are especially interesting. One is the 3D imagery that was obtained of the ancient fossilized brain, and the other is the analysis of the fish’s ear canals. The brain is cool just because it is cool (and shows some interesting morphology). The ear canal study is interesting because it shows a pattern different than expected for a fish: This creature was probably really good at keeping track of it’s position in the horizontal plane, but not the vertical plane. That is odd for a fish.

From the abstract:

…During Carboniferous times, 358-300 million years (Myr) ago, [the chimaeroids] underwent a remarkable evolutionary radiation, with some odd and poorly understood forms, including the enigmatic iniopterygians that were known until now from poorly informative flattened impressions. Here, we report iniopterygian skulls found preserved in 3 dimensions in â??300-Myr-old concretions from Oklahoma and Kansas. The study was performed by using [ a mixture of traditional and novel technologies, fancy software, and analytical techniques] which revealed their peculiar anatomy. Iniopterygians also share unique characters with living chimaeroids, suggesting that the key chimaeroid skull features were already established 300 Myr ago. Moreover [visualization] of an articulated skull revealed a strikingly brain-shaped structure inside the endocranial cavity, which seems to be an exceptional case of soft-tissue mineralization of the brain, presumably as a result of microbially induced postmortem phosphatization. This was imaged with exceptional accuracy by using holotomography, which demonstrates its great potential to image preserved soft parts in dense fossils.

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The anatomy of iniopterygians. (A) Reconstruction of Sibyrhynchus denisoni (based on ref. 5, not to scale). (B and C) Part (B) and counterpart (C) of a phosphatic nodule from the Pennsylvanian of Oklahoma (AMNH OKM38) containing the braincase and shoulder girdle of Sibyrhynchus sp. (D-F) Threedimensional reconstruction of the same specimen, obtained from conventional X-ray CT images, showing the braincase in dorsal (D), ventral (E), and lateral (F) view, with associated teeth. (G-I) Three-dimensional reconstruction of the braincase, shoulder girdle, and pectoral fin elements of a sibyrhynchid iniopterygian from the Pennsylvanian of Kansas (KUNHM 21894), based on SR- CT images. Braincase in dorsal (G), posterior (H), and ventral views, with articulated shoulder girdles and pectoral fin radials (I). (Scale bar, 5 mm; f.IX and f.X, foramina for glossopharyngeus and vagus nerves).

I quickly add that previous finds of soft tissue preserved have turned out to be something else. (See: The seductive siren of soft tissue preservation: Ancient dinosaur flesh wasn’t ancient. Or dinosaur flesh.)

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Braincase anatomy and exceptional brain preservation in a sibyrhynchid iniopterygian from the Pennsylvanian of Kansas. (A and B) Articulated skull preserved in a nodule (KUNHM 22060) (see also Fig. S1) in dorsal (A) and anterior (B) view (arrow points forward). (C-Q), Three-dimensional reconstructions and putative preserved brain structures of the same specimen, obtained from SR- CT images (and holotomography for brain details). (C-H), Braincase, teeth, and lower jaw in lateral (C), anterior (D), ventral (E), posterior (F), and dorsal (G) view, showing by transparency the outline of the endocranial cavity and labyrinth (H). (I-K), Selected transverse (I and J), and horizontal (K) SR- CT (holotomography) slices through the calcite-filled endocranial cavity, showing the probably phosphatized brain at the level of the rhombencephalon (I), hypophysis (J), and roof of the optic tectum and cerebellum (K). (L-N) Reconstruction of the endocranial cavity and otic capsule in dorsal (L and M) and lateral (N) view, showing the putative brain by transparency (M and N). (O-Q), reconstruction of the putative phosphatized brain in dorsal (O), ventral (P), and lateral (Q) view. (Scale bar, 5 mm for A-N and 1 mm for I–K and O-Q. Asc, anterior semicircular canal; Cer, cerebellum; Ed, endolymphatic duct; Hsc, horizontal semicircular canal; Hyp, hypophysis; Olftr, canals for olfactory tracts; Opch, optic chiasm; Optec, optic tectum; Psc, posterior semicircular canal; II, optic nerve; III?, oculomotorius nerve?; IV?, trochlear nerve?; X?, roots of vagus nerve?).

More information:
Continue reading A 300 million year old fish brain …

A most amazing set of spoor

Dino spoor, that is. A recently reported finding in PLoS ONE clarifies a number of questions about how certain dinosaurs held their front limbs (zombie/Frankenstein-position palm-down vs. huggie-wuggie palms-facing-each-other). This research confirms …

that early theropods, like later birds, held their palms facing medially, in contrast to … prints previously attributed to theropods that have forward-pointing digits. Both the symmetrical resting posture and the medially-facing palms therefore evolved by the Early Jurassic, much earlier in the theropod lineage than previously recognized, and may characterize all theropods.

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Figure 7 from the paper. Restoration by Heather Kyoht Luterman of Early Jurassic environment preserved at the SGDS, with the theropod Dilophosaurus wetherilli in bird-like resting pose, demonstrating the manufacture of SGDS.18.T1 resting trace.

ResearchBlogging.orgThe find is from southwestern Utah. In particular, the tracks were found in the Whitmore Point Member of the Moenave Formation (WP), which in turn is one of about nine or so formations that are exposed in Zion and Kolob canyons in Zion National Park. The WP Member itself is about 100 meters thick. The Moenave Formation and together with the Kayenta formation (just above it) are considered to be Lower Jurassic in age. The base of the Moenave formation is a disconformity caused when the basin was uplifted, and thus eroded, for about ten million years. Subsequent to this shallow seas to the north of this region repeatdly expanded or shifted into this area, and the sediments of the Moenave formatoi represent lake, river, and flood plain (river-side and beyond) sediments that were part of this sea basin.

Because of the constant (in geological time) shifts between environments, the Moenave Formation possesses layers bearing fossils and traces of a wide range of sediments. Within the WP Member itself, there are plant fossils in some of the lower layers, and fish fossils throughout. Dinosaur bones have been found in the upper most layer. But in many layers, from the lowest to nearly the uppermost, there at tracks. The tracks discussed in this paper are from the lower part of the formation.

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Figure 2 from the paper: Stratigraphic section of the Moenave Formation at the St. George Dinosaur Discovery Site at Johnson Farm. Resting trace and trackway SGDS.18.T1 is in the “Top Surface” of the Main Track-Bearing Sandstone Bed (indicated by the blue arrow) in the Whitmore Point Member of the Moenave Formation.

The reason that I’m pointing all of this out is to give an (accurate) impression of the significance of this basin (see this discussion). There are many hundreds of meters of sediment at Zion and other nearby locations (including the Grand Canyon) that tell the story of major changes in the landscape, and that preserve long, well represented records of life. Immense geological time is represented here, as well as the occasional brief and fleeting moments, like when some dinosaur lays down to rest and leaves behind an impression of its body, which happens, against all odds, to be preserved as a trace fossil. It is a paleontologists dream:

Twenty-five track-bearing horizons contained within a small area (1 km2) in St. George, Utah, contain a diverse, theropod-dominated ichnofauna. The most fossiliferous and diverse surface … is preserved within the St. George Dinosaur Discovery Site at Johnson Farm … museum. Mudflat, shoreline, and periodically submerged surfaces coincide on the same bedding plane as evidenced by mud cracks, ripple marks (current, symmetrical, wind-driven, interference, and wave-formed), erosive mega-ripples, load and flute casts, rill and tool marks of various sizes, raindrop impressions, and invertebrate and vertebrate ichnites. [an “ichnite” is a fossilized foot print.] This suite of sedimentary features formed on a beach or shoal along the shores of an Early Jurassic freshwater body (Lake Dixie) that underwent seasonal regressive-transgressive fluctuations. The majority of theropod trackways on this surface trend north-south, paralleling the paleoshoreline. The 22.3 m long SGDS.18.T1 trackway … includes the unique crouching traces….


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Figure 4 from the paper. Eubrontes trackway with resting trace (SGDS.18.T1) in the Whitmore Point Member of the Moenave Formation, St. George, Utah. A, Overhead, slightly oblique angle photograph of SGDS.18.T1 resting trace. Note normal Eubrontes track cranial to resting traces (top center) made by track maker during first step upon getting up. Scale bar equals 10 cm. B, Schematic of SGDS.18.T1 to scale with A: first resting traces (manus, pes, and ischial callosity) in red, second (shuffling, pes only) traces in gold, final resting traces (pes and ischial callosity) in green, and tail drag marks made as track maker moved off in blue. Note long metatarsal (“heel”) impressions on pes prints. C, Direct overhead photograph and D, computerized photogrammetry with 5 mm contour lines of Eubrontes trace SGDS.18.T1. Color banding reflects topography (blue-green = lowest, purple-white = highest); a portion of the berm on which the track maker crouched is discernible. Abbreviations: ic = ischial callosity, lm = left manus, lp = left pes, rm = right manus, rp = right pes, td = tail drag marks.

Because early Jurassic dinosaurs of the type that left these tracks had relatively undifferentiated feet, it is impossible to assign these tracks to species. The tracks themselves, grouped together from different locations but looking similar, form what is called an “ichnotaxon” … a species or set of species as represented by tracks of similar morphology. Indeed, when dealing with dinosaurs, perhaps we should say that a given ichnotaxon of this type may even represent a set of genera. The paper itself provides a lengthy discussion of this issue, if you want to delve into it.

The paper concludes that …

… other ostensible theropod manus [manus = front foot] prints are either dubiously attributable to theropods, dubiously made by the manus of a pes-print [pes = back foot] maker, or uninformative with regard to the track maker’s forelimb functional morphology. Because the crouching traces in the trackway [studies here] match the architecture of known theropods, we support the alternative interpretation that most, if not all, other prints showing manus impressions instead pertain to ornithischian or other non-theropodan dinosaurs or dinosauriforms with functionally tridactyl pedes. [This trackway] therefore includes the only unambiguous theropod manus impressions recognized to date and indicates that the avian orientation of the manus, with medially-facing palms, evolved very early within the Theropoda. Less parsimoniously, this posture evolved in immediate dinosaur ancestors; absence in other dinosaurs would thus constitute reversals.

The lack of marks in [this trackway] made by the distal thoracic and pelvic limbs and the ventral portion of the pelvis indicate that, while resting, even the earliest theropods adopted a modern ratite-like [bird-like] posture with the legs folded symmetrically beneath the body such that the weight of the body was distributed between each metatarsus and pes. … The clear symmetry of [this trackway] demonstrates that even some of the oldest, basal-most theropods engaged in this additional avian-style behavior, which therefore also evolved very early in the theropod lineage or was retained in theropods from pre-dinosaurian archosaurs.

Background and references:

Continue reading A most amazing set of spoor

How diverse were early hominoids?

And hominids.

We know the fossil record underestimates diversity at least a little, and we know that forested environments in Africa tend to be underrepresented. Given this, the diversity of Miocene apes may have been rather impressive, because there is a fairly high diversity in what we can assume is a biased record.

But I’d like to make the argument from another angle, that of modern ecological analogues. Let us assume that the greater apparent diversity of apes in the middle and late Miocene compared today can be accurately translated as a modern reduction in ape diversity. Not counting the relatively diverse lesser apes, there are five species (2 chimps, gorilla, human, orang) which can be further divided into 10 subspecies, across the entire old world.

Now look at the size range of all of the living apes. Gibbons are the smallest and gorillas the largest. When a family or subfamily of land mammal is diverse in a particular region (a biome or something larger than a biome) we tend to see that diversity played out along a spectrum of size, and against size we can find additional diversity derived from dietary or subhabitat differences and geography. It seems to me that there is room in the size spectrum between gibbons and chimps, and orangs and gorillas, and there is certainly room above the gorilla size as indicated by the existence in the fossil record of very large Asian forms.

We know that some of the later Miocene apes were bipedal, and it is starting to look like bipedalism or something like bipedalism is showing up among other apes in the Miocene as well. So perhaps there is a spectrum of locomotory pattern along which diversity may be spread.

This gives us a the following size classes: gibbon, siamang, [something in between], chimp, orang, [something in between], goriilla, [something bigger], or at total (a minimum?) of eight size classes across which apes might exist in a world in which apes are divers. Like the Miocene. If we add to this a more arboral form and a more bipedal form, perhaps we double the number, or perhaps we add about five new classes (I’m guessing that a Mighty Joe Young size ape would not have been bipedal!). This gives us about a dozen, conservatively estimated, niches when we divvy up size and so-called positional behavior.

To this we can add geography. It is probably reasonable to assume that a wetter, more forested middle and late Miocene Africa could be divided into at least four or regions, between the West/Central divide that modern biogeogrpahy tells us was effective at least in the Late Miocene, the Congo River divide, North/Central Africa, East Africa and Southern Africa. Let’s conservatively assume four, and let’s assume that only half (six) of the hypothesized ape species are divided among these areas. That means that 24 species are endemic to varoius regions, and six additional species are more widely spread for a conservative estimate of 30 species.

Among these species there may have been several bipedal forms, but only one of them (plus or minus a little hybridization hanky panky here and there) would have been the human ancestor. Of course, no one at the time suspected that …. (Or they probably would have done something about it.)

This is not an outrageous suggestion. The idea that if you went back in time to a more ape-rich time (and we know it was more ape-rich) and got a current copy of the Guide to the Mammals of Africa, the ape section would have a few dozen species, just like the monkey section or the antelope section today has a few dozen species.

Go apes!

Did Triceratops fight with their faces?

ResearchBlogging.orgOr, more accurately, did these dinosaurs either engage in intraspecific combat (such as territorial or mating contests among males) or fight predators such as Tyrannosaurs, like in the movies?

Well, one thing we know for sure: If any folklore, belief, or ‘fact’ related to a fossil species sits around long enough, eventually someone will come along and study it. This usually involves reformulating the idea as one or more testable hypotheses, then attacking the hypotheses … much like Tyrannosaurus might or might not have attacked Triceratops, to see if it can be killed, or alternatively, has the mettle to survive for a while longer.

And thus, science progresses.

So now we have a paper entitled “Evidence of Combat in Triceratops” by Farke et al, just out in PLoS ONE.
Continue reading Did Triceratops fight with their faces?

Amazing Fossil Finding: Proto Whales Gave Birth on Land, not at sea

ResearchBlogging.orgAn article released moments ago in PLoS ONE, by Gingerich et al., describes one of the more interesting fossil discoveries ever.

To cut right to the conclusion: We now have reason to believe that the proto-whale Maiacetus inuus, a true transitional form, gave birth on land, not in the water.
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Artist’s conception of male Maiacetus inuus with opaque skeleton overlay. Credit: John Klausmeyer and Bonnie Miljour, University of Michigan Museums of Natural History

Continue reading Amazing Fossil Finding: Proto Whales Gave Birth on Land, not at sea

The Fantastic Mystery of the Younger Dryas

One of the most interesting and exciting stories in science is that of the Younger Dryas. The Younger Dryas was a climate event that had important effects on human history, and that has been reasonably linked to some of our most important cultural changes, and ultimately some evolutionary changes as well. That is one reason why it is interesting. In addition, the Younger Dryas was a pretty big deal … a climate change or something like a climate change that caused massive changes all around the earth, and fairly recently. But the cause of the Younger Dryas is at present unknown, although a series of explanations have been advanced, each as convincing as the next depending on one’s point of view. The Younger Dryas itself is interesting, and the story of how scientists have studied it and the changing explanations emerging from that research is just as interesting.

The latest science is beginning to suggest that it is all even more interesting and exciting (and scary) than previously thought.

Continue reading The Fantastic Mystery of the Younger Dryas

Canadian Dinosaur Find: New Species?

ResearchBlogging.orgThe first dinosaur bones (that we know of) to have been discovered in British Columbia, Canada, are now being reported. These are bones found in 1971, eventually making their way to the Royal British Columbia Museum, and now being reported by V.M. Arbour and M.C. Graves. The bones were initially found by Kenny Flyborg Larsen, a geologist prospecting for thorium. He was drawn to these bones because the bones themselves are radioactive, and his instruments led him to them.(This is an update on this, as Arbour kindly sent me a copy of the original paper.) Continue reading Canadian Dinosaur Find: New Species?

Reconsidering the Reconstruction of the Pterosaur

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A very large Azhdarchid shown with a human for scale.
Azhdarchids were pterosaurs (flying reptile-like creatures) of the Cretaceous. These included some gigantic critters with up to a 10 meter wing span, but also some little ones (2.5 meters or so). Most reconstructions of these flying animals have them skim-feeding across the surface of bodies of water, grabbing near-surface animals with their beaks.A new paper in PLoS criticizes this view suggesting that there is very little evidence in support of it, and offers an interesting alternative interpretation of Azhdarchid morphology.From the abstract of the paper:

Azhdarchids lack the many cranial specialisations exhibited by extant skim-feeding birds, most notably the laterally compressed lower jaw and shock absorbing apparatus required for this feeding style. … Taphonomic data indicates that azhdarchids predominately inhabited inland settings … We argue that azhdarchids were stork- or ground hornbill-like generalists, foraging in diverse environments for small animals and carrion. Proficient terrestrial abilities and a relatively inflexible neck are in agreement with this interpretation.

Continue reading Reconsidering the Reconstruction of the Pterosaur

Earliest Known Abalone Discovered

May 18, 2008 — A tiny abalone specimen 5.9 mm in length and approximately 78 million years old (putting it in the middle Campanian Stage of the Late Cretaceous) has been documented from rocks in the Garapito Creek area of Topanga Canyon, Los Angeles County by Lindsey T. Groves and John M. Alderson of the Natural History Museum of Los Angeles County in the latest issue of the molluscan journal The Veliger.

i-2ff8eef8584f461eace66b36bef1b550-abalone.jpg Continue reading Earliest Known Abalone Discovered