Archive for the 'Paleontology' Category

100 Years 100 Objects: Merychippus

The Houston Museum of Natural Science was founded in 1909 - meaning that the curators of the Houston Museum of Natural Science have been collecting and preserving natural and cultural treasures for a hundred years now. For this yearlong series, our current curators have chosen one hundred exceptional objects from the Museum’s immense storehouse of specimens and artifacts—one for each year of our history. Check back here frequently to learn more about this diverse selection of behind-the-scenes curiosities—we will post the image and description of a new object every few days.

This description is from Dr. Robert Bakker, the museum’s associate curator of paleontology. He’s chosen a selection of objects that represent the most fascinating fossils in the Museum’s collections, that we’ll be sharing here – and at 100.hmns.org/ – throughout the year.

CHI_7740Folks stop and stare at our fossil horse. It is cute in a coltish way, all gangly and long-legged. And it is dynamic – rearing up as if it just saw you and was whinnying a “Hello!”

But sharp-eyed visitors take a second look. Our Merychippus demands a digital double-take. Count the toes. There’s one big hoof on each foot, as there should be. It’s a horse, of course. The French word is “solipede,” meaning “Single Toe Foot.” Today, among all animals domestic and wild, horses and only horses have just the single, solitary toe to run on.

Wait – look closely. There’s more. Our Merychippus has too many toes. There are extra digits, little ones, on the inside and outside of the main hoof. The mini-toes have hoofs too but they’re narrow and pointed.

I imagine I’m petting our Merychippus along its muzzle, like I do to my neighborhood ponies. And I’d feel another odd thing – Merychippus has a more delicate, lightly-built face and nose. If you stare at the fossil, you see a row of molar teeth far smaller than any horse-owner would expect.

Those small molars and accessory digits tell a story that’s literally earth-shaking. Back in the 1870s, Merychippus and the other three-toed horses shattered the scientific status quo. The side-toes made Archbishops fume and fuss and get red in the face. German philosophers smiled and puffed their pipes with satisfaction.

You see, Merychippus proved that Darwin was right. Click here to read the full story.

Wander among prehistoric beasts in the Paleontology Hall, a permanent exhibition at the Houston Museum of Natural Science.

You can see more images of this fascinating artifact – as well as the others we’ve posted so far this year – in the 100 Objects section at 100.hmns.org.

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100 Years – 100 Objects: Ankylosaurus

The Houston Museum of Natural Science was founded in 1909 - meaning that the curators of the Houston Museum of Natural Science have been collecting and preserving natural and cultural treasures for a hundred years now. For this yearlong series, our current curators have chosen one hundred exceptional objects from the Museum’s immense storehouse of specimens and artifacts—one for each year of our history. Check back here frequently to learn more about this diverse selection of behind-the-scenes curiosities—we will post the image and description of a new object every few days.

This description is from David Temple, the museum’s curator of paleontology. He’s chosen a selection of objects that represent the most fascinating fossils in the Museum’s collections, that we’ll be sharing here – and at 100.hmns.org/ – throughout the year.

CHI_4415One of the oldest displays in the Houston Museum of Natural Science is the full scale recreation of the dinosaur Ankylosaurus. This recreation of a late cretaceous herbivore was created by the Sinclair Oil Company for the exhibit “Sinclair Dinoland” which opened at the 1964-1965 Worlds Fair in New York.

Dr. Barnum Brown acted as a consultant to world renowned zoological sculptor Louis Paul Jonas to create a paleontological menagerie of dinosaurs that would showcase the Dinosaurs of the Mesozoic. This would be the end of Dr. Barnum Brown’s long paleontological career and association with Sinclair oil as he died shortly before the fair opened in 1964.

The dinosaurs were created at Louis Paul Jonas Studios and then transported to the fair grounds past New York City on a flat barge in a brilliant and surreal publicity stunt. In addition to carrying the Sinclair banner at national stops by train and flatbed trucks, the dinosaur sculptures were used by Sinclair in other advertising campaigns, such as the print ad you see here, featuring the Houston Ankylosaur advertising the dinosaurs and the Dinoland exhibit.

After the closing of the fair, the models toured the country on specially constructed flatbed trailers. Visiting Houston in 1966 and 1968, the nationwide tours attracted millions of visitors. One of the Houston visits was to Gulfgate Mall- the first shopping mall in the city. The second was to HMNS. The Museum, newly expanded in 1969, had empty space and the popularity of these visits was not lost on Museum staff.

The Jonas Dinosaur menagerie was conceived as being an outdoor exhibit, and after the fair and all the national tours, all but two of the sculptures in the collection ended up as open air exhibits. The Houston Ankylosaurus remained indoors and, though modified, it is perhaps the best preserved of the Sinclair Dinoland models.

Learn more about the ankylosaur: check out David’s post “Ankylosaur at HMNS: A 40-year mystery solved” Or, wander among prehistoric beasts in the Paleontology Hall, a permanent exhibition at the Houston Museum of Natural Science.

You can see more images of this fascinating artifact – as well as the others we’ve posted so far this year – in the 100 Objects section at 100.hmns.org.

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Find Fun Fossils at Dino Days 2009! This Saturday

dinoDaysJoin us Saturday, Nov. 7 for HMNS Dino Days, a family paleo festival that features fossil related activities and arts and crafts. Museum paleontologist Robert “Bob” Bakker will be on hand to answer any of your dinosaur questions.

This is a great chance for enthusiasts of all ages to come learn and discuss dinosaurs. We encourage you to bring in your own rocks, fossils, and other unique objects for identification. While you are here, take some time to help our volunteers sift through soil to recover bone fragments, teeth, and claws spanning 287 million years of natural history. Some of the Cretaceous age sediments you can sift through come from Texas and may contain fossilized shark teeth – and if so, finders keepers!

C. chubutensis 2
Creative Commons License photo credit: reed_flickr

So come join us this Saturday for an afternoon of dinosaur fun from 11 a.m. to 3 p.m. The activities are included free with your museum admission.


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Ice Age Extinctions and Dino-Plagues

About a year ago Dr. Bakker wrote a post about the different extinction periods that killed off the dinosaurs, mammoths, and saber-tooths. Recently, one of our readers asked some very thoughtful questions. R. Richards asks,  “How long would it take for this lethal concoction of plagues to do significant damage to a variety of species? Even with multiple pathogens and mutation allowing cross species infections it would have to take quite some time for this scenario to run its course among all of the different fauna.” (To see the full comment, click here.)

Dr. Bakker has taken this opportunity to write a follow-up blog, and hopefully answer any more questions that our faithful readers might have.

Thanks for the nuanced and provocative thoughts about dino-plagues and dino-extinctions.

I’ll discuss the time-line of extinctions first. Then, in a follow-up blog, I’ll talk about body size and rebound after an extinction.

The question here is: When dino-style extinctions happen, do the die-offs occur everywhere in the world at the same time?

IMG_4957
Creative Commons License photo credit: Javier Paredes

The most recent extinction event is the Ice Age die-offs, and these extinctions do offer help in interpreting the terminal Cretaceous disaster among dinosaurs. The “Asteroid Theory” predicts that extinction should happen almost instantly – in a matter of weeks or months after the impact. We have an excellent fossil record for what happened when a land bridge permitted exchange between North and South America just as the Ice Age began. South America had been an isolated island continent that evolved its own unique large herbivores and carnivores, very different from what North America had. If the Immigrant Plague Theory works, we should see episodes of extinction that coincide with episodes of mingling of faunas, North and South.

We do. The first pulse of die-off happened when North American mammal carnivores began to invade South America, towards the end of the Pliocene about 3 million years ago. The South American native carnivores suffered right away. The giant carnivorous ground birds died out almost completely and the giant marsupial predators disappeared. The invasions were not all one sided. Some South American herbivorous maxi-fauna did invade North America – giant ground sloths came up in great abundance. And one species of killer ground bird made it to Florida.

Mastodon
Creative Commons License photo credit: BryanKemp

A second pulse happened as mastodons, deer and other Northern large herbivores invaded South America. Several native South American herbivore clans disappeared.

The third round of extinctions happened 15,000 to 10,000 years ago, when all the native South American big mammals went extinct. Humans entered South America about this time. At the same event all the biggest invaders too died out – gone were mastodons and saber-tooth cats that had come across the Panama land bridge from the North. In North America, the saber-cats, mastodons and mammoths died out along with the ground-sloths that had invaded from the south.

The entire Ice Age extinctions, world wide, took over three million years. They did not happen all at once, everywhere.

WLA-HMNS-Triceratops
Creative Commons License photo credit: gwenturnerjuarez

The final dino-die offs were also complicated. You see the beginning of the crash in North American diversity about 72 million years ago, in the Horseshoe Canyon Fauna. Only a very few big dinosaurs have large numbers. In the Lancian Fauna, 67 to 65.5 million years ago, we still have some dinosaurs but only two herbivores are common: Triceratops and Edmontosaurus. Then, at 65.4 million years ago, all the remaining big dinos go extinct.

These pulses of dino die-offs probably coincide with pulses of faunal interchange among the continents.

Conclusion: the Cretaceous dino extinctions were complicated in time and space. They did not happen suddenly all over the globe.

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