The Pleistocene- Vertebrate Fossils from Mississippi Gravel Bars Dr. Nina L. Baghai-Riding

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The Pleistocene- Vertebrate Fossils from Mississippi Gravel Bars Dr. Nina L. Baghai-Riding. The Pleistocene Epoch lasted from about 1.65 million until 10,000 years ago. Much of northern North America was covered by a large ice sheet. - PowerPoint PPT Presentation

Transcript of The Pleistocene- Vertebrate Fossils from Mississippi Gravel Bars Dr. Nina L. Baghai-Riding

  • The Pleistocene- Vertebrate Fossils from Mississippi Gravel Bars

    Dr. Nina L. Baghai-Riding

  • The Pleistocene Epoch lasted from about 1.65 million until 10,000 years ago. Much of northern North America was covered by a large ice sheet. Continental glaciers extended in Illinois and northern Missouri

  • Extent of ice sheets during the coolest glacialperiod, Cutchins and Johnston, 2000). More than 18 million square kilometers of ice covered North America

    The center of the ice sheet was about 3 km (almost 2 miles) thick.

  • Sea-levels were much lowerGreat Lakes and Finger Lakes were formed.In the southeastern United States there were pine-hardwood forest similar to that of the modern Great Lakes as well as oak forests, prairies, and swamps.

  • Compare the various vegetational zones 18.000 years ago to the present

  • The world of the ice ages is much more familiar to us than any other geological time Pleistocene epoch

  • Most spectacular components of the Pleistocene are large animal bones of mammals.Age of the Cavemen, mammoths, and saber-toothed cats.

  • Mammoths were the dominate fauna of the Irvingtonian.They grazed on grasslands and steppes in the Arctic (Prothero, 2006). They had huge grinding molars that could crush almost any vegetation. Their molars look like a shoe with deep treads.

  • Mammoths came across the Bering land bridge from Eurasia to North America at 1.9 Ma\Three different species: Columbian Mammoth, Woolly Mammoth, and Jeffersons MammothBering Land Bridge in orange connected Alaska to Siberia. This area is currently under water.

  • Mammoth localities - common in areas that were covered by savannas, grasslands, or tundra during the last Ice Age.

  • About 50% of the new genera immigrated from South America and 27% from Asia during the Irvingtonian--Great Animal Interchange (Cutchins and Johnston 2000).

  • Other mammals that first appeared ~ 1.9 ma1. Sabertoothed cat (Smilodon)2. hares (Lepus)3. jaguars4. shrub oxen (Euceratherium)119 genera of Irvingtonian mammals (Savage and Russell, 1983).

    North America was known for the American mastodons (Mammut americanum)

  • Mastodon molar from Danny West collection - note its simple molar with conical rounded cusps.

    Forest animals

  • American mastodon was about 3 meters (10 feet) at the shoulder, with slightly curved tusks,One tusk usually was longer than the other indicating feeding and behavioral preferences.Tusks were used to pry on bark and branches and broke them into pieces.Preferred spruce forests

  • Other important large herbivores:Equus - One-toed horsesTapirs found in forested parts of the landscapeMylohyus - Long nosed peccaryPlatygonus flat skulled peccarySeven species of camels and llamas including PalaeolamaVariety of deer and elkPronghornsMusk oxen - Soergilia

  • Preying on the herbivores were:HyenaUrsus - Black bearArctodus huge short-faced bear the top predator in North America and the largest carnivore that ever lived.Smilodon sabertoothed catCanis dirus - Dire wolf - heavily built, short-limbed predator

  • Other animals during the Ice AgeLepus haresBatsSquirrelsBeavers including the giant beaver Castoroides ohioensis about 2.5 m long and weighed almost the size of a bear.Moles, hamsters, porcupines

  • Rancholabrean 300,000 10,000 years ago marks the climax of the Ice Age Mammal assemblage in North America.Bison came in during this time from EurasiaBison latifrons - huge bison that had horns that spanned 2 m in width.Other Eurasian immigrants came in including the musk oxen, moose, reindeer, new rodents.

  • Numerous large mammals occurred in the Midwestern United States below the ice sheetDate between 40,000 and 10,000 years ago (the last Ice Age). Most of these animals no longer live in the United States and are extinct.Sites older than 40,000 years old are less common than younger sites.

  • Giant tortoises and strange glyptodonts the size of a car occurred in the underbrush.Glyptodont from FossilTreasures of Florida-com

  • Giant ground sloths 4.5 m (15 ft) tall reaching for leaves to eat. Weighed close to 5,000 lbs (2,267 kg).Four species inhabited the United States.They spent all of their time on the groundThe shape of their hip bones indicates that they could stand up on their hind legs. This would allow them to reach high up into trees for the best leaves and twigs.

  • Ground sloth had blunt teeth (Specimen from Danny West collection).

    Huge claws and powerful arms were used to break and bend branches

  • The Lower Mississippi River region served as an important ecological resource for many land-dwelling and freshwater animals.

    Grassland habitats and forests prevailed - dominant presence of large grazing animals (bison, mammoth, horse, and stag moose).

    Tapirs (cow-sized) could swim, wallow in mud, and hide in dense vegetation.

  • Giant Ice Age Beaver Probably an excellent swimmerHuge version of the modern-day beaver. 8 ft or 2.4 m long from its nose to the tip of its tail Its teeth possibly were used to uproot water plants instead of cutting down trees.Probably did not build dams

  • The Lonnie Looper Ice Age fossil vertebrate collection is being acquired by Delta State University.This collection contains 545 well-preserved cranial and post-cranial elements of various land grazers, browsers, carnivores, and estuarine animals that inhabited the Lower Mississippi River Delta.18 different semi-permanent gravel bars (collecting sites) bordering woodlands along the Mississippi River throughout northwestern Mississippi and southeastern Arkansas.

  • The collection was obtained over a 5-year period (1990-1995).

    Specimens are all well- preserved and documented as to site and location (river mile markers and longitude and latitude).

    Productive localities are Catfish Point, Henrico Dikes, and Montgomery Island in Desha Co., AR, and Rosedale Gravel Bar, Bolivar Co, MS.

  • Each specimen has a collector number and date of collection.There is no other collection that so adequately represents the late Pleistocene life from this region. Some specimens represent rare documentations of the existence of various mammals in North America.

  • Specimens appear not to have moved far from their source.Limb and toe bonesJaws and Teeth (incisors, canines, molars)Vertebrae, Horn Cores

  • List of taxa contained in the Looper CollectionFish unidentified speciesReptilesCaudochelys crassiscutata Giant Land TortoiseTurtles fluvial speciesBirds unidentified species MammalsArctodus simus Great Short Faced BearBison sp. Ancient BisonBootherium bombiforns Musk OxCastor canadensis modern beaverCastoroides ohioensis Giant Ice Age Beaver

  • Cervaices scotti Stag MooseEuarctos americanus American Black BearEquus complicates Fossil HorseEquus sp.Mammut americanum American MastodonMammuthus primigenius Mammoth Megalonyx jeffersonii Giant Ground SlothOdocoileus virginianus Whitetail DeerPaleolama mirifica LlamaPlatugonus compressus Flat Headed PeccaryTapirus haysii TapirTapirus veroensisTrichechus manatus Manateeunidentified large and small carnivores

  • Vertebrate elements in the collectionHerbivores are dominant and carnivores are rareDominant herbivores:Fossil bison (129)Whitetail Deer (126)Fossil Horse (115)American Mastodon (32)Giant Ground Sloth (23)About half of the horse elements are teeth.No isolated teeth are known from the whitetail deer.Only about a dozen bison teeth

  • Complex palmate antlers

    Similar lifestyle to a modern moose Preferred mires and other wetlands environments such as spruce parklands Stag moose the name implies that it is cross between an elk and a moose. Actually it was a large deer.

  • Bootherium bombifrons - Woodland Musk Ox (note red dots on the map as to where specimens have been found). Lived in woodlands and plains

  • Carnivores/ predators Great Short-faced bear (1)Dire wolf (1)American Black Bear (1)

    Dire wolf - Had a larger head and bigger teeth than any past or present member of the wolf family - Hunted in packs- A crushed skull was found on the Rosedale Gravel Bar.

  • Great Short-faced bear - Regarded as the most powerful predator in North America during the Pleistocene.- Stood 8-10 ft (2.4 3 m) tall on its hind legs.- Canine teeth were suited for puncturing tough hide- Large, jagged molars were exceptional for gnawing, tearing, and slicing meat.

  • A lower jaw was found on The Bar in Desha Country, Arkansas.

  • The Great short-faced bear was believed to become 13,400 years ago as the result of competition with invading brown bears (including the grizzly bear) that are also predatory in nature. Range of Great short-faced (

  • The manatee is believed to have migrated up the Mississippi River. This is the second reported occurrence of manatee from the interior of North America during the Pleistocene (the other occurrence is from the Ohio River drainage basin in Ohio) .Manatee Unusual find

  • A right radius-ulna of a manatee was found on the Ludlow Bar, Phillips Co., AR near Rena Lara, MS. Length of the ulna is 139 mm; the radius is 114 mm.

  • Reasons for this diverse assemblage:During the Late Pleistocene there was a wide land bridge betw