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Important Dates and Cool Creatures in Earth History – Focus on Kentucky
Numbers shown for eons, periods, and epochs in the following list are in millions of years before the present, and are based on the International Stratigraphic Commission's 2003 time chart. Eons are the largest subdivisions of time, then periods, then epochs. Relative ages of important dates and creatures are also in millions of years before the present.
Links to references for material in this list can be found at the KGS earth history web site.
(beginning of Precambrian time)
- 4,600 Beginning of the Earth based on data from meteorites.
- 3,800 Oldest age-dated rocks on the present surface of the Earth.
- 3,500 Fossil evidence of cyanobacteria, also called blue-green algae. These cellular organisms lived in large mounds, called stromatolites. Stromatolites dominated the world for the next 2 and a half billion years.
(latter part of Precambrian time)
- 1,750 Oldest fossil evidence of single-celled life with a nucleus (eukaryotes).
- 1,500 The oldest multi-celled (metazoan) organisms, based on fossils, were algae.
- 1, 100 Inferred time when a north-south-oriented rift (tear in the earth's crust) started in what is now central Kentucky . Basaltic lavas were extruded into the rift. The lava and rift-filling sediments are now buried thousands of feet beneath the surface.
- 670 Ediacara fossil site. Famous locality in Australia , in which soft-body impressions of primitive marine invertebrate (lacking a backbone) life is preserved. Oldest fossil evidence of marine worms and jellyfish.
- Age uncertain During the late Precambrian or during the early Cambrian a second period of rifting began in Kentucky . This time the rift (tear in the earth's surface) was oriented in an east-west direction. One rift was in western Kentucky and became a feature geologists call the Rough Creek Graben. The second, in eastern Kentucky , became the Rome Trough. Both features were filled with thousands of feet of Cambrian and younger sediments.
Cambrian Period (542 to 488 million years ago)
- 542 Abundant fossil evidence of invertebrate life throughout the world, sometimes termed the “Cambrian Explosion” because of the sudden appearance of diverse fossils in rocks of this age. During much of the Cambrian, Kentucky was covered by shallow seas and probably looked much like the Bahamas today (without the palm trees, sea gulls, and fish!). We know about the rocks from drilling into the earth for oil and natural gas. Cambrian rocks are exposed at the surface in many of the states around Kentucky, including Virginia and Tennessee . Trilobites and brachiopods are the most common fossils in these rocks.
- 530 Oldest fossil vertebrates, which are also the oldest fossil fish. The fossil Myllokunmingia was found in China . It was a small fish, about the size of a sardine, but had no jaws.
- 515 Burgess Shale organisms. Famous fossil locality in Canada in which soft parts of marine invertebrate organisms were preserved. Sponges and trilobites were common. The top predator in the world was a 2-foot long marine arthropod called Anomalocaris , from the Burgess Shale.
Ordovician Period (488 to 443 million years ago)
- 488 Invertebrate (no backbone) fossils of sea life are common in Ordovician rocks because much of North America, including Kentucky , was covered with shallow seas. Trilobites and brachiopods were still common. Cepahlopods, which were squids that lived in long shells, became common.
- 480 Taconic mountain-building event in eastern North America . Formed an early mountain chain in what is now the Appalachians, but prior to the Appalachian mountains we know today. This mountain-building event lasted for 40 million years.
- 470 Oldest fossil evidence of land plants. The first plants looked like lichen. These plants probably did not reach Kentucky for some time, since Kentucky was mostly covered by shallow seas during the Ordovician.
- 470 Approximate age of the oldest rocks exposed at the surface in Kentucky along the Kentucky River . These rocks are composed of limestone and contain abundant brachiopods, bryozoans, cephalopods, trilobites, and gastropods; all indicating that Kentucky was covered by shallow seas.
- 450 Bentonite beds in Ordovician strata of central Kentucky and surrounding states indicate that there were large volcanic eruptions in the southern pre-Appalachian mountains, which spread ash as far west as South Dakota. In Kentucky , the ash fell into a shallow sea.
- 440 End-Ordovician mass extinction. Continental glaciation in the southern hemisphere triggered global climate changes and falling sea levels, which caused global extinctions. An estimated 60% of life went extinct.
Silurian Period (443 to 416 million years ago)
- 443 Silurian rocks outcrop in Kentucky around the Knobs region. These limestones and dolomites indicate that shallow marine seas covered the state during the early part of the Silurian. Trilobites, brachiopods, and corals are common fossils. Silurian strata, however, were partly eroded prior to deposition of Devonian rocks in Kentucky, indicating that Kentucky was land during the latter part of the Silurian.
- 438 Large coral reefs flourished and coral fossils are common.
- 428 Oldest fossil evidence of vascular land plants, Cooksonia . Vascular plants have internal tissues for exchanging liquids and gases. Vascular tissue also provides internal support so plants could begin to grow up off of the ground. These primitive plants had no leaves and were less than an inch (1-2 cm) tall.
- 428 Oldest fossil land animal, the millipede Pneumodesmus from Scotland . Scorpions also lived on land by the late Silurian.
- 419 Eurypterids (called “sea scorpions”) were common from the late Silurian into the Devonian. The largest was Pterygotus from New York , which grew to nearly 6 ft in length.
Devonian Period (416 to 359 million years ago)
- 416 The Devonian is called “The Age of Fishes.” Many different types of strange-looking fish became widespread.
- 412 Oldest fossil insect, Rhyniognatha, from Scotland . The earliest insects were small springtails, also called bristletails. Rhyniognatha has what have been interpreted as support structures for wings, which means that it may have been able to fly, although no wings were found on the fossil.
- 412 Approximate age of oldest lungfish (dipnoans). The fossil Powichthys (a proto-lungfish) from North America, and Youngolepis and Diabolepis from South China are all from the Early Devonian.
- 410 Acadian mountain building on the eastern coast of North America, formed another mountain system in what is now the Appalachians . This mountain-building event lasted for 30 million years.
- 409 Oldest fossil shark, Doliodus from New Brunswick , Canada . These ancient sharks had spines that stuck out of their back in front of their pectoral fin. Fossil shark's teeth have been found in Mississippian and Pennsylvanian strata in Kentucky (younger than the oldest fossils).
- 400 Approximate age of the main fossil beds at the Falls of the Ohio in Louisville . Fossils at the Falls are from both the late Silurian and Devonian periods. Coral fossils are most common, including large horn-shaped (rugose) corals. Brachiopods, clams, sea snails, and trilobites are also found.
- 400 Coral fossils are common, especially horn corals. Many animals lived among the corals including bony fish called arthrodires.
- 395 Rhynie Chert fossil Beds. This famous fossil locality includes preservation of primitive land plants and small arthropods (crustaceans and spider-like trigonotarbids) that were living and dieing in a geyser basin.
- 380 Oldest fossil large trees and therefore, forests. Fossil trunks of the tree Eospermatopteris are known from Gilboa , New York . Spider-like trigonotarbids, centipedes, spiders, mites, and wingless insects are also known from this site.
- 380 Oldest fossil spider, Attercopus fimbriungus , from the Devonian
- 375 Oldest fossil amphibian, Acanthostega , from Greenland Also, the oldest evidence of land vertebrates.
- 375 Oldest trees with bark (woody tissue) and leaves, Archaeopteris. Fossils of these logs have been found in Kentucky . The Kentucky fossils appear to be logs that floated into the shallow seas from land to the east in what is now Virginia , Pennsylvania , and New York . On land, in areas east of Kentucky, the deep roots of forest trees changed the Devonian land landscape, by promoting soil formation, stabilizing the ground, and increasing photosynthesis, which changed the earth's carbon cycle, which may have led to another glaciation.
- 370 In Kentucky , the seas deepened across much of Kentucky during the latter part of the Devonian. Thick, black shales accumulated in the seas, which later became the source for most of the oil and natural gas produced in Kentucky today.
- 370 Armored fish called arthodires ruled the seas throughout the Devonian. The largest, Dunkeosteus, lived near the end of the Devonian and grew to lengths of 25 feet. Their heads were covered with bony armor and at their mouths the armor had large, hook-like protrusions that acted as teeth. Fossil evidence from Ohio suggests that they ate sharks! Arthrodire bones have also been found in Kentucky .
- 360 End-Devonian mass extinction. Another period of continental glaciation in the southern hemisphere triggered global climate changes and falling sea levels, which caused global extinctions. An estimated 70% of life went extinct.
Carboniferous Period (European term which equals the combined Mississippian and Pennsylvanian Periods in the United States )
Mississippian Period (359 to 318 million years ago)
- 360 In Kentucky , shallow seas once again covered most of the State. Brachiopods, crinoids, and corals are common fossils. Screw-shaped, Archimedes bryozoan fossils are also common. Primitive shark teeth and starfish fossils have also been found. Thick limestones were deposited including the limestones in which Mammoth Cave was formed (although the cave didn't form until much later, in the Quaternary Period).
- 359 Corals and crinoid fossils are common.
- 340 Deltas from eastern shores began to build outward into the shallow seas, covering the Mississippian limestones with thick muds and silts. These are exposed at the surface in the Knobs region of Kentucky .
- 330 Oldest fossil evidence of conifers, seed-bearing plants with cones.
- 330 East Kirkton fossil site, England . This famous fossil site included the bones of many fish, lungfish, amphibians, and a reptile-like animal, once thought to be the oldest reptile.
- 330 Toward the end of the Mississippian, continued delta building, and a drop in sea-level turned the area that is now Kentucky into a coastal plain. In fact, sea-level fluctuated numerous times toward the end of the Missisippian.
- 330 Oldest fossil tetrapod (4-legged) vertebrates in Kentucky . Several amphibians, called embolomeres, have been found in western Kentucky . The amphibians died in estuarine channels and swamp lakes along the ancient late Mississippian coastline.
Pennsylvanian Period (318 to 299 million years ago)
- 318 A major drop in sea level caused the seas to withdraw to the edge of the continent, and rivers to cut deep valleys in what is now Kentucky . The deep valleys filled with conglomeratic sandstones. These conglomerates, form the cliffs at many of Kentucky 's most scenic parks including Natural Bridge and Cumberland Falls (although these features weren't formed until much later).
- 315 Kentucky continued to occupy a coastal position during most of the Pennsylvanian. Broad swamps were common, and peat from these swamps was buried, ultimately becoming Kentucky 's coal seams. Sea-level fluctuations resulted in numerous rises and falls in sea level and more than 50 coal seams in eastern Kentucky . Common fossils include plant fossils like ferns, reeds like Calamites, and large swamp trees called lycopods .
- 315 Oldest fossil evidence of reptiles. Hylonomus was a small lizard-like reptile that was trapped in the trunk of a swamp tree in what is now Nova Scotia , Canada .
- 315 The largest land-arthropod of all time, Arthropleura , a 5 ft (3.8 m) long, millipede-like giant, which lived in the same swamps. Giant dragonfly-like insects were also common.
- 315 Oldest evidence of flying insects (unless Devonian Rhyniognatha had wings) Fossil wings on giant mayflies, dragonflys, and dragonfly-like arthropods make these the oldest definite evidence of flight in nature.
- 315 Alleghenian mountain building. This mountain-building event resulted from the collision of what is now Europe with eastern North America . The event lasted through the Permian, and formed the Appalachian mountains in eastern North America .
- 315 A reptile trackway from McCreary County , Kentucky , is one of the oldest evidence of reptiles in the world. It is on display at the University of Kentucky .
- 311 A volcanic ash fall covered the eastern part of Kentucky , burying part of a peat swamp that would become the Fire Clay coal bed, one of the most productive coal seams in eastern Kentucky .
- 307 Some of the most widespread coal-forming swamps in earth history stretched across Kentucky into surrounding states, including the peat swamp that became the Springfield coal in western Kentucky , our state's most productive coal seam.
Permian Period (299 to 251 million years ago)
- 299 During the Permian, many of the earth's continents began to collide. Global climates were dryer. Mammal-like reptiles, called synapsids, became the dominant large land animals. Sail-backed synapsid reptiles like Dimetrodon and Edaphosaurus are characteristic. They may have used their sales for display to attract a boyfriend or girlfriend, or for controlling their body temperature.
- 299 Permian rocks are mostly missing from Kentucky . They are preserved in an igneous dike and in a single fault block in western Kentucky . Preservation of Permian strata in nearby states indicates that Kentucky was mostly land, and that dryer climates began to replace the equatorial humid climates that dominated the Pennsylvanian.
- Age uncertain. At some time near the end of the Pennsylvanian or in the Permian, Appalachian mountain-building resulted in the formation of Pine Mountain . Pine Mountain was formed when part of the earth's crust in what is now Virginia was pushed westward up and over what is now eastern Kentucky.
- Age uncertain. At some time after Pine Mountain was formed, but before the Quaternary Period (1.81 million years ago), a meteorite collided into eastern Kentucky forming the Middlesboro basin. The age of the impact is uncertain because the crater and any material ejected from the crater have long since been eroded. All that remains is the broken rock with evidence of intense pressure and rings of faults, which once were deep beneath the original impact site.
- 270 Glossopteris trees become the dominant vegetation on the southern continents, their fossils provide evidence that they were connected.
- 267 Intrusion of an igneous dike in Elliott County , Kentucky . This is the only igneous rock at the surface in Kentucky . In the Permian, magma was injected into the dike, but did not reach the surface. The volcanic activity was part of Appalachian mountain-building. Erosion has exposed the dike at the present surface of our state.
- 260 Karoo Basin fossils from South Africa include a wide array of large land reptiles, including the dicynodonts. The largest Permian animal was Moschops , a 16 ft-long mammal-like synapsid reptile from South Africa .
- 251 A long history of continental collision result in the formation of the supercontinent, Pangea, which stretches nearly from the North to South Pole.
- 251 The End-Permian, also called the End-Paleozoic Extinction. The greatest mass extinction of all time. More than 90% percent of all life went extinct. Giant lava flows pored out of what is now Siberia and continental collisions destroyed many shallow marine areas.
Triassic Period (251 to 199 million years ago)
- 251 Life hangs on after the mass extinction. One hold-over, the synapsid dicynodont Lystrosaurus , is found on many continents and provides evidence that the continents were connected. Triassic rocks are missing from Kentucky, but information from nearby states suggests that Kentucky was probably land during the Triassic.
- 245 Reptiles diversify. Archosaurs (“ruling reptiles”) take to the air, sea, and land. One type of archosaur that was especially widespread in the Triassic were the thecodonts, a group of reptiles that were the ancestors of dinosaurs.
- 228 Oldest dinosaur fossil. Eoraptor was found in South America . This little dinosaur was a cat-sized meat eater.
- 225 Dinosaurs diversify. Fabrosaurus , Lesothosaurus , and Saltoposuchus are examples of early dinosaurs.
- 225 In the seas, dolphin-like marine reptiles called ichthyosaurs were common. Shonisaurus , from Nevada , was the largest, measuring 55 ft in length.
- 221 Oldest mammal fossils (they looked like shrews). Mammals remained small throughout the Mesozoic.
- 220 Petrified Forest National Park fossils contain a wide array of Triassic plant and animal life including the largest predatory animal of the day, the archosaur Postosuchus.
- 216 Dinosaurs continue to diversify. Coelophysis is an example from the American southwest. The oldest, large dinosaur fossil is Plateosaurus . Plateosaurs were the ancestors of the long-necked (sauropod) dinosaurs. They were called prosauropods.
- 210 Oldest turtle fossil, Proganochelys .
- 199 End-Triassic mass extinction. There appears to have been dramatic climate changes, which may have caused the extinctions. Large outpourings of lava from the break-up of Pangea, may have been a cause for the climate change. More than 50% of life, including all thecodonts and synapsids, went extinct.
Jurassic Period (199 to 145.5 million years ago)
- 199 Jurassic rocks are missing from Kentucky , but information from nearby states suggests that Kentucky was probably land during the Jurassic.
- 200 After the extinction, dinosaurs become the dominant large land animals.
- 195 Dilophosaurus is a good example of an early Jurassic dinosaur. It had twin bony crests on the top of its head, and was 20 ft long. This is much larger than it was shown to be in the Jurassic Park movies. Also, there is no evidence that it spit poison, as shown in the movies.
- 155 The oldest bird, Archeopteryx from the Solenhofen Limestone of Germany . This bird had many dinosaur characteristics, including a long tail, and reptile-like jaws with teeth. The same limestone contains fossils of dinosaurs and marine reptiles, including ichthyosaurs preserved with their babies.
- 150 Large, long-necked (sauropod) dinosaurs dominate the landscape. Apatosaurus , Brachiosaurus , and Diplodocus are good examples of late Jurassic long-necked dinosaurs. All are found in the western United States .
- 150 Seismosaurus was one of the longest long-necked (sauropod) dinosaurs, and possibly the largest land animal of all time, with an estimated length of 125 feet.
- 150 Allosaurus and Centrosaurus are good examples of late Jurassic meat-eating (theropod) dinosaurs from the western United States . At 25 feet in length, Allosaurus was the largest meat eater of the Jurassic, which has led to it being called the “lion of the Jurassic.”
- 150 Stegosaurus was an armored, plant-eating dinosaur that shared the floodplains of the Western United States with Allosaurus and Diplodocus . Stegosaurus had sharp spikes on its tail and large bony plates on its back. The plates may have been used for display or for controlling its body temperature.
- 149 Liopleurodon was a giant marine reptile called a pliosaur, which lived in the Jurassic seas of Europe . Liopleurodon was the largest carnivorous (meat-eating) animal of all time.
Cretaceous Period (145.5 to 65.5 million years ago)
- 144 Cretaceous sediments are preserved in the Jackson Purchase area of western Kentucky . The sediments indicate that Kentucky was mostly land during the Cretaceous. Kentucky formed the eastern margin of a broad inland sea that covered what is now the Great Plains . No dinosaur fossils have been found in Kentucky , but they probably lived here, since they were common in other areas that were land during the Cretaceous.
- 142 Oldest flowering plants (angiosperms). Angiosperms are seed plants that dominate the world today (deciduous trees, grasses, etc.). The oldest, Archaefructus was a submerged wetland plant, found in China . By the mid-Cretaceous (120 to 130 million years) lily pads, Nypa palms, and magnolias had developed.
- 110 Sauroposiedon , a long-neck (sauropod) brachiosaur from Oklahoma , possibly the tallest animal of all time, at an estimated height of 60 feet.
- 105 Argentinosaurus , a long-neck (sauropod) titanosaur from South America, possibly the longest animal of all time, at an estimated 130 to 140 feet length.
- 100 Carnotaurus , a horned, meat-eating (theropod) dinosuar from South America , shown in Disney's Dinosaur movie. The fossil includes skin impressions of its face.
- 95 Spinosaurus was perhaps the largest meat-eating dinosaur, estimated to have been 45 to 50 feet long. It lived in Africa and may have used the 6-foot sail on its back for display (to attract a boyfriend or girlfriend) or to help this giant animal control its temperature. The only skeleton ever found was destroyed during World War 2.
- 84 Beginning of Laramide mountain-building in the western Untied States, which led to the formation of the Rocky Mountains . This mountain-building continued for more than 30 million years.
- 82 Duck-billed dinosaurs (hadrosaurs) were common like Corythyosaurus , Edmontosaurus , Lambeosaurus , Maiasaurus , and Parasaurolophus . Maiasaurs are examples of dinosaurs from which fossil nests, eggs, and baby dinosaurs have been found.
- 80 Protoceratops was an early shield-headed (ceratopsian) dinosaur. It was the first dinosaur discovered with fossil eggs. These eggs and nests were found in Mongolia in the 1920's.
- 80 Raptors (dromaeosaurs) are famous Cretaceous dinosaurs, which had large, hook claws on their feet. Velociraptor is the most famous because of the Jurassic Park movies, although the actual dinosaurs were much smaller than shown in the movies; about 3 feet high at the hip and 5 to 6 feet in length. The most famous Velociraptor is a skeleton preserved in combat with a Protoceratops from Mongolia , China .
- 75 Ceratopsian (shield-headed) dinosaurs were common in the late Cretaceous. Examples are Monoclonius , and Styrakosaurus . Triceratops, which lived at the end of Cretaceous, was the largest of its kind, reaching 30 feet in length. .
- 70 Two of the largest (longest, tallest, and heaviest) meat-eating dinosaurs of all time (which also makes them the largest land-dwelling carnivores of all time) lived at the end of the Cretaceous. In North America, Tyrannosaurus rex was king, in South America Giganotosaurus ruled. Both were 45-50 feet long.
- 70 The armored ankylosaurs (shield back and/or club tails) become the most heavily armored land-animals of all time. These plant-eating tanks were as much as 25 feet in length, but built low to the ground for optimal protection. Many had spikes that stuck out from their bone-covered bask. Ankylosaurus even had bony plates on its eyelids!
- 70 Giant marine reptiles ruled the inland seas throughout the Mesozoic but toward the end of the Cretaceous they were home to the largest turtle of all time, Archelon, which was 12 ft long. Mososaurs, a type of sea serpent, hunted the turtles and grew to 75 ft in length!
- 65 Pterasaurs, the flying reptiles of the Mesozoic reached their largest size with Quetzalcoatlus, which had a wing span of 40 ft. This was the largest flying animal of all time.
- 65.5 End-Cretaceous mass extinction. This extinction is also called the K-T extinction for the Cretaceous-Tertiary extinction (Cretaceous is spelled Kretaceous, hence “K” in german and latin). Huge amounts of lava erupted from India , and a comet or meteor collided with the Earth in what is now the Yucatan Peninsula of Mexico. No large animals survived on land, in the air, or in the sea.
Tertiary Period (65.5 to 1.81 million years ago). In Europe the beginning of the Cenozoic Era is called the Paleogene Period (65.5 to 23.03 million years ago)
Paleocene Epoch (65.5 to 55.8 million years ago)
- 65 Tertiary sediments are preserved in a small area around Kentucky Lake , in western Kentucky . Most of Kentucky appears to have been land during the Tertiary, and probably looked much as it does today, although the vegetation was different. Cypress swamps flourished along the Mississippi river embayment. These swamps formed lignites, a type of brown coal with low heating value.
- 65 Rapid increase in new species of fossil mammals after the extinction of the dinosaurs. Most early Cenozoic mammal fossils are small.
- 60 In South America, the Andes mountain chain began to form.
- 60 Oldest fossil rodents.
- 60 The creodonts, cat-like predators, including Oxyaena, from North America , were common.
- 57 Oldest hooved mammals, the condylarths, from North America . These were the ancestors of all hooved animals including pigs, deer, and cattle.
- 57 Coryphodon , a pantodont, was the largest Paleocene mammal.
Eocene Epoch (55.8 to 33.9 million years ago)
- 55 Oldest (definite) fossil primates, Teilhardina, from Europe, North America, and Asia .
- 55 The unitatheres, like Unitatherium , become the largest land animals.
- 55 Oldest fossil horse, Hyractotherium , the oldest horse was tiny, about the size of a dog).
- 50 Oldest fossil elephants, an unnamed fossil from Algeria .
- 50 Green River Formation fossils from the western United States . This is where many of the fossil fish sold in stores come from.
- 50 India collided with Eurasia , resulting in the formation of the Himalayan mountains. This mountain-building event continued for millions of years.
- 49 Messel Quarry fossils from Germany . This famous fossil site was a lake in which many early Tertiary mammals died, including primitive horses and the oldest fossil bats. Many reptiles, amphibians, and fish also perished in the lake. A large otter-like animal from the Messel shales, called Ambulocetus , may be he ancestor of whales.
- 49 The largest meat-eating land animals of the Paleocene and Eocene epochs were flightless birds, like Diatryma from America , and Gastornis from Europe .
- 40 In Europe , the Alpine mountain chain began to form. This mountain-building episode lasted for millions of years.
- 40 Mid-Eocene weasel-like fossils of Miacis , the ancestor of dogs and bears.
- 37 Oldest fossil dog, the weasel-like Hesperocyon .
Oligocene Epoch (33.9 to 23.03 million years ago)
- 30 Indrictotherium was the largest land mammal of all time. It stood 18 feet high at the shoulder and lived in India .
- 30 Oligocene and Miocene mammal fossils are abundant from the Badlands of South Dakota. Some of the Oligocene mammals included brontotheres, rhinos, horses, oredonts, and camels.
- 25 Oldest fossil cat, Proailurus.
In Europe , the latter part of the Cenozoic is called the Neogene Period (23.03 to the present)
Miocene Epoch (23.03 to 5.33 million years ago)
- 20 Grasslands become widespread in the warmer, dry climates of the Miocene. It is hard for most people to imagine, but prior to the Miocene, ground cover was dominated by small ferns and other plants, rather than grasses.
- 15 The largest shark of all time, Carcharodon megalodon lived during the Miocene and Pliocene. It may have been 40 feet in length.
Pliocene Epoch (5.33 to 1.81 million years ago)
- 5 The Pliocene was a time of global cooling, which led to ice build ups at the poles and culminated in the Ice Ages.
- 4 Australopithecus , the oldest hominid (human-like ancestors) fossils from Africa . Many different species from 4 million to 1.1 million years ago.
- 3 Closing of the isthmus of Panama and connection of North and South America through central America.
- 2.5 to 1.5 Homo habilis , a hominid from Africa that made crude spear points.
- 2.4 Arctic glaciation begins. For the next 2 million years ice sheets would advance and retreat across the northern continents.
- 2.4 Marks the beginning of what archeologists call the Paleolithic Age
Quaternary Period (1.81 million years ago to the present)
Pleistocene Epoch (1.81 to 0.015 million years ago)
- 1.8 Quaternary sediments are preserved in river sediments, caves, and sinkholes thoughout the State. Throughout the Quaternary, Kentucky looked much as it does today, except at times it was much cooler.
- 1.2 Homo erectus , the oldest evidence of hominids outside of Africa .
- 1.0 First of many ice ages in North America . Thick, glacial ice sheets covered the northern parts of North America . These are the great Ice Ages. Wooly mammoths, wooly rhinos, mastodons, ground sloths, and ice age buffalo roamed the plains in front of the advancing ice. In the U.S. , the last ice sheet, called the Wisconsinan, extended south to the present-day position of the Ohio River . In fact, melting of that glacial ice sheet, created the river valley. Sediments from the melt water were deposited throughout northern Kentucky . When you drive north of the river and see the flat landscape of Indiana and Ohio , you are looking at the result of erosion from the glaciers.
- 0.50 Neandertal man, Homo sapiens neandertalis . This Ice Age human lived in Europe during the Ice Age and went extinct approximately 35,000 years ago when the last continental glaciers retreated.
- 0.09 Cro-Magnon (modern) man, Homo sapiens sapiens, coexisted with neanderthals, but survives to the present day.
- 0.06 The last of the great North American Ice Ages (Wisconsinan) begins
- 0.05 Age uncertain, but close to the time when fossil mammoth, mastodon, giant ground sloth, and Ice Age bison bones were buried at Big Bone Lick, in northern Kentucky. Baron Georges Cuvier, a French scientist, used bones from Big Bone Lick as evidence for the theory of extinction. Benjamin Franklin and Thomas Jefferson also studied fossils from Big Bone Lick, Kentucky .
- 0.04 Sabre-tooth cats, mammoths, American lions, and dire wolves were trapped in the La Brea tar pits from 40,000 to 10,000 years ago, in what is now downtown Los Angeles, California.
- 0.03 Estimated age of a fossil peccary (wild pig) herd found in western Kentucky . These wild pigs appear to have been buried in a slump or slide of glacial material called loess.
Holocene Epoch (0.015 million or 15,000 years ago to the present)
- 0.01 Beginning of what archeologists term the Mesolithic Age
- 0.006 Beginning of what archeologists term the Neolithic Age
List compiled by Stephen Greb, Kentucky Geological Survey
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