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Oceans of Kansas: A Natural History of the Western Interior Sea by Michael J. Everhart Indiana Univ. Press, 2005 332 pp., $39.95

Last winter, while traveling by train just south of the Arkansas River in Kansas, I was fortunate to observe one of the most scenic areas in the state. White-tailed deer and wild turkeys were numerous in the vegetated areas bordering the river. Except for the exclusion of the American bison, this area looked a lot like it did when the first settlers entered the state. Most students of natural history are familiar with the terrestrial plant and animal communities that were present on the Great Plains when this region was settled. Prairie grasses and herds of bison stretched as far as the eye could see. By the 1870s, the hide hunters and the cowboys had arrived, and the flora and fauna of the Great Plains was altered forever. The human history of this period is well-known. Most people know that Kansas was an "ocean of grass" before the introduction of modern agriculture in the state. What many people do not realize is that Kansas was covered by a shallow ocean for many millions of years. In his book, Oceans of Kansas, Michael Everhart introduces his readers to the creatures that flourished in this realm.

The shallow sea that covered Kansas and most of the interior of North America in the Cretaceous Period is known as the Western Interior Sea. The Cretaceous Period is the last geologic time period in the Mesozoic Era (the Mesozoic runs from roughly 250 million to 65 million years ago). During this period, dinosaurs dominated the terrestrial landscape.

Everhart devotes much of his book to a description of the history of the organisms that were preserved in the Smoky Hill Chalk geologic deposit, created when the sea was at its deepest and a chalky mud was deposited on the sea floor over a five-million-year time span between 87 and 82 million years ago. Later, the chalk was buried under several hundred feet of shale when the sea receded at the end of the Cretaceous. The uplift of the Rocky Mountains and the Great Plains to the east exposed these chalk and shale layers to erosion, and today the Smoky Hill Chalk is exposed in the northwestern part of the state. Everhart describes the faunal component fossilized in this chalk in the context of the changing environmental conditions of the Western Interior Sea.

To give readers a sense of how we arrived at our present knowledge of the Western Interior Sea—and to convey the all-too-human side of science—Everhart recounts the history of paleontological discovery in the region. The first fossil from this ancient sea was found by the Lewis and Clark Expedition in 1804 along the Missouri River in what would later become northwest Iowa. The explorers misidentified the fossil as a large prehistoric fish; it was actually that of a mosasaur, a large aquatic reptile. Everhart describes the contributions of Benjamin F. Mudge of the Kansas Geological Survey, who began the first scientific collection of fossils from the Western Interior Sea. He also details the early paleontological finds in Kansas that occurred along the construction route of the Kansas Pacific Railroad. Many military posts were located along this railroad, and the military doctors stationed at these posts were the most educated men in the region and some of the region's first paleontologists. They sent many of the fossils back East for identification by paleontologists such as Joseph Leidy, Othniel Charles Marsh, and Edward Drinker Cope. Discoveries made in the Smoky Hill Chalk led to fierce rivalries between paleontologists, who were vying to name the new species found in this deposit. The rivalry between Marsh and Cope began with the unearthing of these Kansas fossils, a precursor to the "Bone Wars" that flared up when fossilized dinosaur bones were discovered in Colorado and Wyoming. Marsh and Cope would remain bitter rivals throughout their entire lives.

Everhart does a masterful job in organizing the book. After a detailed history of the discovery of the Western Sea, he devotes the following chapters to the principal faunal groups found in the sea: invertebrates, sharks, turtles, elasmosaurs, pliosaurs, polycotylids, mosasaurs, pteranodons, early birds, and dinosaurs. Most of these organisms were excavated from the Smoky Hills Chalk. In each of the chapters, he begins by describing a "Day in the Life" of these organisms, and in each case he takes some artistic license in describing how they interacted with other organisms and their environment. These reconstructions are based upon the physical clues that are preserved in the fossil record. For example, at the beginning of the chapter on sharks Everhart describes in vivid detail how a ginsu shark, Cretoxyrhina mantelli, might have attacked and devoured a large mosasaur (marine lizard). This predator-prey scenario is based upon evidence in the form of shark teeth imbedded in the fossil remains of many mosasaurs, and examples of partially digested, severed vertebrae.

Some of the organisms that lived in the Western Interior Sea are rather familiar—large marine clams, for instance, and sea turtles—while others are wonderfully strange. Among the latter are mosasaurs and elasmosaurs. These creatures were not dinosaurs but large marine reptiles. The mosasaurs, distantly related to Monitor lizards, were first described from fossils found in Europe (in the Netherlands) in the late 1700s. The discovery of these extinct organisms predated the discovery of the dinosaurs by almost 80 years. Mosasaurs were the dominant carnivores in the sea. They moved through the water by swishing their large tail back and forth in an undulating motion. The largest mosasaur, Tylosaurus proriger, grew to a length of over 10 meters. Not something that you would want to run into if you were snorkeling! The evidence in the fossil record shows that mosasaurs would feed on almost anything that was smaller than they were. Fossil remains also indicate that the mosasaurs were capable of giving live birth. The elasmosaurs—whose name suggests a quirky comic book superhero—had extremely long necks and four limbs that were developed into paddles, with which they "flew" through the water like modern penguins. They could reach lengths of 14 meters and fed principally on fish. The first Cretaceous vertebrate fossil that was found in Kansas in 1867 was an elasmosaurus, Elasmosaurus platyurus.

Everhart concludes with a chapter entitled "The Big Picture" and an epilogue, "Where Did It All Go?" In "The Big Picture" he lists the organisms that were present from the beginning to the end of the deposition of the Smoky Hills Chalk, dividing the chapter into the geologic stages that are preserved within this chalk. He describes the major environmental changes that occurred in each of these stages along with the changes in the diversity of the faunal life in the Western Interior Sea, taking account of extinction of organisms as well as diversification. Finally, in the epilogue he offers his perspective on the mass extinctions that took place in both the Western Interior Sea and on land at the end of the Cretaceous.

Entertainingly written and superbly illustrated, Everhart's book is an excellent introduction to the natural history of the Western Interior Sea. Readers whose appetite is whetted should check out Everhart's accompanying website, www.oceansofkansas.com.

Robert Reber is associate professor of Earth and Environmental Science at Taylor University.

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