Beautifully illustrated, thoroughly researched, and very accessible popular and academic work on when Kansas was covered by an ocean. Specifically, it is on a 5-million-year span of time during the Late Cretaceous, the time when the Smoky Hill Chalk was deposited on the bottom of the Western Interior Sea, roughly 87-82 million years ago. This chalk is accessible in many locations in Kansas and is the most thoroughly studied of any period of the Cretaceous in Kansas. The book chronicles the history of fossil collecting in the chalk (occurring since the late 1860s), the history of the study of the fossil organisms in the Smoky Hill Chalk, the animals that called the sea home (from invertebrates to reptiles and birds), what we know of conditions in the Western Interior Sea and how they changed over time, and what study of this region tells us about the wider Mesozoic world both before and after and in other areas of the world. The book is richly illustrated with black and white and mainly color photographs of fossils from the Smoky Hill Chalk and has a series of gorgeous color plates of various life reconstructions of the sharks, bony fish, birds, pterosaurs, and most of all marine reptiles of the Western Interior Sea, all by the amazing Dan Varner. Though the book is primarily on the Smoky Hill Chalk, the younger Pierre Shale is discussed some (as for instance, the first major Cretaceous fossil from Kansas and the type specimen of Elasmosaurus platyurus came from the Pierre Shale).
Chapter 1, the introduction, begins with a fictionalized account of a day in the life of a mosasaur in the Inland Sea, beginning a tradition for each subsequent chapter starting with a fictionalized depiction of the fish, reptiles, and birds of the Western Interior Sea. The chapter goes on to introduce the reader to general information on the Western Interior Sea (the water was probably less than 600 feet deep for instance, and the name of the chalk derives from the Smoky Hill River, which gets its name from the Smoky Hills in eastern Kansas, though the chalk itself is important in mostly the western third of Kansas).
Chapter 2, “On Discovery of the Western Interior Sea,” discusses the earliest days of fossil hunting in the Smoky Hill Chalk, beginning with the Lewis and Clark expedition in 1804 and goes on to discuss the Sternbergs, most particularly Charles H. Sternberg, the famous fossil hunter of the Smoky Hill Chalk, Cope and Marsh’s “Bone War” competitions for the marine fossils of Kansas, and closes with a discussion of early studies of biostratigraphy (a subject collectors decades paid little if any attention to for decades, with many times specimens lacking even good locality data).
Chapter 3, discusses invertebrate, plant, and trace fossils of the Western Interior Sea. Topics covered include the giant inoceramid clams of the ocean bottom (reaching diameters of 5 feet), what life was like on the sea bottom (often quite low in oxygen), the numerous leaf fossil imprints from the Dakota Sandstone of the early part of the Late Cretaceous, ammonites (their shells rarely occur in the chalk and most often only their impression remains), belemnites, squid (Tusoteuthis longus), colonial and free-living crinoids (the only echinoderms of the chalk, in genus Uintacrinus), fossilized pearls, coprolites (primarily from sharks and mosasaurs), and fossil wood, sometimes showing openings made by borings of Teredo clams.
Chapter 4 is on sharks. An important part of the chapter is how many bone fragments and other fossils from the Smoky Hill Chalk show evidence of shark predation or scavenging in terms of bite marks, broken tips of embedded shark teeth, and/or weathering showing that the bone was at least partially digested by a shark, perhaps later coughed up. Lots of photos of shark teeth fossils that are found in the Smoky Hill Chalk (at their greatest variety in the lower half of the formation), a discussion of “shark mummies” that were found, and the main species of sharks found such as the ginsu shark (Cretoxyrhina mantelli) and several species of ptychodontid sharks that most likely fed on clams and other hard-shelled prey due to their “pavement” toothed upper and lower jaws. Also, some discussion of the decline of sharks as mosasaurs increased in numbers, size, and diversity, a point revisited later on in the book as well.
Chapter 5 is on “Fishes, Large and Small,” with the star being the famed “fish within a fish” fossil, the nearly 14 foot long Xiphactinus audax fossil that died shortly after having swallowed Gillcus arcuatus, a fish about half its length, though other fishes are also discussed as well, such as fish of the family Saurodontidae, which had a predentary bone projecting forward from the lower jaw (perhaps used like the beak of a modern swordfish), Cimolichthys nephaholica, one of the more common species of fish preserved in the chalk and appears to have been a medium sized predator like a barracuda, and Protosphyraena gladius, a enormous filter feeder fish that was probably about 15 feet in length. The author noted that after shark teeth, fish fossils are the most common vertebrate fossils in the Smoky Hill Chalk and that perhaps 80 to 90% of the fossils seen in the field are fish (though as they are so common, are less often collected and make up about 60% of the fossils in museum collections).
Chapter 6 is on turtles, a group that was apparently heavily preyed upon and is most often known from skulls and isolated limb material or shell fragments, with most of the current research being done on turtles of genus Protostega. The famous and enormous Archelon is known to have existed in the Western Interior Seaway, but rocks of the age that could have contained their remains in Kansas were apparently exposed and eroded away millions of years ago. There is a nice discussion and illustration of a Protostega gigas turtle that was apparently killed but not consumed by a 30-foot Tylosaurus proriger.
Chapter 7 is on elasmosaurs, a wonderfully written chapter discussing the history of the discovery and study of them, elasmosaur gastroliths, the various types of plesiosaurs (the giant pliosaurids, extinct before the formation of the Smoky Hill Chalk, the short-necked polycotylids, and the extremely long-necked elasmosaurs), a fascinating discussion of how elasmosaurs moved and hunted, how they gave birth and possibly protected their young, and how thanks to the Late Cretaceous explosion of mosasaurs, may have been driven to the edge of extinction as mosasaur numbers and diversity increased.
Chapter 8 is on pliosaurs and polycotylids. I had heard of pliosaurs, but polycotylids were new to me and were fascinating to read about, once lumped in with all the other short-necked, large-headed pliosaurids, but beginning in the mid-1990s, it was determined (assuming it is correct according to the author) that Late Cretaceous short-necked pleisosaurs are more closely related to elasmosaurs than to the pliosaurids.
Chapter 9 is in some ways the heart of the book, the chapter the author in my opinion was the most passionate and knowledgeable about, and pretty much worth the price of admission, that being a chapter on mosasaurs (I think it is the longest chapter too). Mosasaurs 100 million years ago, just into the second half of the Cretaceous, went from shore dwellers to ocean dwellers and within a short amount of time evolved so they could no longer leave the water. Though hardly the first reptile of course to reenter the ocean, “they were probably the most successful in terms of their diversity, large numbers, and eventual domination of the marine environment,” and though they appeared to have caused the extinction or decline of several species of sharks and the decline of plesiosaurs and were so successful they appeared to be invading freshwater environments as well, they too for reasons unknown went extinct at the end of the Cretaceous along with the dinosaurs, plesiosaurs, and pterosaurs.
Lots to read in the chapter on mosasaurs, from the history of the discovery of the fossils and the study of these animals, discussion of locomotion, raising their young, their anatomy, ecology, how big they got (several lineages reaching more than 50 feet in length), how they were spreading and specializing throughout the world, and how some were adapted not to eat fish or anything else swimming they could catch but instead for crushing the hard shells of clams and other shellfish.
Chapter 10 is on “Pteranodons, Rulers of the Air,” with Pteranodon longiceps joining Tyloaurus proriger as signature fossils of not only the Smoky Hill Chalk but of Kansas as a whole, with both first discovered in Kansas and occurring mostly in Kansas and both (with the author’s help) becoming co-State Fossils in 2014. Though Pteranodon is the star, there is a good bit of discussion of Nyctosaurus with its bizarre head crests. Lots of discussion of the history of the fossils finds, their study, theories on how these animals flew, how they took off, what they ate (and what we know of what they ate thanks to fossil remains), and why their fossils would turn up in the middle of the ocean, hundreds of miles from land.
Chapter 11 is titled “Feathers and Teeth” and is on the toothed birds of the Smoky Hill Chalk, namely the flying (possibly diving too) Ichthyornis (“fish bird”) and the much larger and flightless and likely unable to go far at all on land, Hesperornis (“western bird”), a bird that successfully competed with the plesiosaurs, mosasaurs, fish, and sharks, though the author discusses how the fossil evidence shows they may have been more common in cooler, northern waters. There are brief mentions of other fossil birds, Baptornis advenus, Baptornis varneri (named after Dan Varner, the chief artist on display in the book), and Fumicollis hoffmani.
Chapter 12 is on the few dinosaur fossils known from the Smoky Hill Chalk, five sets of remains discovered since 1871, two of which are hadrosaur remains and the rest belong to nodosaurs, all discussed at length, with possibly the first two nodosaur specimens might actually belong to the same individual animal.
Chapter 13, “The Big Picture,” shows the Western Interior Sea and what it was like, all of its fauna, during the 5-million-year span of the Smoky Hill Chalk, with the author further breaking down what the fauna was like in three shorter periods, the late Coniacian (a period of about 1.2 million years), the entirety of the Santonian (about 2.3 million years), and the beginning of the Campanian (about 1.5 million years), with in charts and descriptive text the author noting the appearance and disappearance of species of clams, ammonites, squid, sharks, bony fish, the various marine reptiles, pterosaurs, and birds as well as noting general conditions of the ocean and of deposition conditions.
The final section of text is the epilogue, discussing what happened to the Western Interior Sea and the author discussing that while the Chicxulub impact may have been a factor in Mesozoic mass extinctions, he discusses for a few pages why he thinks it “would have happened anyway,” as “[w]hatever killed off the marine reptiles and the dinosaurs of the Late Cretaceous was a far more complex mix of environmental problems than just a big rock falling out of the sky,” noting in passing that the Manson impact, creating a crater 22 miles across, that occurred 10 million years before Chicxulub and caused some local devastation appears according to the author based on “the size and condition of the elasmosaur and the large number of other species that were collected (mosasaurs, fishes, invertebrates), it certainly appeared to me that life in the sea was back to normal” by the time of Chicxulub.
Following this is an extensive section of references and a thorough index. A few sections could get a little technical with the terms used to describe different bones or their appearance and structure and with the scientific names, but I was never lost. I found the style of writing engaging and really enjoyed the fictionalized accounts of life in the Western Interior Sea. The author also made the human story of fossil hunting and studying the fossils interesting and included a number of first-hand accounts of his and his colleague’s work out in the field and in museums. I loved how he showed many fossils revealed a lot about life in the Western Interior Sea by what in fact was fossilized and I also loved how he showed trends in study of the fossils and exciting new areas of research. The book is lavishly illustrated and probably is one of the finest popular paleontology books anywhere for color photos of a wide variety of marine fossils.