William Smith is considered by many to be the Father of English Geology and is best rememberedfor his remarkable geological map of England and Wales, made in 1815.From an early date, Smith recognized that many of the strata which he showed on hismap were characterized by the fossils they contained. In 1816 he started a book called StrataIdentified by Organized Fossils which, although unfinished, was a fundamental work inestablishing the science of stratigraphy. In this book Smith figured fossils from each stratum.The fossil plates were exquisitely engraved by the renowned illustrator, naturalist and mineralogist,James Sowerby, from fossils provided by Smith.Although a brilliant geologist, Smith was an unlucky business man and because of hisprecarious financial position he was forced to sell his extensive fossil collection to the BritishMuseum. In William Smith's Fossils Reunited, the authors have included new photographs offossils from Smith's Collection, now housed at the Natural History Museum. These photographshave been arranged next to the original engravings, and in some cases, Smith's sketches.Smith's original texts for both Strata Identified and a later work Stratigraphical System ofOrganized Fossils, which catalogued the fossils, have been reprinted within the book. AsSmith roamed the English countryside collecting fossils he was careful to note the exactgeographical location of each fossil and also the rock layer from which it came. In this bookthese locations are shown on copies of Smith's own geological maps.With a Foreword by Sir David Attenborough, William Smith's Fossils Reunited is intendedboth for the William Smith enthusiast and also for those with a more general interest in thework of this remarkable pioneering geologist. The fossil illustrations and maps in this exquisitevolume are aesthetically pleasing in their own right and demonstrate the extraordinary skill ofearly nineteenth-century engravers and map makers.
This work weaves important strands of the paleontological literature into a coherent worldview that emphasizes the importance of understanding the geological record.
Finding Time for the Old Stone Age explores a century of colourful debate over the age of our earliest ancestors. In the mid nineteenth century curious stone implements were found alongside the bones of extinct animals. Humans were evidently more ancient than had been supposed - but just how old were they? There were several clocks for Stone-Age (or Palaeolithic) time, and it would prove difficult to synchronize them. Conflicting timescales were drawn from the fields of geology, palaeontology, anthropology, and archaeology. Anne O'Connor draws on a wealth of lively, personal correspondence to explain the nature of these arguments. The trail leads from Britain to Continental Europe, Africa, and Asia, and extends beyond the world of professors, museum keepers, and officers of the Geological Survey: wine sellers, diamond merchants, papermakers, and clerks also proposed timescales for the Palaeolithic. This book brings their stories to light for the first time - stories that offer an intriguing insight into how knowledge was built up about the ancient British past.
This textbook will appeal to students and graduates making their first steps in the application of both microfossils and stratigraphy. It presents, in detail, the historical development of microfossil biostratigraphy, from its birth to the emergence of sequence stratigraphy, including its roots in classical biostratigraphy. The interplay between the academic and economical challenges, on one hand, and developments in microfossil biostratigraphy, on the other, is explored thoroughly. The book also presents an introduction to the scientific concepts used in microfossil biostratigraphy practice, and the uses in microbiostratigraphy of 25 groups of microfossils, such as algae, protistans, reproductive plant debris, invertebrates, chordates and vertebrates, and microproblematica groups. It also provides a numerical method to calculate the biostratigraphical resolution of these microfossil groups.