Explore the vast range of titles available.

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.

The Vallès-Penedès Basin (Catalonia, Spain) is a classical area for the study of the Miocene land mammal faunas and includes one of the densest and most continuous records in Eurasia. Furthermore, it is the type area for the Vallesian European land mammal age. After decades of study a huge amount of bio- and magnetostratigraphic data have been collected, allowing an unprecedented dating accuracy. Here we provide an updated local biostratigraphy for the late Aragonian, Vallesian and Turolian of the Vallès-Penedès Basin. This new biostratigraphic scheme is almost exclusively based on fossil rodents, which are the most abundant and one of the best known mammal orders in the area. Our proposal represents a significant refinement compared to previous attempts and provides a formal diagnosis and description of each zone, as well as clear definition of boundaries and a reference locality and section. The chronology of zone boundaries and main bioevents is based on detailed magnetostratigraphic data. The defined biozones allow for the correlation of the sites without associated magnetostratigraphical data. Finally, the correlation of the Vallès-Penedès local zones with other detailed local biostratigraphies, such as those of the Calatayud-Montalbán and Teruel basins (east-central Spain) is discussed. The sequence and chronology of the main bioevents is roughly comparable, although the rodent succession and the structure of the assemblage show important differences between these areas.

Science, the growth of reliable knowledge, became a major triumph of the European Enlightenment in the seventeenth century, under the guise of 'natural philosophy': investigating what the earth and universe are made of and how things work. It took another century for the parallel subject ‘natural history’ to glimpse how the earth, its geography and its richly diverse life came to be. Later, geology and biology became intertwined as biogeohistory—an ever-changing environmental theatre hosting an ever-changing evolutionary play. This environmental theatre has shifted with the making and breaking of supercontinents, the birth and death of global oceans, and the rise and fall of global hothouses and ice ages. The evolutionary play begins with biostratigraphy, wherein fossils revealed deep time and ancient environments and built the first meaningful geological timescale, and ends with the still young science of palaeoceanography—central to which are microfossils, rich in information about the oceans and climates of the past. In Southern Limestones under Western Eyes, Brian McGowran recounts the history of biogeohistory itself: the ever-changing perceptions of rocks, fossils and landscapes, from the late 1600s to the present. McGowran’s focus is southern Australia, the north shore of the dying Australo-Antarctic Gulf, in an era bracketed by two catastrophes: the extinction of dinosaurs and the emergence of humans.

New excavations in Liang Bua, where the remains of the ‘Hobbit’ ( Homo floresiensis ) were discovered, show that this diminutive human species used this cave between 190,000 and 50,000 years ago, and not until as recently as 12,000 years ago as previously interpreted; modern humans have been present in Australia since around 50,000 years ago, so whether Homo floresiensis survived long enough to witness the arrival of modern humans is still an open question. An earlier date for Homo floresiensis The discovery in Liang Bua cave on the island of Flores in Indonesia of the diminutive Homo floresiensis , an archaic member of the human family commonly known as the 'Hobbit', was an archaeological sensation in 2004. A source of considerable debate was the fact that it lived in Liang Bua cave between 95,000 and 12,000 years ago, after modern humans had colonized the area (around 50,000 years ago). Thomas Sutikna and colleagues — including many of the original research team — have gone back to Liang Bua, where new excavations have exposed previously unexplored parts of the cave. They have found that the layers of sediment in the cave are not deposited evenly, and it now seems that the H. floresiensis -bearing strata are older than was thought. New radiometric dating places the H. floresiensis remains and stone artefacts to between 190,000 and 50,000 years ago. Whether H. floresiensis survived long enough to witness the arrival of modern humans is an open question. Homo floresiensis , a primitive hominin species discovered in Late Pleistocene sediments at Liang Bua (Flores, Indonesia) 1 , 2 , 3 , has generated wide interest and scientific debate. A major reason this taxon is controversial is because the H. floresiensis -bearing deposits, which include associated stone artefacts 2 , 3 , 4 and remains of other extinct endemic fauna 5 , 6 , were dated to between about 95 and 12 thousand calendar years (kyr) ago 2 , 3 , 7 . These ages suggested that H. floresiensis survived until long after modern humans reached Australia by ~50 kyr ago 8 , 9 , 10 . Here we report new stratigraphic and chronological evidence from Liang Bua that does not support the ages inferred previously for the H. floresiensis holotype (LB1), ~18 thousand calibrated radiocarbon years before present (kyr cal. bp ), or the time of last appearance of this species (about 17 or 13–11 kyr cal. bp ) 1 , 2 , 3 , 7 , 11 . Instead, the skeletal remains of H. floresiensis and the deposits containing them are dated to between about 100 and 60 kyr ago, whereas stone artefacts attributable to this species range from about 190 to 50 kyr in age. Whether H. floresiensis survived after 50 kyr ago—potentially encountering modern humans on Flores or other hominins dispersing through southeast Asia, such as Denisovans 12 , 13 —is an open question.

The first introductory palaeontology text which demonstrates the importance of selected fossil groups in geological and biological studies, particularly in understanding evolutionary patterns, palaeoenvironmental analysis, and stratigraphy. Part one explores several key concepts, such as the processes of fossil preservation, the determination of evolutionary patterns, and use of fossils and statigraphical tools. Part two introduces the main fossil groups of value in these applied fields. Part three concentrates on the examination of important case histories which demonstrate the use of fossils in diverse practical examples. Evolutionary studies, palaeoenvironmental analysis, and stratigraphical applications are documented using up-to-date examples supported by overviews of the principles.

Conventional and varietal heavy mineral studies of the earliest Eocene Hermod S2 Member (Mbr) sandstones in the Greater Alvheim area of the northern North Sea have revealed marked lateral variations and more subtle vertical evolution in provenance signature. Major variations are of geographic rather than stratigraphic nature as biostratigraphy reveals that all investigated sandstones are coeval. The provenance variations show an organized pattern, with sandstones in the north showing a different signature than those in the south. The position of the sandstones relative to the East Shetland Platform (ESP) is inferred to be the main control on provenance, with sediment input from at least two different point sources. Sediment supplied from both catchments is predominantly recycled in nature, given the mineralogical maturity of the heavy mineral assemblages, consistent with the evidence for widespread Permo-Triassic and Devonian sediments on the ESP. However, some direct supply from metasedimentary (Moine and Dalradian) basement is implied by the sporadic occurrence of unstable minerals. The southern catchment incorporated a greater exposure of Permo-Triassic sandstones than the northern catchment. The Permo-Triassic part of the catchment can be reconstructed as comprising equivalents of the Foula and Otter Bank sandstones present to the west of Shetland, with the majority of the Foula section having been stripped off prior to Hermod S2 deposition, exposing Otter Bank equivalents for erosion and redeposition. However, remnant Foula-like sandstones remained exposed further south on the ESP until at least the earliest Eocene since Foula-type garnet signatures are found in the Forties Sandstone Mbr of the central North Sea. In addition to lateral differences, stratigraphic evolution of provenance can also be detected in the Hermod S2 Mbr, with variations in key provenance-sensitive parameters related to a sea-level rise that reduced the extent of alluvial storage and altered the geological framework of the hinterland.