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Books > Earth & environment > Earth sciences > Palaeontology
The plant fossil record provides evidence that the genus Metasequoia was widely distributed and experienced a wide range of climatic and environmental conditions throughout the Northern Hemisphere from the early Late Cretaceous to the Plio-Pleistocene. Today the genus is limited to one species with approximately 5,000 mature individuals growing in the Xiahoe Valley in southeastern China. This book is a distillation of the collective efforts and results of the worlda (TM)s Metasequoia specialists and enthusiasts. It is the most up-to-date and comprehensive reference source for the genus and the authors have sought to incorporate obscure, hard-to-get and non-English reference sources. The book reviews what is known about the biology, ecology and physiology of fossil and living Metasequoia, current research directions and problems that remain unresolved. This book presents a definitive overview of fossil and living Metasequoia and was written by sixteen of the worlda (TM)s experts on this important genus. Given the reality of increasing human pressure and the inevitability of global change, efforts to conserve this ancient genus are underway. This book will be of interest to botanists, geologists, paleobotanists, biogeographers, foresters, ecologists, paleoecologists, ecophysiologists, geochemists, climate modelers, geneticists, naturalists, science historians, and gardeners and will be useful as a supplemental text for advanced undergraduate and graduate level courses in paleoecology.
Although it is generally accepted that the Arctic Ocean is a very
sensitive and important region for changes in the global climate,
this region is the last major physiographic province of the earth
whose short-and long-term geological history is much less known in
comparison to other ocean regions. This lack of knowledge is mainly
caused by the major technological/logistic problems in reaching
this harsh, ice-covered region with normal research vessels and in
retrieving long and undisturbed sediment cores. During the the last
about 20 years, however, several international and
multidisciplinary ship expeditions, including the first scientific
drilling on Lomonosov Ridge in 2004, a break-through in Arctic
research, were carried out into the central Artic and its
surrounding shelf seas. Results from these expeditions have greatly
advanced our knowledge on Arctic Ocean paleoenvironments.
What would it be like to experience the ancient landscapes of the past as we experience the reality of nature today? To actually visit the Jurassic or Cambrian worlds, to wander among their spectacular flora and fauna, to witness their continental shifts? In Otherlands, the multi-talented palaeontologist Thomas Halliday gives us a breath-taking up close encounter with worlds that are normally unimaginably distant. Journeying backwards in time from the most recent Ice Age to the dawn of complex life itself, and across all seven continents, Halliday immerses us in sixteen lost ecosystems, each one rendered with a novelist's eye for detail and drama. Every description - whether the colour of a beetle's shell, the shambling rhythm of pterosaurs in flight or the lingering smell of sulphur in the air - is grounded in fact. We visit the birthplace of humanity on the shores of the great lake Lonyumun, in Pliocene-era Kenya; in the Miocene, we hear the crashing of the highest waterfall the world has ever known as it fills the evaporated Mediterranean Sea; we encounter forests of giant fungus nine metres tall in Devonian-era Scotland; and we gaze at the light of a full and enormous moon in the Ediacaran sky, when life hasn't yet reached land. To read Otherlands is to time travel, to see the last 550 million years not as an endless expanse of unfathomable time, but as a series of worlds, simultaneously fantastical and familiar.
In this deep examination of functional morphology, a renowned paleoanthropologist offers a new way to investigate human evolution through the fossil record. It is common for two functional anatomists to examine the exact same fossil material, yet argue over its evolutionary significance. How can this be? Traditionally, paleoanthropology has interpreted hominin fossil morphology by first considering the ecological challenges hominins faced, then drawing adaptive inferences based on the idea that skeletal morphology is largely a reflection of paleoecology. In Functional Inference in Paleoanthropology, innovative paleoanthropologist David J. Daegling suggests that researchers can resolve dichotomous interpretations of the fossil record by instead focusing on the biology and development of the bones themselves-such as measurable responses to deformations, stresses, and damage. Critically exploring how scientists probe and interpret fossil morphology for behavioral and adaptive inferences, Daegling makes the case that an intelligible science of functional morphology in the fossil record is impossible without the inclusion of this mechanobiological perspective. Drawing on historical examples from long-standing debates on the emergence of bipedality and the dietary shifts that facilitated the emergence of the hominin clade, Daegling traces the disjunctions between theoretical principles of comparative morphology and methodological practice in the paleontological context of human evolution. Sharing rich findings from recent decades of research in skeletal biomechanics, Functional Inference in Paleoanthropology examines how bone adapts over the lifespan, what environmental factors influence its quality, and how developmental constraints limit the skeleton's adaptive potential over evolutionary time.
Every day, in natural history museums all across the country, colonies of dermestid beetles diligently devour the decaying flesh off of animal skeletons that are destined for the museum's specimen collection. That time-saving process was developed and perfected at the University of Kansas Natural History Museum by Charles D. Bunker, a lowly assistant taxidermist who would rise to become the curator of recent vertebrates and who made an indelible mark on his field. That innovative breakthrough serves as a testament to the tenacity of a quietly determined naturalist. Bunker was part of the small team of men who constructed and installed the famous Panorama of North American Mammals, the centerpiece exhibit of the KU Natural History Museum located in Dyche Hall. That iconic building on the KU campus was expressly built to house the collection of mounted animals that impressed the world a decade earlier at the 1893 Chicago Columbian Exposition and World's Fair. Once the panorama was completed, Bunker turned his attention to field collecting. Bunker's field notes provide an accurate, authentic account of several expeditions to collect such specimens as well as a rare view of the extreme hardships of fieldwork in those early days. Perhaps most notable is “Bunk's” 1911 expedition to western Kansas, where he discovered the fossil remains of a forty-five-foot-long sea serpent—later identified as Tylosaurus proriger, an aquatic reptile from the mosasaur genus and the largest example of the species found in North America. In 2014, Tylosaurus was named the marine fossil of the state of Kansas. Birds, Bones, and Beetles tells the story of a man whose passion for learning led to remarkable discoveries, extraordinary exhibits, and the prestigious careers of many students he mentored in the natural sciences.
This work is a detailed study of people and plants in Little Dixie, a seven-county region of central Missouri. Based on three summers of field research, Professor Nolan combines ethnoscience with folklore to document what and why people know about wild plants in this little-known section of the American Midwest. The book is organized around the cognitive and behavioral differences between local experts and 'novices' who gather wild plant foods and medicines regularly throughout the seasons in Little Dixie. Ethnobotanical knowledge is described as an ongoing interaction between ecology and cognition, under constant modification by shifting cultural beliefs about edibility, efficacy, and sensory appeal. As consumable resources and symbols of belonging, wild plants are detailed with ethnographic context and vivid pen-and-ink sketches. Wild Harvest in the Heartland will appeal to a broad audience of anthropologists, ethnobotanists, folklorists, and ecologists, and will provide a welcome resource for naturalists, conservationists, and outdoor enthusiasts.
The present volume is the first in a series of two books dedicated
to the paleoceanography of the Late Cenozoic ocean. The need for an
updated synthesis on paleoceanographic science is urgent, owing to
the huge and very diversified progress made in this domain during
the last decade. In addition, no comprehensive monography still
exists in this domain. This is quite incomprehensible in view of
the contribution of paleoceanographic research to our present
understanding of the dynamics of the climate-ocean system. The
focus on the Late Cenozoic ocean responds to two constraints.
Firstly, most quantitative methods, notably those based on
micropaleontological approaches, cannot be used back in time beyond
a few million years at most. Secondly, the last few million years,
with their strong climate oscillations, show specific high
frequency changes of the ocean with a relatively reduced influcence
of tectonics. The first volume addresses quantitative methodologies
to reconstruct the dynamics of the ocean andthe second, major
aspects of the ocean system (thermohaline circulation, carbon
cycle, productivity, sea level etc.) and will also present regional
synthesis about the paleoceanography of major the oceanic basins.
In both cases, the focus is the "open ocean" leaving aside
nearshore processes that depend too much onlocal conditions. In
this first volume, we have gathered up-to-date methodologies for
the measurement and quantitative interpretation of tracers and
proxies in deep sea sediments that allow reconstruction of a few
key past-properties of the ocean( temperature, salinity, sea-ice
cover, seasonal gradients, pH, ventilation, oceanic currents,
thermohaline circulation, andpaleoproductivity). Chapters encompass
physical methods (conventional grain-size studies,
tomodensitometry, magnetic and mineralogical properties), most
current biological proxies (planktic and benthic foraminifers, deep
sea corals, diatoms, coccoliths, dinocysts and biomarkers) and key
geochemical tracers (trace elements, stable isotopes, radiogenic
isotopes, and U-series). Contributors to the book and members of
the review panel are among the best scientists in their specialty.
They represent major European and North American laboratories and
thus provide a priori guarantees to the quality and updat of the
entire book. Scientists and graduate students in paleoclimatology,
paleoceanography, climate modeling, and undergraduate and graduate
students in marine geology represent the target audience. This
volume should be of interest for scientists involved in several
international programs, such as those linked to the IPCC (IODP -
Integrated Ocean Drilling Program; PAGES - Past Global Changes;
IMAGES - Marine Global Changes; PMIP: Paleoclimate Intercomparison
Project; several IGCP projects etc.), That is, all programs that
require access to time series illustrating changes in the
climate-ocean system.
All of man's life is in some way associated with the plant world, from his food and shelter to his art, religion and language. The study of this all-pervading relationship between man and the plant world is called "ethnobotany." This book provides a systematic reconstruction of the ethnobotany of one of the hearths of American civilization, in the prehistoric cultures of the Peruvian Central Andes. As we learn more about the rise and spread of New World agriculture, it becomes evident that Peru was one of the sources of its development. Plants were cultivated here at least 2,000 years before the beginning of the Christian era. Village life was intimately bound up with this cultivation, later civilizations rested upon it as a foundation, and from Peru agriculture was diffused to other parts of the Americas. Towle bases her work on the evidence of plant remains found in archeological sites, surveys of botanical and ethnological literature, and field studies of modern plant utilization. After a methodological and historical introduction, she proceeds to a systematic listing of plant species, each fully described. She then presents the ethnobotanical data for each of the cultural-geographic divisions of the area, giving a chronological picture of the use of wild and cultivated plants against a background of the cultures of which they were part. A summary of the evolutionary trends in the region as a whole is followed by a full bibliography and index. The book contains fifteen pages of plates. "Margaret A. Towle" (1902-1985) received her doctorate from Columbia University in 1958 and was research fellow in ethnobotany in the Botanical Museum of Harvard University.
This book serves as an up-to-date introduction, as well as overview
to modern trace fossil research and covers nearly all of the
essential aspects of modern ichnology. Divided into three section,
Trace Fossils covers the historical background and concepts of
ichnology, on-going research problems, and indications about the
possible future growth of the discipline and potential connections
to other fields. This work is intended for a broad audience of
geological and biological scientists. Workers new to the field
could get a sense of the main concepts of ichnology and a clear
idea of how trace fossil research is conducted. Scientists in
related disciplines could find potential uses for trace fossils in
their fields. And, established workers could use the book to check
on the progress of their particular brand of ichnology. By design,
there is something here for novice and veteran, insider and
outsider, and for the biologically-oriented workers and for the
sedimentary geologists.
The Late Devonian and Permian-Triassic intervals are among the most
dynamic episodes of Earth history, marked by large secular changes
in continental ecosystems, dramatic fluctuations in ocean
oxygenation, major phases of biotic turnover, volcanism, bolide
impact events, and rapid fluctuations in stable isotope systems and
sea level. This volume highlights contributions from a broad range
of geological sub-disciplines currently striving to understand
these critical intervals of geologically rapid, global-scale
changes.
Molluscs comprise the second largest phylum of animals (after arthropods), occurring in virtually all habitats. Some are commercially important, a few are pests and some carry diseases, while many non-marine molluscs are threatened by human impacts which have resulted in more extinctions than all tetrapod vertebrates combined. This book and its companion volume provide the first comprehensive account of the Mollusca in decades. Illustrated with hundreds of colour figures, it reviews molluscan biology, genomics, anatomy, physiology, fossil history, phylogeny and classification. This volume includes general chapters drawn from extensive and diverse literature on the anatomy and physiology of their structure, movement, reproduction, feeding, digestion, excretion, respiration, nervous system and sense organs. Other chapters review the natural history (including ecology) of molluscs, their interactions with humans, and assess research on the group. Key features of both volumes: up to date treatment with an extensive bibliography; thoroughly examines the current understanding of molluscan anatomy, physiology and development; reviews fossil history and phylogenetics; overviews ecology and economic values; and summarises research activity and suggests future directions for investigation. Winston F Ponder was a Principal Research Scientist at The Australian Museum in Sydney where he is currently a Research Fellow. He has published extensively over the last 55 years on the systematics, evolution, biology and conservation of marine and freshwater molluscs, as well as supervised post graduate students and run university courses. David R. Lindberg is former Chair of the Department of Integrative Biology, Director of the Museum of Paleontology, and Chair of the Berkeley Natural History Museums, all at the University of California. He has conducted research on the evolutionary history of marine organisms and their habitats on the rocky shores of the Pacific Rim for more than 40 years. The numerous elegant and interpretive illustrations were produced by Juliet Ponder.
'Truth and courage are what memoirs need and this one has them both in spades … The unforgotten boy: that is what makes this a book a revelation' ADAM NICOLSON ‘Wonderful, absolutely beguiling … I learnt a lot and really loved it’ RICHARD HOLMES ‘Gloriously evocative’ DAILY MAIL What makes a scientist? Charming, funny and wise, in this memoir Richard Fortey shows how restless curiosity about the natural world led him to become a leading scientist and writer, with adventures and misadventures along the way. From a garden shed laboratory where he manufactured the greatest stink in the world to a tent high in the Arctic in pursuit of fossils, this is a story of obsession and love of nature, flavoured with the peculiarities and restrictions of post-war Britain. Fortey tells the story of following his father down riverbanks to fish for trout, and also of his father's shocking death. He unfolds his early passions – fungi, ammonite hunting and eyeing up bird's eggs. He evokes with warmth and wit how the natural world started out as his playground and refuge, then became his life's work. Much more than a story about science alone, this memoir gives an unforgettable portrait of a young, curious mind, and shows how luck and enthusiasm can create a special life.
This volume is an outcome of the 12th international conference of the international bryozoology association in Dublin. It consists of 85 oral and 16 poster presentations which cover all aspects of bryozoological research.
ANOXIA defines the lack of free molecular oxygen in an environment. In the presence of organic matter, anaerobic prokaryotes produce compounds such as free radicals, hydrogen sulfide, or methane that are typically toxic to aerobes. The concomitance of suppressed respiration and presence of toxic substances suggests these habitats are inhospitable to Eukaryota. Ecologists sometimes term such environments 'Death Zones'. This book presents, however, a collection of remarkable adaptations to anoxia, observed in Eukaryotes such as protists, animals, plants and fungi. Case studies provide evidence for controlled beneficial use of anoxia by, for example, modification of free radicals, use of alternative electron donors for anaerobic metabolic pathways, and employment of anaerobic symbionts. The complex, interwoven existence of oxic and anoxic conditions in space and time is also highlighted as is the idea that eukaryotic inhabitation of anoxic habitats was established early in Earth history.
This multidisciplinary book focuses on the relationships and interactions between palaeobiogeography, biogeography, dispersal, vicariance, migrations and evolution of organisms in the SE Asia-Australasian region. The book investigates biogeographic links between SE Asia and Australasia which go back more than 500 million years. It also focuses on the links between geological evolution and biological migrations and evolution in the region. It was in the SE Asian region that Alfred Russell Wallace established his biogeographic line, now known as Wallace's Line, which was the beginning of biogeography. Wallace also independently developed his theory of evolution based on his work in this area.;The book brings together, for the first time, geologists, palaeontologists, zoologists, botanists, entomologists, evolutionary biologists and archaeologists, in the one volume, to relate the region's geological past to its present biological peculiarities. The book is organized into six sections. Section 1 Paleobiogeographic Background provides overviews of the geological and tectonic evolution of SE Asia-Australasia, and changing patterns of land and sea for the last 540 million years. Section 2 Palaeozoic and Mesozoic Geology and Biogeography discusses Palaeozoic and Mesozoic biogeography of conodonts, brachiopods, plants, dinosaurs and radiolarians and the recognition of ancient biogeographic boundaries or Wallace Lines in the region. Section 3 Wallace's Line focuses on the biogeographic boundary established by Wallace, including the history of its establishment, its significance to biogeography in general and its applicability in the context of modern biogeography.;Section 4 Plant biogeography and evolution includes discussion on primitive angiosperms, the diaspora of the southern rushes, and environmental, climatic and evolutionary implications of plants and palynomorphs in the region. The biogeography and migration of insects, butterflies, birds, rodents and other non-primate mammals is discussed in section 5, Non Primates. The final section 6 Primates focuses on the biogeographic radiation, migration and evolution of primates and includes papers on the occurrence and migration of early hominids and the requirements for human colonization of Australia.
This impeccably-researched volume skillfully reports and discusses
advances in phytolith research, addressing in particular the use of
phytoliths for deciphering fundamental issues in earth science and
human history. Comprising thirty reviews and original papers,
findings are presented in the following five sections:
This book examines case studies of North American Quaternary mammalian evolution within the larger domain of modern evolutionary theory. It presents previously unpublished studies of a variety of taxa (xenarthrans, rodents, carnivores, ungulates) examined over several temporal scales, from a few thousand years during the Holocene to millions of years of late Pliocene and Pleistocene time. Different organizational levels are represented, from mosaic population variation, to a synopsis of Quaternary evolution of an entire order (Rodentia). In addition to specific case histories, the book includes purely theoretical and methodological contributions, for example, on the statistical recognition of stasis in the fossil record, new ways to calculate evolutionary rates, and the use of digital image analysis in the study of dental ontogeny. Perhaps the most important aspect of the studies reported in this book is that they span the time between the "ecological moment" and "deep time." Modern taxa can be traced back into the fossil record, and variation among extant taxa can be used as a control against which variation in the extinct ones can be understood.
Our knowledge of extinct animals depends almost entirely upon the study of fossils. This richly illustrated book clothes the skeletons of dinosaurs and other Mesozoic reptiles with flesh, and shows how these fascinating animals evolved and probably lived. Expert author John L. Cloudsley-Thompson provides an interesting synthesis of current views on their ecology, physiology and behaviour, and outlines the various hypotheses that have been proposed to explain their extinction. Numerous beautiful drawings of the animals and their environment illustrate this exciting monograph.
The 11 chapters provide a wide ranging perspective on some of the problems under investigation and several of the systematic approaches currently in use by those concerned with refining the knowledge of the changing environments in the world's drylands during the latter part of the Quaternary. Dealing with a part of the globe that is highly sensitive to small changes of climate, or other stresses such as human impact, this book brings together a set of excellent reviews that will be of great value to students beginning to understand the subject and to paleoenvironmental scientists actively concerned with finding solutions to problems of the region. Additionally, it will be an invaluable archive of important references covering the subject of arid lands palaeoenvironmental research. This volume achieves the aspirations of the International Geological Correlation Programme.
Palaeohydrological research is a comparatively recent development. However, research undertaken has already demonstrated a significant multidisciplinary impact and shown how palaeohydrology can provide an important contribution to the study of global change. Although a considerable amount of exciting palaeohydrological research has been applied to particular areas, there has not previously been a systematic approach to research into the palaeohydrology of the Earth's surface. It was for this reason that a Commission was established by INQUA in 1991 on Global Continental Palaeohydrology. This volume provides the background to that exciting international research project and has been written to provide a basis for understanding the current state of research into the palaeohydrology of the land surface of the Earth. It therefore gives a summary of the work achieved to date and of the research investigations currently taking place, together with an indication of the way in which palaeohydrological research relates to other global research programmes.
These proceedings record the results of climate change in many areas which are hyper-arid deserts today but which, almost cyclically, at intervals of thousands or even hundreds of thousands of years, have had a much more humid climate.
The first palaeoecology book to focus on evolutionary palaeoecology, in both marine and terrestrial environments. Discusses reconstruction of the past ecological world at population, community and biogeographic levels. A well-illustrated and substantial volume giving accessible coverage of the full range of subjects within palaeoecology. Reviews and summarises all the major mass extinctions. |
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