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Palynos

Palynos PDF Author:
Publisher:
ISBN:
Category : Palynography
Languages : en
Pages : 22

Book Description


Palynos

Palynos PDF Author:
Publisher:
ISBN:
Category : Palynography
Languages : en
Pages : 22

Book Description


Palynos

Palynos PDF Author:
Publisher:
ISBN:
Category : Palynography
Languages : en
Pages : 26

Book Description


Paleopalynology

Paleopalynology PDF Author: Alfred Traverse
Publisher: Springer Science & Business Media
ISBN: 1402056109
Category : Science
Languages : en
Pages : 816

Book Description
This book provides complete coverage of all aspects of the study of all fossil palynomorphs yet studied. It is a profusely illustrated treatment. The book serves both as a student text and general reference work. Palynomorphs yield information about age, geological and biological environment, climate during deposition, and other significant factors about the enclosing rocks. Extant spores and pollen are treated first, preparing the student for more difficult work with fossil sporomorphs and other kinds of palynomorphs. An appendix describes laboratory methods. The glossary, bibliographies and index are useful tools for study of the literature.

Palyno-stratigraphy of the Ketewaka Coalfield (Lower Permian), Tanzania

Palyno-stratigraphy of the Ketewaka Coalfield (Lower Permian), Tanzania PDF Author: Svein Manum
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 20

Book Description


The Indian Paleogene

The Indian Paleogene PDF Author: Sunil Bajpai
Publisher: Springer
ISBN: 3319774433
Category : Science
Languages : en
Pages : 331

Book Description
This unique book provides a concise account of Indian Paleogene and presents a unified view of the Paleogene sequences of India. The Paleogene, comprising the early part of the Cenozoic Era, was the most dynamic period in the Earth’s history with profound changes in the biosphere and geosphere. The period spans ~42 million years, beginning from post- K/T mass extinction event at ~65 Ma and ending at ~23 Ma, when the first Antarctic ice sheet appeared in the Southern Hemisphere. The early Paleogene (Paleocene–Eocene) has been considered a globally warm period, superimposed on which were several transient hyperthermal events of extreme warmth. Of these, the Palaeocene Eocene Thermal Maxima (PETM) boundary interval is the most prominent extreme warming episode, lasting 200 Ka. PETM is characterized by 2–6‰ global negative carbon isotope excursion. The event coincided with the Benthic Extinction Event (BEE) in deep sea and Larger Foraminifera Turnover (LFT) in shallow seas. Rapid ~60–80 warming of high latitudinal regions led to major faunal and floral turnovers in continental, shallow-marine and deep-marine areas. The emergence and dispersal of mammals with modern characteristics, including Artiodactyls, Perissodactyls and Primates (APP), and the evolution and expansion of tropical vegetation are some of the significant features of the Paleogene warm world. In the Indian subcontinent, the beginning and end of the Paleogene was marked by various events that shaped the various physiographic features of the Indian subcontinent. The subcontinent lay within the equatorial zone during the earliest part of the Paleogene. Carbonaceous shale, coal and lignite deposits of early Eocene age (~55.5–52 Ma) on the western and north-eastern margins of the Indian subcontinent are rich in fossils and provide information on climate as well as the evolution and paleobiogeography of tropical biota. Indian Paleogene deposits in the India–Asia collision zone also provide information pertaining to the paleogeography and timing of collision. Indian Paleogene rocks are exposed in the Himalayan and Arakan mountains; Assam and the shelf basins of Kutch–Saurashtra, Western Rajasthan; Tiruchirappalli–Pondicherry and Andaman and, though aerially limited, these rocks bear geological evidence of immense importance.

Amazon

Amazon PDF Author: Paul A Collinvaux
Publisher: CRC Press
ISBN: 1482283603
Category : Science
Languages : en
Pages : 413

Book Description
Amazon will prove a powerful tool for ecologists and climate modelers. It also contains brief reviews of pioneering pollen work in the Amazon to date; sections on pollen methods, pollen statistics, paleoecology, and lake coring methods.

Journal of the Palaeontological Society of India

Journal of the Palaeontological Society of India PDF Author: Palaeontological Society of India
Publisher:
ISBN:
Category : Paleontology
Languages : en
Pages : 502

Book Description


Sedimentary Organic Matter

Sedimentary Organic Matter PDF Author: R. Tyson
Publisher: Springer Science & Business Media
ISBN: 9401107394
Category : Science
Languages : en
Pages : 634

Book Description
A sound understanding of the global carbon cycle requires an appreciation of the various physico-chemical and biological processes that determine the production, distribution, deposition and diagenesis of organic matter in the natural environment. This book is a comprehensive interdisciplinary synthesis of this information, coupled with an organic facies approach based on data from both microscopy and bulk organic geochemistry.

Foraminifera and their Applications

Foraminifera and their Applications PDF Author: Robert Wynn Jones
Publisher: Cambridge University Press
ISBN: 1107036402
Category : Science
Languages : en
Pages : 407

Book Description
A one-stop practical guide to foraminifera with numerous case studies demonstrating their applications, for graduate students, micropalaeontologists and industry professionals.

The SE Asian Gateway

The SE Asian Gateway PDF Author: Robert Hall
Publisher: Geological Society of London
ISBN: 9781862393295
Category : Continental drift
Languages : en
Pages : 400

Book Description
Collision between Australia and SE Asia began in the Early Miocene and reduced the former wide ocean between them to a complex passage which connects the Pacific and Indian Oceans. Today, the Indonesian Throughflow passes through this gateway and plays an important role in global thermohaline flow. The surrounding region contains the maximum global diversity for many marine and terrestrial organisms. Reconstruction of this geologically complex region is essential for understanding its role in oceanic and atmospheric circulation, climate impacts, and the origin of its biodiversity. The papers in this volume discuss the Palaeozoic to Cenozoic geological background to Australia and SE Asia collision. They provide the background for accounts of the modern Indonesian Throughflow and oceanographic changes since the Neogene, and consider aspects of the region's climate history--