saraswati pratul kumar (10 Ergebnisse)

hardcover. Zustand: Very Good.

Paperback. Zustand: Brand New. reprint edition. 236 pages. 9.25x6.10x0.54 inches. In Stock.

Hardcover. Zustand: Brand New. 236 pages. 9.25x6.25x0.75 inches. In Stock.

Zustand: New.

Hardcover. Zustand: Brand New. 199 pages. 9.25x6.10x9.49 inches. In Stock.

Buch. Zustand: Neu. Neuware -Foraminifera are single-celled marine organisms, usually less than a millimeter in size, and their fossil records extend back in geological time some 500 million years. Some foraminifera have grown to over 10 centimeters; these are informally called 'larger benthic Foraminifera' (LBF). LBF are of outstanding value in field and in laboratory experiments. They can serve as geochemical proxies and can be used to learn about biology, biomineralization process, and more. Their study finds wide-ranging geological applications, including the carbonate platforms' past environmental changes and stratigraphy. There are many books on micropaleontology, fewer on Foraminifera and practically none on LBF. The ones that do exist are generally too specialized for micropaleontology and carbonate sedimentology doctoral students to utilize. This volume aims to fill this gap by providing readers with an understanding of the morphology and distribution of LBF in space (environment) and time (evolution). In addition, the isotope and trace metal proxies in LBF are discussed for paleoclimate reconstruction. This volume will benefit researchers and professionals in micropaleontology, hydrocarbon exploration, carbonate sedimentology, and paleoclimate.Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 200 pp. Englisch.

Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Foraminifera are single-celled marine organisms, usually less than a millimeter in size, and their fossil records extend back in geological time some 500 million years. Some foraminifera have grown to over 10 centimeters; these are informally called 'larger benthic Foraminifera' (LBF). LBF are of outstanding value in field and in laboratory experiments. They can serve as geochemical proxies and can be used to learn about biology, biomineralization process, and more. Their study finds wide-ranging geological applications, including the carbonate platforms' past environmental changes and stratigraphy. There are many books on micropaleontology, fewer on Foraminifera and practically none on LBF. The ones that do exist are generally too specialized for micropaleontology and carbonate sedimentology doctoral students to utilize. This volume aims to fill this gap by providing readers with an understanding of the morphology and distribution of LBF in space (environment) and time (evolution). In addition, the isotope and trace metal proxies in LBF are discussed for paleoclimate reconstruction. This volume will benefit researchers and professionals in micropaleontology, hydrocarbon exploration, carbonate sedimentology, and paleoclimate.

Zustand: New. Provides an overview of the Earth history as witnessed and evidenced by foraminifera Discusses a variety of geochemical proxies used in reconstruction of environment, climate and paleobiology of foraminifera Presents a new insight.

Paperback. Zustand: Brand New. 350 pages. 9.00x7.50x0.75 inches. In Stock.

Taschenbuch. Zustand: Neu. Neuware - Foraminiferal Micropaleontology for Understanding Earth's History incorporates new findings on taxonomy, classification and biostratigraphy of foraminifera. Foraminifera offer the best geochemical proxies for paleoclimate and paleoenvironment interpretation. The study of foraminifera was promoted by oil exploration due to its exceptional use in subsurface stratigraphy. A rapid technological development in the past 20 years in the field of imaging microfossils and in geochemical microanalysis have added novel information about foraminifera. Foraminiferal Micropaleontology for Understanding Earth's History builds an understanding of biology, morphology and classification of foraminifera for its varied applications. In the past two decades, a phenomenal growth has occurred in geochemical proxies in shells of foraminifera, and as a result, crucial information about past climate of the earth is achieved. Foraminifera is the most extensively used marine microfossils in deep-time reconstruction of the earth history. Its key applications are in paleoenvironment and paleoclimate interpretation, paleoceanography, and biostratigraphy to continuously improve the Geologic Time Scale.