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Paleobiology of the Polycystine Radiolaria [Mīkstie vāki]

(Museum fur Naturkunde, Germany), (Kyushu University, Japan), (Tohoku University, Japan), (University of Tsukuba, Japan)
  • Formāts: Paperback / softback, 504 pages, height x width x depth: 244x170x27 mm, weight: 992 g
  • Sērija : TOPA Topics in Paleobiology
  • Izdošanas datums: 12-Feb-2021
  • Izdevniecība: Wiley-Blackwell
  • ISBN-10: 0470671440
  • ISBN-13: 9780470671443
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  • Formāts: Paperback / softback, 504 pages, height x width x depth: 244x170x27 mm, weight: 992 g
  • Sērija : TOPA Topics in Paleobiology
  • Izdošanas datums: 12-Feb-2021
  • Izdevniecība: Wiley-Blackwell
  • ISBN-10: 0470671440
  • ISBN-13: 9780470671443
Citas grāmatas par šo tēmu:
"Polycystine radiolarians (e.g., those groups which produce robust siliceous shells) are single-celled marine planktonic organisms, and their shells are important as fossils in marine sediments and rocks from the early Paleozoic to the Recent. They are used extensively for biostratigraphy and paleoenvironmental studies in all geologic age intervals, particularly where other fossils are absent (e.g. metamorphosed older rocks, Cenozoic deep-sea sediments in upwelling zones and polar regions). Scientists using radiolarians in their work are based in geological surveys, university departments, marine institutes and the oil industry. The largest concentrations of radiolarian specialists currently are located in Europe and Japan, although specialists exist in many countries."--

Polycystine radiolaria are exclusively marine protists and are found in all ocean waters, from polar regions to the tropics, and at all water depths. There are approximately 600 distinct described living species and several thousand fossil species of polycystines. Radiolarians in general, and polycystines in particular, have recently been shown to be a major component of the living plankton and important to the oceanic carbon cycle. As fossils radiolarians are also fairly common, and often occur in sediments where other types of fossils are absent. This has made them very valuable for certain types of geologic research, particularly estimating the geologic age of the sediments containing them, and as guides to past oceanic water conditions. As our current understanding of the biology, and even taxonomy of the living fauna is still very incomplete, evolutionary studies based on living polycystines are still rare. However, the common occurrence of numerous specimens for many species, and in a wide variety of oceanic environments, provides an excellent opportunity to study the processes of biologic evolution in the fossil record. 

Paleobiology of the Polycystine Radiolaria is the first major book on radiolarians to appear in the western literature since 2001.&;Focusing on living and fossil siliceous shelled radiolarians, it is notable for its emphasis not upon morphologic or taxonomic detail but on concepts and applications. The book attempts to provide a balanced, critical review of what is known of the biology, ecology, and fossil record of the group, as well as their use in evolutionary, biostratigraphic and paleoceanographic research. Full chapters on the history of study, and molecular biology, are the first ever in book form.  

Written for an audience of advanced undergraduate to doctoral students, as well as for a broad range of professionals in the biological and Earth sciences, Paleobiology of the Polycystine Radiolaria summarizes current understanding of the marine planktonic protist group polycystine radiolaria, both in living and fossil form. 

 

Recenzijas

Paleobiology of the Polycystine Radiolaria is well worth the purchase price and should be in the personal library of all protistologists working on marine forms. Journal of Eukaryotic Microbiology

A welcome addition to the literature in a field that is rich in potential for interdisciplinary research. Journal of Plankton Research

Preface xi
Acknowledgements xv
Chapter 1 History 1(40)
Introduction
1(3)
Scientific Context
4(4)
Early Studies (First Half of the Nineteenth Century)
8(5)
C.G. Ehrenberg and J. Muller
8(5)
Second Half of the Nineteenth Century to ca. 1920
13(3)
E. Haeckel and his Disciples
13(3)
Legacy of Early Studies
16(1)
Early Twentieth Century (ca. 1920-1940)
17(3)
The Early New Period (ca. 1940-1970)
20(8)
The Origins of Radiolarian Biostratigraphy: 1940s to 1950s
20(1)
Deep-Sea Drilling
21(4)
Taxonomy
25(2)
Biology
27(1)
Mid New Period (1970-2000)
28(9)
Current Period (2000-Present)
37(4)
Chapter 2 Biology 41(30)
General Characteristics of Planktonic Protist Biology
41(1)
Physical Characteristics of the Pelagic Ocean
42(4)
Plankton Taxa
46(1)
Ecologic and Behavioral Constraints due to Small Body Size
46(2)
Basic Radiolarian Cellular Structure
48(5)
Skeleton
53(2)
Skeleton Formation and Growth
55(4)
Size
59(1)
Colonial Forms
59(1)
Life Cycle
60(2)
Longevity
62(1)
Motility
63(1)
Feeding
63(2)
Predators
65(1)
Abundance and Role in Carbon Cycle
66(1)
Symbiosis
67(1)
Bioluminescence
68(1)
Summary
69(2)
Chapter 3 Ecology 71(24)
Introduction
71(4)
Biogeography
75(8)
Vertical Distribution
83(3)
Tropical Submergence
86(3)
Longitudinal Gradients and Upwelling Assemblages
89(1)
Latitudinal Gradients
90(1)
Coastal Gradients
90(1)
Seasonal Variability
91(2)
Interannual Variability
93(2)
Chapter 4 Genetics 95(22)
Introduction
95(1)
Molecular Phylogenetic Position of "Radiolarians" within Eukaryotes
96(1)
Molecular Studies of Radiolarian's Position within Eukaryotes
97(1)
Relationships of Radiolarian Clades
98(4)
Origination Times of Radiolarian Clades
102(1)
Family-Level Phylogeny
102(5)
Spumellaria (Shell-Bearing Radiolarians)
105(1)
Collodaria (Colonial or Naked Radiolarians)
105(1)
Nassellaria
106(1)
Acantharia
107(1)
Microevolution of Radiolaria
107(4)
Diversity of Pico-Radiolarian Material
111(1)
Transcriptomics of Radiolaria
112(1)
Methodology
113(1)
DNA Extraction
114(1)
Reproductive Cell Method
114(1)
Dissecting Cell Method
114(1)
PCR
114(1)
Summary
114(3)
Chapter 5 Taxonomy and Fossil Record 117(100)
Introduction
117(1)
Part 1 Radiolarian Taxonomy
118(75)
Principles of Species-Level Taxonomy
118(3)
Rules for Describing and Naming Species
121(3)
Current Status of Descriptive Radiolarian Taxonomy
124(5)
Principles of Higher-Level Taxonomy
129(1)
Haeckel and the Beginnings of Higher-Level Radiolarian Taxonomy
129(3)
Biologic Systematics
132(2)
Higher-Level Taxonomy in Radiolaria
134(9)
The Observational Basis of Taxonomy: Structures of the Radiolarian Shell
136(3)
Higher-Level Taxonomy in this Book
139(4)
Formal Classification of Polycystina
143(42)
Cenozoic Taxa
143(1)
Order Spumellaria Ehrenberg 1876
143(17)
Family Actinommidae Haeckel 1862
145(4)
Family Heliodiscidae Haeckel 1881
149(2)
Family Coccodiscidae Haeckel 1862, emend. Sanfilippo and Riedel 1980
151(2)
Family Pylonlidae Haeckel 1881
153(2)
Family Lithelidae Haeckel 1862
155(1)
Family Tholonidae Haeckel 1887
156(1)
Family Spongodiscidae Haeckel 1862
156(4)
Order Nassellaria Ehrenberg 1876
160(23)
Family Plagiacanthidae Hertwig 1879
162(1)
Family Trissocyclidae (Haeckel) Goll 1968 [ superfamily Acanthodesmiacea]
163(1)
Family Theoperidae Haeckel 1881
163(4)
Family Artostrobiidae Riedel 1967
167(1)
Family Pterocoryithidae (Haeckel) Moore 1972
167(4)
Family Carpocaniidae (Haeckel) Riedel, 1967 [ Carpocaniinae]
171(2)
Family Cannobotryidae Haeckel, 1881
173(1)
Superfamily Collodaria
173(2)
Family CollosphaeridaeIler, 1858
175(1)
Family Sphaerozoidae Haeckel, 1862
175(2)
Family Collophidiidae Biard and Suzuki, in Biard et al., 2015
177(6)
Order Entactinaria
183(2)
Family Orosphaeridae Haeckel, 1887
183(1)
Family Saturnalidae Deflandre 1953
184(1)
Mesozoic and Paleozoic Taxa
185(1)
Species-Level Variation in Radiolaria
185(8)
Part 2 Summary of the Radiolarian Fossil Record
193(24)
Cambrian and Ordovician
194(1)
Silurian to the Lower Carboniferous
195(1)
Late Paleozoic to Late Mesozoic Siliceous Sedimentation
196(1)
Mass Extinctions at the End of the Paleozoic Era
197(3)
Basal Mesozoic Scarcity of Radiolarian Fossils and Faunal Turnover (Early Triassic)
200(1)
Triassic
201(3)
Triassic-Jurassic Boundary Mass Extinction
204(1)
Jurassic
205(1)
Early and Middle Jurassic Radiolaria
205(3)
Late Jurassic-Early Cretaceous
208(1)
Cretaceous
208(4)
The K/T Extinction Event and Early Paleocene
212(2)
Cenozoic
214(3)
Chapter 6 Preservation and Methods 217(36)
Introduction
217(1)
Preservation
218(9)
Geographic Variation in Preservation
222(1)
Diagenesis
222(2)
Loss of Rock Record
224(1)
Differences between Modern and Ancient Oceans
224(1)
Quality of Radiolarian Fossil Record
225(2)
Methods
227(26)
Collecting Material from the Water Column
228(3)
Collecting Sediments
231(5)
Collecting Lithified Material from Sections on Land
236(2)
Recovering Radiolarians from Samples
238(5)
Extracting Radiolarians with Intact Protoplasm
238(1)
Extracting Radiolarian Skeletons
238(4)
Separation of Radiolarians from other Chemically Resistant Similar-Sized Components of Residue
242(1)
Mounting Radiolarians
243(2)
Live Preparations
245(1)
Dissection and Serial Sectioning
246(1)
Imaging Radiolarians
247(1)
Visualization (enhanced imagery)
248(1)
Morphometrics
249(1)
Automatic Identification
249(4)
Chapter 7 Paleoceanography 253(28)
Introduction
253(6)
Radiolarians as Tracers of Water Masses
259(1)
Assemblage-Based Methods of Paleoceanographic Analysis
259(14)
Non-temperature Uses of Assemblage Analyses
268(5)
Radiolarians in Bulk: Summary Indices and Non-Taxonomic Uses of Radiolarians in Paleoceanography
273(8)
Chapter 8 Radiolarian Biostratigraphy 281(46)
Introduction
281(2)
Biostratigraphy in Shallow Marine Rocks: General Aspects
283(2)
Biostratigraphy in Deep-Sea Sediment Sections
285(2)
Other Types of Geochronologic Information
287(8)
Radiometric Dating and Absolute Age
287(1)
Paleomagnetic Stratigraphy
288(2)
Stable Isotope Stratigraphy
290(1)
Cyclostratigraphy
291(1)
Quantitative Biostratigraphy
292(3)
Cenozoic Radiolarian Stratigraphy
295(24)
History of Development
296(1)
Tropical Cenozoic Radiolarian Stratigraphy
297(2)
Subtropical North Atlantic to Arctic
299(3)
North Pacific
302(3)
Southern Ocean
305(3)
History
305(2)
Characteristics
307(1)
Important Sections
307(1)
Important Species
307(1)
Mesozoic Radiolarian Stratigraphy
308(1)
Cretaceous
308(5)
Europe and Southwest North America
311(1)
Low-Latitude Western part of Mesotethys
311(1)
Mid-Ltitude Northern Part of Mesotethys
311(1)
Russian Epicontinental Seas
312(1)
East Margin of the Mid-Latitude Pacific
312(1)
Northwest Pacific
312(1)
Other Regions
313(1)
The Jurassic-Cretaceous Boundary (Tithonian-Berriasian Boundary)
313(1)
Jurassic
314(2)
Middle and Late Jurassic
314(2)
Lower Jurassic
316(1)
Triassic-Jurassic Boundary
316(1)
Triassic
316(2)
Latest Triassic (Rhaetian)
317(1)
Carnian and Norian
318(1)
Late Olenekian to Ladinian
318(1)
Basal Triassic (Induan) and Permian-Triassic (P-T) boundary
318(1)
Paleozoic Radiolarian Stratigraphy
319(8)
Permian
319(12)
Carboniferous
321(1)
Devonian and Silurian
321(4)
Ordovician and Cambrian
325(2)
Chapter 9 Evolution 327(66)
Introduction and General Principles
327(3)
Features of the Deep-Sea Microfossil Record Relevant to the Study of Evolution
330(1)
Microevolution
331(15)
Pattern and Processes
332(1)
Examples of Microevolution
333(13)
Cladogenesis
333(6)
Anagenesis
339(5)
Extinction
344(1)
Hybridization
344(2)
Macroevolution
346(3)
Definitions and Theory
346(2)
Theories of Diversity and Evolution
348(1)
Macroevolutionary Patterns in Radiolaria
349(39)
Origin of Radiolarians
349(5)
Origin of Collodaria and Colonial Radiolaria
352(2)
Origin of Higher Taxa within Radiolaria - General Comments
354(1)
Diversity History of Radiolarians
354(10)
Methods of Diversity Reconstruction
354(4)
Other Problems of Diversity Reconstruction
358(1)
Data for Diversity Reconstruction
358(1)
Global Phanerozoic Diversity
358(5)
Paleozoic
363(1)
Mesozoic
364(4)
Cretaceous-Tertiary Boundary
368(4)
Cenozoic
372(14)
Other Aspects of Cenozoic Radiolarian Macroevolutionary Change
382(4)
Phanerozoic Diversity - A More Modest View
386(2)
Summary Discussion
388(5)
References 393(68)
Index 461
About the Editors

David Lazarus has studied the paleobiology and earth science applications of Cenozoic radiolaria for more than 40 years, formerly holding research positions at Columbia University/Lamont Earth Observatory, the Woods Hole Oceanographic Institution, and the Eidgenössische Technische Hochschule Zürich. He is currently Curator for Micropaleontology at the Museum für Naturkunde in Berlin.

Noritoshi Suzuki has studied the taxonomy and species diversity of radiolarians thoughout the Phanerozoic. He started his career in field geology, switched to Devonian radiolarians for his Masters degree, and received his PhD degree for a study of Cenozoic radiolarians from Tohoku University, Japan. He has co-published a monograph on the radiolarians of the Ehrenberg Collection (Berlin), and has published integrative studies of radiolarian morphology and phylogenetics. He is currently Associate Professor at Tohoku University.

Yoshiyuki Ishitani is a paleobiologist, focusing on the evolution of radiolarians. He is currently a researcher at the University of Tsukuba, and was formerly at Japan Agency for Marine-Earth Science and Technology, Glasgow University, and the University of Tokyo.

Kozo Takahashi has studied the distribution and ecology of radiolarians and other siliceous plankton collected from ocean waters for several decades. Following an early career of staff scientist positions at the Woods Hole and Scripps oceanographic institutions he held multiple professorships in Japan, including universities in Sapporo and Kyushu University in Fukuoka.