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Nearshore marine paleoclimatic regions, increasing zoogeographic provinciality, molluscan extinctions, and paleoshorelines, California: Late Oligocene (27 Ma) to late Pliocene (2.5 Ma) (GSA Special Paper 357)

معرفی کتاب «Nearshore marine paleoclimatic regions, increasing zoogeographic provinciality, molluscan extinctions, and paleoshorelines, California: Late Oligocene (27 Ma) to late Pliocene (2.5 Ma) (GSA Special Paper 357)» نوشتهٔ Clarence A. Hall Jr.، منتشرشده توسط نشر Geological Society of America در سال 2002. این کتاب در فرمت pdf، زبان انگلیسی ارائه شده است.

This volume depicts the distribution of ancient marine basins in western California from the late Oligocene to the late Pliocene periods. In addition, it shows positive feedback mechanisms between paleolatitudinal changes in sea-surface paleotemperature gradients and changes in the diversity of marine mollusks along the California coast through time; uses effective temperature to define "equable" nearshore marine water masses; and analyzes extinction rates among macroinvertebrate marine taxa from coastal California and the possible causes of these extinctions. The slipcase contains 19 folded maps and the codex. Clarence A. Hall, Jr. is a member of the department of earth and space sciences, UCLA. Annotation c. Book News, Inc., Portland, OR Approximately 3000 middle and late Cenozoic nearshore marine molluscan taxa from western California are assigned to six time periods, spanning ~25 m.y. In this interdisciplinary study, western California is palinspastically restored for each of the time periods by backsliding and back-rotating large fault blocks or crustal units. Marine fossil assemblages are assigned to nearshore paleoclimatic regions or water masses within palinspastically restored California. In addition, this volume reveals positive feedback mechanisms between paleolatitudinal changes in sea-surface paleotemperature gradients and changes in the diversity of marine mollusks along the California coast through time; defines "equable" based effective temperatures; and analyzes extinction rates among macroinvertebrate marine taxa from coastal California and the possible causes of these extinctions. The late Paleogene to Neogene faunas reflect an increase in faunal diversity related to strengthened temperature gradients, greater extremes in sea-surface temperatures, reduction in temperateness, and the development of an embayed California coastline Nearshore marine paleoclimatic regions, increasing zoogeographic provinciality, molluscan extinctions, and paleoshorelines, California: Late Oligocene (27 Ma) to late Pliocene (2.5 Ma)......Page 1 ISBN 0-8137-2357-4......Page 2 INTRODUCTION......Page 3 PROCEDURE......Page 6 PALEOSHORELINE MAPS AND PALEOCLIMATIC REGIONS......Page 43 DISCUSSION......Page 45 CONCLUSIONS......Page 72 SUMMARY......Page 73 ACKNOWLEDGMENTS......Page 75 APPENDICES......Page 77 Back cover / Contents......Page 493
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