Download Free Fossil Scleractinian Corals From James Ross Basin Antarctica Book in PDF and EPUB Free Download. You can read online Fossil Scleractinian Corals From James Ross Basin Antarctica and write the review.

Presents a comprehensive overview of the fossil record of Antarctica framed within its changing environmental settings. Jeffrey Stilwell, Monash University; John Long, Australian palaentologist, currently at Natural History Museum of Los Angeles, USA.
Ocean margins are the transitional zones between the oceans and continents. They represent dynamic systems in which numerous processes shape the environment and result in impacting the utilization and hazard potentials for humans. These processes are influenced by a variety of steering mechanisms, from mountain building and climate on the land to tectonics and sea-level fluctuations in ocean margins. This book examines various aspects of regulation for the long-term development of ocean margins, of the impact of fluids and of the dynamics of benthic life at and below the seafloor in ocean margin systems.
"This broad-ranging treatment is the first to synthesise current understanding of all types of cold-water coral, covering their ecology, biology, paleontology and geology."--Back cover.
Obdobje 20 milijonov let, ki je sledilo opustošenju po kredno-terciarni meji in izumrtju dinozavrov, ima posebno mesto v zgodovini Zemlje. V tem času se je postopoma obnavljalo življenje z vso pestrostjo svojih oblik. Podrobno proučevanje tega obnavljanja nam daje ključ za razumevanje vzrokov, zakaj in kako je vzniknila in napredovala raznovrstnost življenja. Pričujoči zvezek je zbir zgodovinskih dokumentov, ki ilustrirajo nekatere od mnogih podob obnove.
Literaturverz. S. 269 - 282
Published by the American Geophysical Union as part of the Antarctic Research Series, Volume 78. The seas surrounding Antarctica are the least-studied on Earth, yet they figure prominently in both the global climate system and the biogeochemical cycling of such key elements as C, N, Si, and P. The Southern Ocean affects climate directly through the sinking of surface waters via cooling and changes in salt content. Such water near Antarctica moves slowly northward through all major ocean basins. In doing so, it retains a long-lived signature of the physical and biological processes that occurred in Antarctic surface waters lasting many hundreds of years through all phases: sinking, northward flow, and mixing or upwelling into the sunlit ocean thousands of kilometers away. By this process, CO2 that dissolves into the Antarctic seas may be stored in the deep ocean for centuries. In fact, the Southern Ocean is one of the most important regions on Earth for the uptake and subsurface transport of fossil fuel CO2.