Fossil Scleractinian Corals from James Ross Basin, Antarctica

Fossil Scleractinian Corals from James Ross Basin, Antarctica PDF Author: Filkorn
Publisher: American Geophysical Union
ISBN:
Category :
Languages : en
Pages : 107

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Fossil Scleractinian Corals from James Ross Basin, Antarctica

Fossil Scleractinian Corals from James Ross Basin, Antarctica PDF Author: Filkorn
Publisher: American Geophysical Union
ISBN:
Category :
Languages : en
Pages : 107

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Book Description


Frozen in Time

Frozen in Time PDF Author: Jeffrey Stilwell
Publisher: CSIRO PUBLISHING
ISBN: 0643096353
Category : Nature
Languages : en
Pages : 249

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Book Description
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 Margin Systems

Ocean Margin Systems PDF Author: Gerold Wefer
Publisher: Springer Science & Business Media
ISBN: 3662051273
Category : Science
Languages : en
Pages : 486

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Book Description
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.

Cold-water Corals

Cold-water Corals PDF Author: J. Murray Roberts
Publisher: Cambridge University Press
ISBN: 0521884853
Category : Coral reefs and islands
Languages : en
Pages : 351

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Book Description
"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.

Paleogene Shallow Benthos of the Tethys, 2

Paleogene Shallow Benthos of the Tethys, 2 PDF Author: Katica Drobne
Publisher: Založba ZRC
ISBN: 961624213X
Category : Science
Languages : en
Pages : 353

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Book Description
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.

The West Antarctic Ice Sheet

The West Antarctic Ice Sheet PDF Author:
Publisher: American Geophysical Union
ISBN:
Category : Geology
Languages : en
Pages : 297

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Terra Antartica

Terra Antartica PDF Author:
Publisher:
ISBN:
Category : Antarctica
Languages : en
Pages : 658

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Palaeontological Results of the Polish Antarctic Expeditions

Palaeontological Results of the Polish Antarctic Expeditions PDF Author: Andrzej Gaździcki
Publisher:
ISBN:
Category : Paleobotany
Languages : en
Pages : 296

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Scleractinian Corals from the Cretaceous of the Alps and N Dinarides

Scleractinian Corals from the Cretaceous of the Alps and N Dinarides PDF Author: Rosemarie C. Baron-Szabo
Publisher:
ISBN: 9783853160749
Category : Corals, Fossil
Languages : en
Pages : 304

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Book Description
Literaturverz. S. 269 - 282

Biogeochemistry of the Ross Sea

Biogeochemistry of the Ross Sea PDF Author: Giacomo R. DiTullio
Publisher: American Geophysical Union
ISBN:
Category : Nature
Languages : en
Pages : 374

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Book Description
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.