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A to Z of Earth Scientists, Updated Edition
A to Z of Earth Scientists, Updated Edition is a comprehensive A to Z reference of Earth scientists in areas including plate tectonics, climate change, and planetary science. Designed for high school through early college students, this is an ideal reference of notable Earth scientists from the 19th century to the present. Featuring nearly 200 entries and 100 black-and-white photographs, this title uses the device of biography in order to put a human face on science—a method that adds immediacy to the prose for the high school student who may have an interest in pursuing a career in the earth sciences. People covered include: James Hutton (1726–1797) William Smith (1769–1839) Charles Lyell (1797–1875) Mary Anning (1799–1847) Inge Lehmann (1888–1993) Walter Alvarez (1911–1988) Doris Malkin Curtis (1914–1991) Marie Tharp (1920–2006) David Keeling (1928–2005) Dawn Wright (1961–present)
Microbes
From heat waves and wildfires to flooding and record droughts, the impacts of climate change are now obvious. While the primary cause is the rise in greenhouse gases mainly from the burning of fossil fuels such as coal and petroleum, the complete story behind greenhouse gases also involves microbes and what they are doing in natural ecosystems. Although microbes contribute to the problem by producing greenhouse gases, climate change would be even more severe if not for other microbes that consume greenhouse gases. Understanding and solving the biggest environmental problem facing us today depends on the smallest organisms, microbes.
The Carboniferous Timescale
The print edition is published as 2 hardback volumes, parts A and B, and sold as a set. The Carboniferous was the time of the assembly of Pangaea by the collision of the Gondwanan and Larussian supercontinents, and the principal interval of the late Paleozoic ice ages. These tectonic and climatic events caused dramatic sea-level fluctuations and climate changes and produced a Carboniferous world that was diverse topographically and climatologically, perhaps only rivalled in that diversity by the late Cenozoic world. Furthermore, the Carboniferous was a time of the accumulation of vast coal deposits of great economic and societal significance. The temporal ordering of geological and biotic ev...
Basin-wide Diagenetic Patterns
By integrating the methods of different investagitive fields, this work gives us an interdisciplinary look at basic-scale subsurface fluid flow and its link to regional patterns of diagenesis, metasomatism, sedimentary ore deposits, and hydrocarbon accumulations. Issues addessed include the temporal evolution of hydrodynamic system, paleoflow conduits and their diagenetic products, subsurface fluid-rock interactions, the geochern-istry of basinal fluids, and heat flow in sedimentary basins. Paleo-fluid flow in both carbonate and siliciclastic systems is covered.
Understanding Earth's Deep Past
There is little dispute within the scientific community that humans are changing Earth's climate on a decadal to century time-scale. By the end of this century, without a reduction in emissions, atmospheric CO2 is projected to increase to levels that Earth has not experienced for more than 30 million years. As greenhouse gas emissions propel Earth toward a warmer climate state, an improved understanding of climate dynamics in warm environments is needed to inform public policy decisions. In Understanding Earth's Deep Past, the National Research Council reports that rocks and sediments that are millions of years old hold clues to how the Earth's future climate would respond in an environment ...
AAPG ... Annual Convention
Issue for 2000 includes also the abstracts of papers presented, in a separately-paged section.
Understanding Earth's Deep Past
There is little dispute within the scientific community that humans are changing Earth's climate on a decadal to century time-scale. By the end of this century, without a reduction in emissions, atmospheric CO2 is projected to increase to levels that Earth has not experienced for more than 30 million years. As greenhouse gas emissions propel Earth toward a warmer climate state, an improved understanding of climate dynamics in warm environments is needed to inform public policy decisions. In Understanding Earth's Deep Past, the National Research Council reports that rocks and sediments that are millions of years old hold clues to how the Earth's future climate would respond in an environment ...
