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Books on the topic 'Radiolaria, Fossil. Marine sediments'

Author: Grafiati
Published: 4 June 2021
Last updated: 19 February 2022

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1

Shaw, Alan B. Distribution of mollusk shells in the sediments of Florida Bay. Ithaca, NY: Paleontological Research Institution, 2006.

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2

Campeau, S. Diatoms from the Beaufort Sea coast, southern Arctic Ocean (Canada): Modern analogues for reconstructing Late Quaternary environments and relative sea levels. Berlin: J. Cramer, 1999.

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3

Poore, Richard Z. Planktic foraminifer census data and [delta]18O and [delta]13C analyses of Globigerinoides ruber from Marine Isotope Stage 11 sediments from Ocean Drilling Program (ODP) Site 1002. [Reston, VA]: U.S. Geological Survey, 2000.

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4

Poore, Richard Z. Planktic foraminifer census data and [delta]18O and [delta]13C analyses of Globigerinoides ruber from Marine Isotope Stage 11 sediments from Ocean Drilling Program (ODP) Site 1002. [Reston, VA]: U.S. Geological Survey, 2000.

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5

Tröger, Karl-Armin. Upper Cretaceous (Cenomanian-Santonian) inoceramid bivalve faunas from the island of Bornholm, Denmark: With a review of the Cenomanian-Santonian lithostratigraphic formations and locality details. København: Danmarks Geologiske Undersøgelse, 1991.

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6

Smirnov, N. N. Istoricheskai︠a︡ ėkologii︠a︡ presnovodnykh zoot︠s︡enozov. Moskva: KMK. Tovarishchestvo nauch. izdaniĭ, 2010.

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7

Oliveira, Paulo Eduardo de, 1955- and Moreno Patiño Jorge Enrique, eds. Amazon pollen manual and atlas =: Manual e atlas palinológico da Amazônia. Amsterdam: Harwood Academic Publishers, 1999.

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8

Lan, Dongzhao. Nanhai wan di si ji chen ji gui zao. Xin hua shu dian Beijing fa xing suo fa xing, 1995.

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9

J, Schroeder, McMahon A, and Geological Survey (U.S.), eds. Planktic foraminifer census data and [delta]18O and [delta]13C analyses of Globigerinoides ruber from Marine Isotope Stage 11 sediments from Ocean Drilling Program (ODP) Site 1002. [Reston, VA]: U.S. Geological Survey, 2000.

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10

Coccolith-bearing late middle Eocene kerogen shale, Tillamook Highlands, Northwest Oregon Coast Range. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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11

David, Bukry, Wells Ray E, and Geological Survey (U.S.), eds. Coccolith-bearing late middle Eocene kerogen shale, Tillamook Highlands, Northwest Oregon Coast Range. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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12

David, Bukry, Wells Ray E, and Geological Survey (U.S.), eds. Coccolith-bearing late middle Eocene kerogen shale, Tillamook Highlands, Northwest Oregon Coast Range. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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13

David, Bukry, Wells Ray E, and Geological Survey (U.S.), eds. Coccolith-bearing late middle Eocene kerogen shale, Tillamook Highlands, Northwest Oregon Coast Range. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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14

Coccolith-bearing late middle Eocene kerogen shale, Tillamook Highlands, Northwest Oregon Coast Range. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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15

David, Bukry, Wells Ray E, and Geological Survey (U.S.), eds. Coccolith-bearing late middle Eocene kerogen shale, Tillamook Highlands, Northwest Oregon Coast Range. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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16

Coccolith-bearing late middle Eocene kerogen shale, Tillamook Highlands, Northwest Oregon Coast Range. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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17

Kirchman, David L. Introduction to geomicrobiology. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0013.

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Abstract:
Geomicrobiology, the marriage of geology and microbiology, is about the impact of microbes on Earth materials in terrestrial systems and sediments. Many geomicrobiological processes occur over long timescales. Even the slow growth and low activity of microbes, however, have big effects when added up over millennia. After reviewing the basics of bacteria–surface interactions, the chapter moves on to discussing biomineralization, which is the microbially mediated formation of solid minerals from soluble ions. The role of microbes can vary from merely providing passive surfaces for mineral formation, to active control of the entire precipitation process. The formation of carbonate-containing minerals by coccolithophorids and other marine organisms is especially important because of the role of these minerals in the carbon cycle. Iron minerals can be formed by chemolithoautotrophic bacteria, which gain a small amount of energy from iron oxidation. Similarly, manganese-rich minerals are formed during manganese oxidation, although how this reaction benefits microbes is unclear. These minerals and others give geologists and geomicrobiologists clues about early life on Earth. In addition to forming minerals, microbes help to dissolve them, a process called weathering. Microbes contribute to weathering and mineral dissolution through several mechanisms: production of protons (acidity) or hydroxides that dissolve minerals; production of ligands that chelate metals in minerals thereby breaking up the solid phase; and direct reduction of mineral-bound metals to more soluble forms. The chapter ends with some comments about the role of microbes in degrading oil and other fossil fuels.
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