Titlebook: Marine Geochemistry; Horst D. Schulz,Matthias Zabel Textbook 20001st edition Springer-Verlag Berlin Heidelberg 2000 Fühdiagenese.Ocean.Oze

Liability

異端邪說(shuō)下

Horst D. Schulznd fibrohistiocytic tumors; biphasic (epithelial/mesenchymal) tumors; chondroid and osseous tumors; and other mesenchymal neoplasms. This chapter will be presented from the practical point of view for the practicing pathologist who may be called upon to interpret these tumors. Clinical, pathological

Thyroiditis

增強(qiáng)

The Solid Phase of Marine Sediments,olved material consolidates by means of biological and geochemical processes and is deposited on the ocean floor along with the particulate matter from weathered rock. The ocean floor deposits therefore embody the history of the continents, the oceans and their pertaining water masses. They therefor

Mosaic

結(jié)合

hereditary

goodwill

Bacteria and Marine Biogeochemistry, Redox reactions between oxidants such as atmospheric oxygen or manganese oxide and reductants such as ammonium or sulfide may proceed by chemical reaction, but they are most often accelerated by many orders of magnitude through enzymatic catalysis in living organisms. Throughout Earth’s history, pr

夾死提手勢(shì)

chondromalacia

The Reactivity of Iron,rface of the bio- and geosphere. Similar to manganese (Chap. 11), iron occurs in two valence states as oxidized ferric iron, Fe(III), and reduced ferrous iron, Fe(II). Two principal biological processes are of importance: Microorganisms such as magnetotactic bacteria or phytoplankton (Chap. 2.2 and