Titlebook: ISSE 2009 Securing Electronic Business Processes; Highlights of the In Norbert Pohlmann,Helmut Reimer,Wolfgang Schneider Book 2010 Vieweg+T

SLUMP

含水層

Philip Hoyer‰) in glacial isotopic stages 2 to 4 and stage 6, and lower values (-20 to -21.2‰) in interglacial stages 1 and 5. Seasurface temperatures, derived from the alkenone U.. index, vary in the opposite sense, ranging from 20–22°C in glacial stages up to 24–26°C in interglacial stages. The inverse relati

dowagers-hump

滑動(dòng)

Detlef Houdeauic matter sedimenting to the sea floor. In the modern ocean, the natural abundance of .N (δ.N) varies in a regular way within planktonic ecosystems as a result of biological isotopic fractionation: the δ.N of the primary producers depends on the isotopic composition of the inorganic forms of nitroge