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CONTENTS 5<br />
5.1.4 Measuring depth dependent concentration profiles via fluorescent pH-indicator 147<br />
5.1.5 3D fluid flow measurement close to free water surfaces . . . . . . . . . . . . . . 148<br />
5.1.6 Small-scale turbulence in the sea-surface microlayer . . . . . . . . . . . . . . . 149<br />
5.1.7 Measurement of short wind waves . . . . . . . . . . . . . . . . . . . . . . . . . 150<br />
5.1.8 Spectroscopic Techniques for Gas-Exchange Measurements . . . . . . . . . . . 151<br />
6 Forschungsstelle “Radiometrie” of the Heidelberger Akademie der Wissenschaften155<br />
6.1 Forschungsstelle ”Radiometrie” of the Heidelberger Akademie der Wissenschaften . . . 157<br />
6.1.1 Modelling growth and isotopic composition of stalagmites . . . . . . . . . . . . 160<br />
6.1.2 A precisely dated climate record for the last 9 kyr from three high alpine stalagmites,<br />
Spannagel Cave, Austria . . . . . . . . . . . . . . . . . . . . . . . . . 161<br />
6.1.3 Measurement of 231 Pa in deep-sea sediments via ICP-MS and AMS . . . . . . . 162<br />
6.1.4 Ghost Resonance in Glacial Climate . . . . . . . . . . . . . . . . . . . . . . . . 163<br />
6.1.5 Dating and interpretation of climate proxies for three Holocene stalagmites from<br />
the South of Chile (Patagonia) . . . . . . . . . . . . . . . . . . . . . . . . . . . 164<br />
6.1.6 14 C in speleothems . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 165<br />
6.1.7 Precise dating of D/O-Events on a stalagmite from Socorta Island (Indian Ocean)166<br />
6.1.8 Trace element mapping of speleothems . . . . . . . . . . . . . . . . . . . . . . . 167<br />
6.1.9 U-series dating and paleoclimatic interpretation of the stable isotope profile of<br />
stalagmite ER76 from Grotta di Ernesto, Italy . . . . . . . . . . . . . . . . . . 168<br />
6.1.10 Kinetic Fractionation of Stable Isotopes in Speletothems - Laboratory Experiments169<br />
6.1.11 231 Pa/ 235 U-Dating of fossil corals with AMS . . . . . . . . . . . . . . . . . . . 170<br />
6.1.12 Reconstruction of the geomagnetic field strength over the past 300.000 years<br />
derived from 10 Be data of deep sea sediments from the North and South Atlantic<br />
Ocean . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 171<br />
Bibliography 177