Detlev K. Richter

TL;DR: In this article, an overview of cathodoluminescence (CL) studies in the last three decades due to the application of enhanced methods such as high-resolution spectroscopy is presented.

TL;DR: In this paper, the authors present a complete analytical dataset of magnesium isotopes (δ 26 Mg) from a monitored cave in NW Germany (Bunker Cave), which includes δ 26 mg values of loess-derived soil above the cave (−1.0 ǫ± 0.5‰), soil water (− 1.8 mdr.

TL;DR: In this paper, a monitoring program performed in Bunker Cave (NW Germany), which includes monthly collection of climatological data as well as air and water samples from the cave and the overlying soil since 2006, is a prerequisite for the interpretation of speleothem data from Bunker Cave in terms of climate variability.

TL;DR: In this paper, the influence of mineralogy, taxonomy and environmental factors (e.g., seawater isotopic composition, temperature, salinity) on magnesium-isotopic (δ26Mg) ratios of skeletal carbonates was explored.

TL;DR: In this paper, the authors used well-established isotope systems (δ18O, δ13C, 87Sr/86Sr), fluid inclusions and elemental data, as well as a detailed sedimentological and petrographic data set, to establish the precipitation environment and subsequent diagenetic pathways of a series of Proterozoic to Pleistocene syn-depositional marine evaporative (sabkha) dolomites.