The pacing of the global climate system by variations in orbital parameters is clearly demonstrated in the timing and specific patterns of various geoarchives, including sapropels, glacial/interglacial cycles and many other examples. The imprint of astronomical cycles can be used as high-precision geochronometer, and as paleoclimatic information. Extreme events can especially be expected to relate to extremes in insolation. We invite contributions utilizing the imprint of Milankovic cycles as preserved in the geological record in...