Chironomid assemblages and inferred summer temperature from the Last Glacial Period (ca. 98–46 ka), from Füramoos, Southern Germany

<p>The data herein presents a new chironomid record and associated chironomid-based temperature reconstruction covering the time interval ca. 98–46 ka from the palaeolake Füramoos, Southern Germany. These data also include non-chironomid invertebrate remains, including Ceratopogonidae, Daphnia and Ephemeroptera as well as Characean oospores.</p>