Description
Working with "four well-preserved continuous sediment sequences from the southern flank of the Skagerrak [approximately 57.8-58.2°N, 8.6-9.6°E]," which he describes as "a current-controlled sedimentary basin between the North and Baltic Seas," the author carried out "granulometric and stable oxygen isotope analyses." This work revealed the past presence of the Medieval Warm Period (AD 800-1350), which, in his words, "was characterized by warm summers, mild winters and little storm activity."