— Ch. 1 · Discovery And Nomenclature —
Last Interglacial.
~5 min read · Ch. 1 of 6
Pieter Harting stood in the Dutch countryside near Amersfoort during 1875 and examined boreholes that revealed a strange layer of sediment. He named this geological bed "Système Eémien" after the nearby river Eem, which flows through the region. The scientist noticed marine molluscan assemblages within these layers differed sharply from modern North Sea fauna. Many species found in these ancient beds now show distribution patterns stretching south to Portugal or into the Mediterranean. Harting's initial work established the foundation for identifying this warm period buried beneath glacial deposits. Subsequent researchers like Lorié in 1887 and Spaink in 1958 added detailed information about these molluscan groups. Van Voorthuysen described specific foraminifera from the type site while Zagwijn published palynology data in 1961. A multi-disciplinary investigation at the end of the 20th century re-investigated the original location using both old and new data. Scientists selected a parastratotype in the Amsterdam glacial basin known as the Amsterdam-Terminal borehole for further study. This team published uranium-thorium dating results showing late Last Interglacial deposits formed approximately 118,200 years ago with an error margin of 6,300 years.
Global Climate Dynamics
The Earth's orbital parameters shifted during the early phase of this interglacial period creating greater seasonal temperature variations across the Northern Hemisphere. Temperatures peaked between 128,000 and 123,000 years before present before declining steadily through the latter half of the interval. Arctic regions experienced temperatures roughly two to four degrees Celsius higher than conditions recorded in 2011. Greenlandic ice cores revealed pronounced temperature swings indicating highly unstable climate patterns during this era. Forests expanded northward reaching North Cape Norway which currently exists as tundra above the Arctic Circle. Hardwood trees including hazel and oak grew as far north as Oulu Finland during the peak warmth. A cooling event similar to but not exactly mirroring the 8.2-kiloyear event occurred at Beckentin within the E5 phase of the Eemian. Soil samples from Sokli in northern Finland identified abrupt cold spells around 120,000 years ago caused by shifts in the North Atlantic Current. These cold periods lasted hundreds of years and triggered significant vegetation changes across these northern regions. Winter temperatures rose throughout Northern Europe while summer temperatures fell over the course of the Last Interglacial. Meltwater from the Dnieper and Volga rivers connected the Black Sea and Caspian Sea during an insolation maximum spanning 133,000 to 130,000 BP.