Tracing sediments back to their catchment sources using biogeochemical and physical
fingerprints involves multiple assumptions. One of the most fundamental assumptions is that …

Colour is a fundamental property of sediment and is often used for lithographic description to
determine sedimentological structures, facies etc. However, the sedimentary information …

In this study, we present new detailed biomarker‐based sea ice records from two sediment
cores recovered in the Chukchi Sea and the East Siberian Sea. These new biomarker data …

Sediment cores from the western Arctic Ocean obtained on the 2005 HOTRAX and some
earlier expeditions have been analyzed to develop a stratigraphic correlation from the …

Airborne mineral dust is sensitive to climatic changes, but its response to orbital forcing is
still not fully understood. Here, we present a reconstruction of dust input to the Subarctic …

A study of three long cores from the outer shelf and continental slope north of Alaska in the
Arctic Ocean indicate that localized drift deposits occur here with sedimentation rates of …

Paleoenvironments during the late Younger Dryas through early Holocene retreat of the
Greenland Ice Sheet from the outer shelf in the Disko Trough system of central West …

Global surface temperature changes and their drivers during the Holocene Epoch remain
controversial. Syntheses of proxy data indicate that global mean annual temperature …

Sediment core ARC4-BN05 collected from the Canada Basin, Arctic Ocean, covers the late
to middle Quaternary (Marine Isotope Stage–MIS–1–15, ca. 0.5–0.6 Ma) as estimated by …

Both statistical methods and artificial neural network (ANN) have been used for lithology or
facies clustering. ANN, in particular, has increasingly gained popularity for clustering of …