Chemical profiles from Greenland ice cores show that the frequency of volcanism was
higher during the last glacial-interglacial transition (LGIT) and early Holocene,(17–9 ka b2k) …

Contiguous sampling of Holocene ice from the NGRIP core, Greenland, has revealed a new
rhyolitic cryptotephra that is geochemically identical to the KHG tephra, a widespread marker …

Large volcanic eruptions occurring in the last glacial period can be detected by their
accompanying sulfuric acid deposition in continuous ice cores. Here we employ continuous …

The last glacial period is characterized by a number of millennial climate events that have
been identified in both Greenland and Antarctic ice cores and that are abrupt in Greenland …

Volcanic eruptions are a key source of climatic variability, and reconstructing their past
impact can improve our understanding of the operation of the climate system and increase …

Integrating proximal and medial-distal tephra records from continuous sedimentary archives
has recently proven to be crucial for obtaining more complete and highly resolved …

Two cores were sampled in the Fucino Basin (central Apennines, Italy), which represents an
extensional intramountain basin filled by Pliocene to Quaternary continental alluvial and …

Laboratory experiments showed that the isotopic fractionation of δ 13 C and of δ 18 O during
calcite formation of planktic foraminifera are species-specific functions of ambient CO 3 2 …

Tephrochronology is a powerful tool used to synchronise and date stratigraphic records by
accurate and precise geochemical analysis of deposited volcanic glass shards. However, in …

In this study, insoluble microparticles from four discrete layers of ice-cores drilled out from
the East Rongbuk glacier of the Himalayas were characterized on a single particle basis by …