Groundwater discharge to a Gobi desert lake during Mid and Late Holocene dry periods

Atlantic surface water inflow to the Nor

Atlantic surface water inflow to the Nordic seas during the Pleistocene–Holocene transition (mid–late Younger Dryas and Pre-Boreal periods, 12 450–10 000 a BP)

✍ Tine L. Rasmussen; Erik Thomsen; Tove Nielsen; Stefan Wastegård 📂 Article 📅 2011 🏛 John Wiley and Sons 🌐 English ⚖ 909 KB

## Abstract The inflow of Atlantic Water to the Nordic seas from mid–late Younger Dryas to earliest Holocene (12 450–10 000 a BP) is reconstructed on the basis of a high‐resolution core (LINK14) from 346 m water depth on the east Faroe shelf. We have analysed the distribution of planktic and benthi