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Showing 1–5 of 5 results
Advanced filters: Author: Frederik Schenk Clear advanced filters

  • Thousands of years long droughts have occurred in eastern North America during the Holocene (past 12,000 years). The authors link the droughts to the impacts of the Laurentide Ice Sheet and the following period of warmer-than-present temperatures.

    • J. Sakari Salonen
    • Frederik Schenk
    • Miska Luoto
    ResearchOpen Access
    Nature Communications
    Volume: 16, P: 1-14

  • Mechanisms causing the Younger Dryas cold reversal have been questioned by inconsistencies between proxy and modelling results. Here, the authors show that the concept of a strong North Atlantic Ocean cooling event as major driver is consistent with warm European summers caused by intensified atmospheric blocking.

    • Frederik Schenk
    • Minna Väliranta
    • Barbara Wohlfarth
    ResearchOpen Access
    Nature Communications
    Volume: 9, P: 1-13

  • The warm Last Interglacial led to a seasonally ice-free Arctic Ocean and a transformation to Atlantic conditions, according to planktic foraminifera records from central Arctic Ocean sediment cores.

    • Flor Vermassen
    • Matt O’Regan
    • Helen K. Coxall
    ResearchOpen Access
    Nature Geoscience
    Volume: 16, P: 723-729

  • In many solution systems, nanometre-sized structural units are present before nucleation, but little is known about these pre-nucleation clusters. Habraken et al.show that, for the crystallization of calcium phosphate, these nanometre-sized units are calcium triphosphate complexes.

    • Wouter J. E. M. Habraken
    • Jinhui Tao
    • Nico A. J. M. Sommerdijk
    Research
    Nature Communications
    Volume: 4, P: 1-12