Now showing items 1-9 of 9

    Issue DateTitleAuthor(s)
    23 February 2017The DeepMIP contribution to PMIP4: Experimental design for model simulations of the EECO, PETM, and pre-PETM (version 1.0)  Lunt, DJ; Huber, M; Anagnostou, E; et al.
    25 July 2019The DeepMIP contribution to PMIP4: methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data, incorporating version 0.1 of the DeepMIP database  Hollis, C; Dunkley Jones, T; Anagnostou, E; et al.
    26 September 2016Geochemical response of the mid-depth Northeast Atlantic Ocean to freshwater input during Heinrich events 1 to 4  Crocker, AJ; Chalk, TB; Bailey, I; et al.
    13 July 2023The history of ice-sheet retreat on North America during Termination 5: implications for the origin of the sea-level highstand during interglacial stage 11  Parker, RL; Foster, GL; Gutjahr, M; et al.
    4 April 2016Incursions of southern-sourced water into the deep North Atlantic during Late Pliocene glacial intensification  Lang, DC; Bailey, I; Wilson, PA; et al.
    25 May 2022Laurentide Ice Sheet extent over the last 130 thousand years traced by the Pb isotope signature of weathering inputs to the Labrador Sea  Parker, RL; Foster, GL; Gutjahr, M; et al.
    11 October 2014Response to “Comment to “The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site, by David Lang et al. Quaternary Science Reviews 93: 125-141””  Lang, DC; Bailey, I; Wilson, PA; et al.
    12 November 2015Tracking the provenance of Greenland-sourced, Holocene aged, individual sand-sized ice-rafted debris using the Pb-isotope compositions of feldspars and 40Ar/39Ar ages of hornblendes  White, LF; Bailey, I; Foster, GL; et al.
    2014The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site  Lang, DC; Bailey, Ian; Wilson, Paul A.; et al.