ODP Site 747, central Kerguelen Plateau, contains a nearly complete record of the Middle Miocene Climate Transition (MMCT). Its unusually well preserved and rich foraminiferal assemblages have resulted in the MMCT interval at Site 747 becoming a focus of high-resolution paleoclimatic studies that have established this sequence as a Southern Ocean reference. We combine X-ray fluorescence (XRF) elemental counts of Fe, Ti, and Al and concentration-dependent magnetic parameters to trace volcanic ash input to sediments at ODP Hole 747A. We observe systematic variations in Al/Ti and Fe/Ti ratios that are consistent with increased primary productivity at times of increased terrigenous input and, therefore, increased nutrient supply. A spike in terrigenous material, which we interpret as volcanic ash, coincides with major changes in species abundance and stable oxygen and carbon isotopic shifts within the MMCT interval. This correlation suggests that nutrient flux associated with volcanic iron fertilization played a significant role in controlling phytoplankton communities at Site 747. We demonstrate that rapidly obtained XRF and magnetic parameters can provide useful proxies for terrigenous input and, therefore, nutrient fluxes in pelagic marine settings that can help to resolve local versus global drivers of paleoenvironmental and paleoceanographic changes. (C) 2014 Elsevier B.V. All rights reserved.