Reversed flow of Atlantic deep water during the Last Glacial Maximum. by Negre, C, Zahn, R, Thomas, A, Masqué, P, Henderson, G, Martínez-Méndez, G, Hall, I, Mas, J

I/Ca in epifaunal benthic foraminifera: A semi-quantitative proxy for bottom water oxygen in a multi-proxy compilation for glacial ocean deoxygenation by Lu, W, Rickaby, REM, Hoogakker, BAA, Rathburn, AE, Burkett, AM, Dickson, AJ, Martinez-Mendez, G, Hillenbrand, C-D, Zhou, X, Thomas, E, Lu, Z