A re-evaluation of the palaeoclimatic significance of phosphorus variability in speleothems revealed by high-resolution synchrotron micro XRF mapping

- Frisia, S., Borsato, A., Drysdale, R. N., Paul, B., Greig, A., Cotte, M.

Evidence for obliquity forcing of glacial termination II

- Drysdale, R. N., Hellstrom, J. C., Zanchetta, G., Fallick, A. E., Sánchez Goñi, M. F., Couchoud, I., McDonald, J., Maas, R., Lohmann, G., Isola, I.

Increasing Australian-Indonesian monsoon rainfall linked to early Holocene sea-level rise

- Griffiths, M. L., Drysdale, R. N., St Pierre, E., Fischer, M. J., Suwargadi, B. W., Gagan, M. K., Zhao, J.-x., Ayliffe, L. K., Hellstrom, J. C., Hantoro, W. S., Frisia, S., Feng, Y.-x., Cartwright, I.

The environmental features of the Monte Corchia cave system (Apuan Alps, central Italy) and their effects on speleothem growth

- Piccini, L., Zanchetta, G., Molli, G., Lotti, L., Roncioni, A., Regattieri, E., Meccheri, M., Vaselli, L., Drysdale, R. N., Hellstrom, J., Isola, I., Fallick, A. E., Leone, G., Doveri, M., Mussi, M., Mantelli, F.

Enhanced rainfall in the Western Mediterranean during deposition of sapropel S1: stalagmite evidence from Corchia cave (Central Italy)

- Zanchetta, G., Drysdale, R. N., Hellstrom, J. C., Fallick, A. E., Isola, I., Gagan, M. K., Pareschi, M. T.

An environmental model of fluvial tufas in the monsoonal tropics, Barkly karst, northern Australia

- Carthew, K. D., Taylor, M. P., Drysdale, R. N.

Are current models of tufa sedimentary environments applicable to tropical systems?: a case study from the Gregory River

- Carthew, K. D., Taylor, M. P., Drysdale, R. N.