Oceanic Forcing of the Marine Isotope Stage 11 interglacial

Dickson, A.J.; Beer, C.J.; Demsey, C.; Maslin, M.; Bendle, J.A.; McClymont, E.L.; Pancost, R.D.

doi:10.1038/ngeo527

All Outputs (2)

The disappearance of Sphagnum imbricatum from Butterburn Flow: A reply to the comment of Bjorn Roebroek. (2009)
Journal Article
McClymont, E., Mauquoy, D., Yeloff, D., Broekens, P., van Geel, B., Charman, D., …Evershed, R. (2009). The disappearance of Sphagnum imbricatum from Butterburn Flow: A reply to the comment of Bjorn Roebroek. Holocene, 19(7), 1094-1097. https://doi.org/10.1177/0959683609345086

Oceanic Forcing of the Marine Isotope Stage 11 interglacial (2009)
Journal Article
Dickson, A., Beer, C., Demsey, C., Maslin, M., Bendle, J., McClymont, E., & Pancost, R. (2009). Oceanic Forcing of the Marine Isotope Stage 11 interglacial. Nature Geoscience, 2(6), 428-433. https://doi.org/10.1038/ngeo527

The interglacial known as Marine Isotope Stage 11 has been proposed to be analogous to the Holocene, owing to similarities in the amplitudes of orbital forcing. It has been difficult to compare the periods, however, because of the long duration of St... Read More about Oceanic Forcing of the Marine Isotope Stage 11 interglacial.