Response of Iberian Margin sediments to orbital and suborbital forcing over the past 420 ka

Author:

Hodell David1,Crowhurst Simon1,Skinner Luke1,Tzedakis Polychronis C.2,Margari Vasiliki2,Channell James E.T.3,Kamenov George3,Maclachlan Suzanne4,Rothwell Guy4

Affiliation:

1. Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences; University of Cambridge; Cambridge; UK

2. Department of Geography; University College London; London; UK

3. Department of Geological Sciences; University of Florida; Gainesville; Florida; USA

4. British Ocean Sediment Core Research Facility; National Oceanography Centre; Southampton; UK

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference82 articles.

1. A northern lead in the orbital band: North-south phasing of Ice-Age events;Alley;Quaternary Sci. Rev.,1989

2. Mineralogical composition of African dust delivered by red rains over northeastern Spain;Avila;J. Geophys. Res.,1997

3. 800,000 years of abrupt climate variability;Barker;Science,2011

4. Quantitative reassessment of brick red lutites: evidence from reflectance spectrophotometry;Barranco;Mar. Geol.,1989

5. Berger , A. M. F. Loutre 1999 Parameters of the Earth's orbit for the last 5 million years in 1 kyr resolution 10.1594/PANGAEA.56040

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