A 13 200 year history of century to millennial-scale paleoenvironmental change magnetically recorded in the Palmer, Deep, western Antarctic Peninsula

Keyphrases

• Paleoenvironmental Changes 100%
• Middle Holocene 100%
• Western Antarctic Peninsula 100%
• Millennial-scale 100%
• Deglaciation 60%
• Iron Oxide 60%
• Magnetic Susceptibility 60%
• Multi-domain 60%
• Magnetic Minerals 40%
• Low Field 40%
• Early Holocene 40%
• Mineral Assemblage 40%
• Late Holocene 40%
• Order of Magnitude 20%
• Increased Productivity 20%
• Source Rock 20%
• Gravel 20%
• Glacier 20%
• Grounding Line 20%
• High Field 20%
• Mineralogy 20%
• Ice-rafted Debris 20%
• Iceberg 20%
• Terrigenous Sediments 20%
• Glacimarine Sedimentation 20%
• Meltwater Plume 20%
• Paleoproductivity 20%
• Magnetic Parameters 20%
• Last Glacial Maximum 20%
• Titanomagnetite 20%
• Magnetic Particle Size 20%
• Single Domain 20%
• Neoglacial 20%
• Peninsula 20%
• Biogenic Silica 20%
• Density Sorting 20%
• Magnitude Change 20%
• Terrigenous Sedimentation 20%
• Scale Variation 20%

Earth and Planetary Sciences

• Holocene 100%
• Peninsula 100%
• Deglaciation 42%
• Magnetic Permeability 42%
• Multidomain 42%
• Magnetic Mineral 28%
• Early Holocene 28%
• Source Rock 14%
• Grounding Line 14%
• Mineralogy 14%
• Ice-Rafted Debris 14%
• Sea Level 14%
• Meltwater 14%
• Paleoproductivity 14%
• Last Glacial Maximum 14%
• Titanomagnetite 14%
• Neoglacial 14%
• Iceberg 14%
• Magnetic Domain 14%