Climate of the Little Ice Age and the past 2000 years in northeast Iceland inferred from chironomids and other lake sediment proxies

Keyphrases

• Chironomids 100%
• Little Ice Age 100%
• Lake Sediments 100%
• Iceland 100%
• Diptera Chironomidae 100%
• Sedimentary Proxies 100%
• Past 2000 Years 100%
• Chironomid Assemblages 60%
• Nineteenth Century 40%
• Data Assemblage 40%
• Biogenic Silica 40%
• Detrended Correspondence Analysis 40%
• 18th Century 20%
• Soil Erosion 20%
• Environmental Change 20%
• Sedimentary Record 20%
• 20th Century 20%
• Carbon-nitrogen 20%
• Climate History 20%
• Historical Documents 20%
• Temperature Variation 20%
• Temperature Shift 20%
• Total Organic Carbon 20%
• Carbon to Nitrogen Ratio 20%
• Instrumental Records 20%
• Carbon-silica Composites 20%
• Subfossil 20%
• Silica Content 20%
• Glacier Extent 20%
• Silica Concentration 20%
• Instrumental Climate 20%
• Proxy Reconstruction 20%
• 11th Century 20%
• 13th Century 20%
• Lake Productivity 20%
• 10th Century 20%
• First Millennium Ad 20%
• Sea Ice Extent 20%
• Paleolimnological Proxies 20%
• Glacier Reconstruction 20%
• Temperature Transfer Function 20%
• Calibration Site 20%

Earth and Planetary Sciences

• Lacustrine Deposit 100%
• Little Ice Age 100%
• Iceland 100%
• Correspondence Analysis 50%
• Environmental Change 25%
• Subfossil 25%
• Organic Carbon 25%
• Transfer Function 25%