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Distinguishing storm or fire events in historic sediments. Willy Amidon, Eric Butler. Introduction. • Lake sediments record past events • Coring allows study of these records. Previous work. Brown (2000), Noren (2001) used long (6m) cores to reconstruct paleoclimate and environment
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Distinguishing storm or fire events in historic sediments Willy Amidon, Eric Butler
Introduction • Lake sediments record past events • Coring allows study of these records Previous work Brown (2000), Noren (2001) used long (6m) cores to reconstruct paleoclimate and environment - identified coarse, inorganic sediment layers - interpreted as storm events OUR PURPOSE: Distinguish fire events from storm events
Goals Use short cores (< 40cm) to: • Quantify historic charcoal levels • Identify historic/prehistoric boundary • Interpret any “storm” layers found • Refine lab techniques
Methods of analysis • Visual logs - Changes in color, density, grain size, debris • Loss on Ignition (LOI) - Identifies trends in organic carbon content • Charcoal analysis - Elemental analyzer quantifies elemental carbon (charcoal)
Coring method • Gravity cores from canoe • Extrude in the field • Cores separated into 1 cm intervals
Sample preparation • Dry samples & weigh • Digest in nitric acid - removes organic carbon • Rinse & dry, weigh • Elemental analyzer - measures elemental carbon (charcoal)
Results • Incomplete digestion (SY) • Incomplete washing (SY, OG)
Alternate methods • Visual log on OG core • LOI on OG core Results • Correlation between LOI and organic material • Suggests a storm/fire layer? • May also represent logging
Coming soon • Elemental analysis on rewashed samples - % charcoal content • Hopeful correlation with LOI and visual log - Does increase in charcoal correlate with decrease in LOI & color change?
Future work • Apply procedure to longer cores • Pb210 dating of macrofossils (wood chips) • Analyze & compare more short cores