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12 - Applications in geological monitoring: paleoseismology and paleoclimatology

Published online by Cambridge University Press:  05 July 2014

David B. Scott
Affiliation:
Dalhousie University, Nova Scotia
Jennifer Frail-Gauthier
Affiliation:
Dalhousie University, Nova Scotia
Petra J. Mudie
Affiliation:
Dalhousie University, Nova Scotia
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Summary

Key points

Coastal ecosystem knowledge is essential for understanding earthquake mechanics and forecasting catastrophic shoreline movement and flooding; multiple sources of fossil proxy-data – including microfossils, pollen and sediment – are best used to reconstruct patterns of earthquakes and tsunamis in time and space; multidisciplinary studies are also needed to distinguish tsunami from tropical storm events; correct measurement of timing and speed of paleoseismic events depend on accurate dating methods, best provided by tree roots and salt marsh peat; foraminifera provide the most precise estimates for amounts of vertical shoreline change; pollen of mangroves and salt marsh plants provide best estimates of climate change; diatom and dinoflagellate paleotransfer functions are best for tracking the prehistoric sea-ice changes.

How wetland archives are used in paleoseismology and paleotempestology

The past is all we know about the future.

(Barbara Kingsolver, The Lacuna, 2009)

In Chapters 3 and 4, we explained how study of foraminifera (Box 4.1 Tidal wetland foraminifera) and pollen grains (Figure 3.3) in present-day tidal wetlands can be used to analyse and interpret geological archives of past changes in sea level, salinity and coastal vegetation. Barlow et al. (2013, p. 90) state that, ‘Understanding late Holocene to present relative sea level changes at centennial or subcentennial scales requires geological records that dovetail with the instrumental era. Salt marsh sediments are one of the most reliable geological tide gauges.’ Here we give additional examples of other microfossils and geochemical tracers that can be used as proxies in studies of coastal wetlands, and we describe various case histories for applications in paleoseismology, which is the study of prehistoric earthquakes and tsunamis – particularly their location in space and time. Paleotempestology is the related study of storms and hurricanes from a primarily geological perspective (Liu, 2004, 2007).

Type
Chapter
Information
Coastal Wetlands of the World
Geology, Ecology, Distribution and Applications
, pp. 248 - 268
Publisher: Cambridge University Press
Print publication year: 2014

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