@article {38091,
	title = {Modern foraminifera, δ<sup>13</sup>C, and bulk geochemistry of central Oregon tidal marshes and their application in paleoseismology},
	journal = {Palaeogeography, Palaeoclimatology, Palaeoecology},
	volume = {377},
	year = {2013},
	note = {Most of this paper is concerned with a technical discussion of a method for making estimates of coastal subsidence following great earthquakes by using bulk geochemistry, delta-13-Carbon and correlations of foraminifera found in sediments with sediment elevations.  There is a brief discussion of the physical characteristics of Siletz Bay and a good review of distributions of present-day foraminifera, as well as what could be learned about the great earthquake of 1700.},
	month = {2013, May 1},
	pages = {p.13-27},
	keywords = {carbon, coastal hazards, earthquakes, foraminerifera, geology, Millport Slough, paleosciences, sea level, Siletz Bay, Siletz Spit, species list, subsidence, tsunamis, wetland vegetation},
	doi = {10.1016/j.palaeo.2013.02.032},
	author = {Engelhart, Simon E. and Horton, Benjamin P. and Vane, Christopher H. and Nelson, Alan R. and Witter, Robert C. and Brody, Sarah R. and Hawkes, Andrea D.}
}
