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Title: Strontium isotopic composition of estuarine sediments as paleosalinity-paleoclimate indicator

Journal Article · · Science (Washington, D.C.); (United States)
 [1];  [2]
  1. Stanford Univ., CA (United States) Univ. of California, Berkeley (United States)
  2. Univ. of California, Berkeley (United States)

The strontium isotopic composition of biogenic precipitates that occur in estuarine sediments can be used as proxy indicator of paleosalinity and for assessing precipitation and river discharge rates over thousands of years. In the San Francisco Bay estuary, river water with low {sup 87}Sr/{sup 86}Sr ratio (average, 0.7065) and low Sr concentration (0.13 parts per million) mixes with seawater with a higher {sup 87}Sr/{sup 86}Sr ratio (0.7092) and Sr concentration (7.9 parts per million). The predicted mixing relation between salinity and Sr isotopic composition is confirmed by measurements of modern estuarine surface waters. A paleosalinity record obtained from foraminifera for the ancestral San Francisco Bay during oxygen isotope substage 5e of the last interglacial reflects a global rise and fall of sea level, and short time-scale variations related to fluctuations in discharge rates of the Sacramento and San Joaquin rivers.

OSTI ID:
7114331
Journal Information:
Science (Washington, D.C.); (United States), Vol. 255:5040; ISSN 0036-8075
Country of Publication:
United States
Language:
English