Item talk:Q245022
From geokb
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"abstract": "We describe the modern distribution of salt-marsh and tidal-flat foraminifera from Sitkinak Island (Trinity Islands) and Simeonof Island (Shumagin Islands), Alaska, to begin development of a dataset for later use in reconstructing relative sea-level changes caused by great earthquakes along the Alaska-Aleutian subduction zone. Dead foraminifera were enumerated from a total of 58 surface-sediment samples collected along three intertidal transects around a coastal lagoon on Sitkinak Island and two intertidal transects on Simeonof Island. Two distinctive assemblages of salt-marsh foraminifera were recognized on Sitkinak Island.\u00a0Miliammina fusca\u00a0dominated low-marsh settings and\u00a0Balticammina pseudomacrescens\u00a0dominated the high marsh. These two species make up >98% of individuals. On Simeonof Island, 93% of individuals in high-marsh settings above mean high water were\u00a0B. pseudomacrescens. The tidal flat on Simeonof Island was dominated by\u00a0Cibicides lobatulus\u00a0(60% of individuals), but the lower limit of this species is subtidal and was not sampled. These results indicate that uplift or subsidence caused by repeated earthquakes along the Alaska-Aleutian subduction zone could be reconstructed in coastal sediments using alternating assemblages of near monospecific\u00a0B. pseudomacrescens\u00a0and low-marsh or tidal-flat foraminifera.",
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