Item talk:Q238234
From geokb
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"abstract": "To explore the timing of hydrothermal activity at the Upper Geyser Basin (UGB) in Yellowstone National Park, we obtained seven new accelerator mass spectrometry (AMS) radiocarbon\u00a014C ages of carbonaceous material trapped within siliceous sinter. Five samples came from depths of 15\u2013152\u00a0cm within the Y-1 well, and two samples were from well Y-7 (depths of 24\u00a0cm and 122\u00a0cm). These two wells, at Black Sand and Biscuit Basins, respectively, were drilled in 1967 as part of a scientific drilling program by the U.S. Geological Survey (White et al., 1975). Even with samples as small as 15\u00a0g, we obtained sufficient carbonaceous material (a mixture of thermophilic mats, pollen, and charcoal) for the\u00a014C analyses. Apparent time of deposition ranged from 3775\u00a0\u00b1\u00a025 and 2910\u00a0\u00b1\u00a030\u00a014C years BP at the top of the cores to about 8000\u00a0years BP at the bottom. The dates are consistent with variable rates of sinter formation at individual sites within the UGB over the Holocene. On a basin-wide scale, though, these and other existing\u00a014C dates hint that hydrothermal activity at the UGB may have been continuous throughout the Holocene.",
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