Progress in Earth and Planetary Science

Table 2 Depositional ages of the event deposits (E1–E16) estimated by the Bayesian age-depth model

From: Marine inundation history during the last 3000 years at Lake Kogare-ike, a coastal lake on the Pacific coast of central Japan

Core location	Name of event deposits	Corrected depth below the lake bottom (cm)	Calibrated depositional age (95% credible interval, cal BP)	Calibrated depositional age (95% credible interval, cal CE/BCE)
K-4	E1	46.9	100-present	1850–1960 CE
K-4	E2	109.8	330–164	1620–1786 CE
K-4	E3	121.7	394–277	1556–1673 CE
K-4	E4	138.4	430–338	1520–1612 CE
K-4	E5	148.5	535–412	1415–1538 CE
K-4	E6	171.5	818–675	1132–1275 CE
K-4	E7	182.7	871–704	1079–1246 CE
K-4	E8	220.5	1243–1070	707–880 CE
K-4	E9	230.3	1273–1154	677–796 CE
K-4	E10	249.5	1354–1279	596–671 CE
K-4	E11	258.6	1396–1320	554–630 CE
K-4	E12	277.9	1503–1367	447–583 CE
K-4	E13	286	1558–1399	392–551 CE
K-4	E14	287.7	1569–1404	381–546 CE
K-4	E15	321.4	2267–1976	317–26 BCE
K-4	E16	331.6	2615–2385	665–435 BCE

The model was consructed using Bchron (Haslett and Parnell 2008; Parnell et al. 2008). Event deposits were treated as instantaneous deposits, and their thickness were removed from the original core log of K-4. “Corrected depth below the lake bottom” represents the event-free depth

Back to article page