Electronic Supplement to
Liquefaction Features Produced by the 2010–2011 Canterbury Earthquake Sequence in Southwest Christchurch, New Zealand, and Preliminary Assessment of Paleoliquefaction Features

by P. Villamor, P. Almond, M. P. Tuttle, M. Giona-Bucci, R. M. Langridge, K. Clark, W. Ries, S. H. Bastin, A. Eger, M. Vandergoes, M. C. Quigley, P. Barker, F. Martin, and J. Howarth

Table S13. Radiocarbon Dates

Sample Number
Lab Number*
13C/12C Ratio 14C Age (yr B.P.) 95% HPDF Calendar Age Range (cal B.P.) 95% HPDF Range for Calibrated Calendar Age (A.D./B.C.) Sample Description
Hardwick
HWK T4a-C2
NZA 50181
−26.4 ± 0.1 4659 ± 24 5465–5146 3516–3197 B.C. HWK 4a trench
Small piece of wood from 1.86 m depth.
HWK T5-C1
NZA 50177
−24.5 ± 0.1 628 ± 18 632–545 A.D. 1318–1405 HWK 5 trench
Pieces of reed from the bottom sedge in unit 7bOh1.
HWK T6-C5
NZA 50335
−24.5 ± 0.1 2004 ± 18 1997–1841 48 B.C.–A.D. 109 HWK 6E trench
Charcoal from paleosol, unit 6bA.
HWK T6-C6
NZA 50179
−23.9 ± 0.1 1133 ± 18 1058–935 A.D. 893–1015 HWK 6E trench
Large piece of wood from L2 (maximum age for paleosand blow).
HWK T6-C7
NZA 50176
−25.8 ± 0.1 668 ± 18 650–556 A.D. 1300–1395 HWK 6E trench
Clods of peat from unit 5Cg above L2 (minimum age for paleosand blow).
HWK T6-C10
NZA 50336
−25.2 ± 0.1 641 ± 20 639–546 A.D. 1311–1404 HWK 6E trench
Large piece of wood, burned. Tree in growth position, growing on unit 6bA.
HWK T6-C12
NZA 50180
−24.6 ± 0.1 721 ± 18 66–567 A.D. 1282–1383 HWK 6W trench
Medium piece of wood (in growth position? rooted in unit 6bA but extended into unit 5Cg above; tree may have survived paleoearthquake).
HWK T6-C14
NZA 50371
−24.7 ± 0.1 641 ± 19 636–547 A.D. 1314–1404 HWK 6E trench
Wood from horizontal tree likely previously rooted in unit 6bA; first dark brown ring.
HWK 6-C1-T2-S1 −25.53 2932 ± 20 3144–2925 B.C. 1195–976 HWK 6-1 core
Sedge and grass fragments. 2.91 m deep from top of the core (51 cm along tube 2; 3.9 m below surface).
HWK 6-C2-T2-S1 −28.12 398 ± 17 493–237 A.D. 1457–1624 HWK 6-2 core
Plant material (roots at the base). 2.17 deep from top of the core (70 cm along tube 2; 3.6 m below surface).
Marchand
MAR T1-C2b
NZA 50175
−27.9 ± 0.1 263 ± 17 310–153 A.D. 1640–1798 MAR 1E trench
Peat with root and pieces of wood; dated reed material; from 2.7 m below surface (initial deeper excavation).
MAR T1-C6
NZA 50178
−25.2 ± 0.1 861 ± 18 763–682 A.D. 1187–1268 MAR 1E trench
Lumps of sediment with embedded fragments of charcoal; dated charcoal fragments; from unit 4Cg (~1.30 m deep).
MAR 1-C1-T2-S1
NZA 54014
−26.6 1009 ± 18 926–802 A.D. 1024–1148 MAR 1 core
Wood. 1.82 deep from top of the core (19 cm along tube 2; 2.9 m below surface).
MAR T3-C1
NZA 50334
−24.7 ± 0.1 1038 ± 20 956–809 A.D. 995–1141 MAR 3 trench.
Tiny fragments of charcoal from unit C(g) (sand hosting paleoliquefaction).
MAR T3-C2
NZA 50670
−32.5 ± 0.1 8872 ± 72 10,179–9631 8230–7682 B.C. MAR 3 trench.
Unit L2 (paleoliquefaction dike).
MAR 4-C1-T1-S1
NZA 54015
−26.6 709 ± 19 665–564 A.D. 1286–1386 MAR 4 core.
Plant material. 1.77 m below surface (BS; 44 cm along tube 1).
MAR 4-C1-T2-S1
NZA 54016
−29.4 1918 ± 20 1877–1745 A.D. 73–206 MAR 4 core.
Plant material. 3.06 m BS (73 cm along tube 2).

* NZA, New Zealand radiocarbon number.

Conventional radiocarbon ages in years B.P. or before present (1950) determined by NZA.

HPDF, highest probability density function. Calibrated age ranges as determined using OxCal v.4.2.4 (Bronk Ramsey, 2009) and southern hemisphere atmospheric data from Hogg et al. (2013). Ranges represent two standard deviation statistics or 95% probability.

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