Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Liao, Jin; Day, Christopher (2026): Calcium isotopes (δ44Ca) of stalagmite HS4 in Heshang Cave, Central China [dataset]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.992726 (DOI registration in progress)

Always quote citation above when using data! You can download the citation in several formats below.

Published: 2026-03-16

RIS CitationBibTeX Citation ShareShow MapGoogle Earth

Abstract:
Stalagmite calcium (d44Ca) isotope data was used to reconstruct regional paleorainfall amount in the Central China between 4.6 kyr BP and 3.5 kyr BP. The stalagmite (HS4) was collected from Heshang Cave in the Middle Yangtze Valley, Central China (30º27′N, 110º25′E, 294 m.a.s.l). HS4 Stalagmite length in this study ranges between 112.63 and 151.03 cm. The working half of HS4 was slabbed. Micro drilling of 343 continuous samples was undertaken by using a New-Wave Micromill. Every eighth sample was measured for d44Ca. The measurement resolution is ~25 years. The data was measured using a Nu Instruments multicollector inductively coupled plasma mass spectrometer (MC-ICP-MS) at the University of Oxford, Department of Earth Sciences in 2016.
Keyword(s):
Archaeological cultures; Calcium isotopes; Central China; speleothem; trace elements
Related to:
Liao, Jin; Day, Christopher; Hu, Chaoyong; Liu, Y; Henderson, Gideon M (2026): Precise chronology of hydrological changes at ∼4.2 kyr in Central China to assess the impact of flooding on Neolithic societies. National Science Review, 13(2), nwaf567, https://doi.org/10.1093/nsr/nwaf567
References:
Owen, R A; Day, C C; Hu, C-Y; Liu, Y-H; Pointing, M D; Blättler, Clara L; Henderson, G M (2016): Calcium isotopes in caves as a proxy for aridity: Modern calibration and application to the 8.2 kyr event. Earth and Planetary Science Letters, 443, 129-138, https://doi.org/10.1016/j.epsl.2016.03.027
Funding:
National Natural Science Foundation of China (NSFC), grant/award no. 41731177
National Natural Science Foundation of China (NSFC), grant/award no. 41902185
Coverage:
Latitude: 30.450000 * Longitude: 110.416700
Minimum DISTANCE: 115.70 cm * Maximum DISTANCE: 147.06 cm
Event(s):
Heshang_Cave_HS4 * Latitude: 30.450000 * Longitude: 110.416700 * Elevation: 294.0 m * Location: Yangtze Valley, Central China * Method/Device: Speleothem sample (SPS)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample numberSample noLiao, Jin
AGEAgeka BPLiao, JinAge, Uranium-ThoriumGeocode – Measured with: Multicollector inductively coupled plasma mass spectrometer (MC-ICP-MS), Nu Instruments, Plasma
Age, errorAge e±Liao, JinAge, 14C calibration OxCal (Ramsey, 2008)2 standard deviation (2SD), 2 sigma
DISTANCEDistancecmLiao, JinMeasuredGeocode – From top of HS4
δ44/42 Caδ44/40 CaLiao, JinInductively coupled plasma mass spectrometer (ICP-MS), Attom, Nu InstrumentsWith respect to NIST SRM 915A
δ44/42 Ca, errorδ44/40 Ca e±Liao, JinCalculated, 2 standard deviation (2SD)With respect to NIST SRM 915A; 2 sigma
Rayleigh fractional model, crystallizationfLiao, JinAccording to Owen et al. (2016)Fraction of dissolved Ca remaining in solution
Rayleigh fractional model, crystallization, errorf e±Liao, JinCalculated, 2 standard deviation (2SD)Fraction of dissolved Ca remaining in solution; 2 sigma
Precipitation, annual totalPrecip annual totmm/aLiao, JinAccording to Owen et al. (2016)Derived rainfall calculated by the fraction of dissolved Ca remaining in solution
10 Precipitation, annual total, errorPrecip annual total e±Liao, JinCalculated, 2 standard deviation (2SD)Derived rainfall calculated by the fraction of dissolved Ca remaining in solution; 2 sigma
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
344 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Sample no

Age [ka BP]

Age e [±]

Distance [cm]

δ44/40 Ca []

δ44/40 Ca e [±]

f

f e [±]

Precip annual tot [mm/a]
10 
Precip annual total e [±]
HS4-I-34.59580147.060.150.060.550.0581193
HS4-I-114.57178146.320.080.060.610.06949143
HS4-I-194.54675145.580.110.060.580.06880116
HS4-I-274.52272144.850.180.060.520.0577080
HS4-I-354.49671144.130.110.060.590.06887119
HS4-I-434.46972143.400.140.060.550.0582698
HS4-I-514.44172142.680.090.060.600.06922132
HS4-I-594.41274141.950.120.060.570.05860110
HS4-I-674.38080141.230.200.060.510.0574773
HS4-I-754.34785140.460.310.060.420.0463945
HS4-I-834.31491139.720.120.060.570.05866111
HS4-I-914.29192138.970.120.060.580.05869113
HS4-II-34.27490138.230.200.060.500.0574372
HS4-II-114.25788137.480.120.060.570.05856108
HS4-II-194.24086136.740.200.060.510.0574573
HS4-II-274.22284135.990.290.060.440.0465649
HS4-II-354.19285135.090.210.060.500.0573770
HS4-II-434.16486134.250.260.060.460.0468456
HS4-II-514.13987133.490.250.060.470.0469358
HS4-II-594.11387132.730.250.060.460.0468656
HS4-II-674.08987131.890.130.060.560.05843104
HS4-II-754.06888131.120.190.060.510.0575174
HS4-II-834.04788130.390.060.060.630.061005166
HS4-II-914.02788129.660.180.060.520.0576980
HS4-III-34.00788128.920.110.060.580.06882117
HS4-III-113.98689128.200.080.060.610.06936138
HS4-III-193.96687127.470.140.100.560.09832167
HS4-III-273.94682126.730.020.100.670.111120363
HS4-III-353.92676126.000.070.100.620.10969251
HS4-III-433.90570125.270.070.100.620.10976256
HS4-III-513.88564124.540.030.100.660.101082334
HS4-III-593.86359123.810.010.100.690.111179413
HS4-III-673.81859123.080.150.100.550.09817158
HS4-III-753.77460122.350.100.100.590.09903208
HS4-III-833.73060121.620.080.100.610.10936229
HS4-III-913.68661120.880.050.100.640.101021288
HS4-IV-33.64161120.150.080.100.610.10942233
HS4-IV-113.59762119.420.020.100.670.111132373
HS4-IV-193.57959118.650.110.100.580.09877192
HS4-IV-273.56957117.910.330.080.410.0562656
HS4-IV-353.55853117.180.290.080.440.0665866
HS4-IV-433.54851116.440.150.080.540.07807122
HS4-IV-513.53159115.700.200.080.510.0674898