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Figure 1.

Geographical location of the Galería site within the abandoned railway trench at Atapuerca, Spain.

The plan view of the Galería karstic complex shows the three conduits (Zarpazos: TZ, Galería: TG, and Tres Simas norte: TN) that have contributed to the infilling of the cavity.

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Figure 2.

Stratigraphic sequence of the cave deposits at Galería Complex.

(a) Ages/sample positions of teeth previously dated by combined ESR/U-series [15] and ages/sample positions of speleothem samples previously dated using U-series and/or ESR [11], [15], [104]. (b) Location of the luminescence dating samples and ages obtained in this study. Legend: (1) Cretaceous limestone; (2) Speleothem; (3) Main stratigraphic uncomformity – allostratigraphic unit (e.g., GII); (4) Lithologic/archaeo-palaeontological level (e.g., TG7); (5) Palaeomagnetic reversal; (6) Zarpazos – tentative GIa/GIb boundary; (7) Soil; (8) Clayey silt/small gravel boundary; (9) Gravels/breccia boundary; (10) Limestone clasts and boulders; (11) Organomineral layer (includes bat guano); (12) U-series and/or ESR speleothem samples; (13) ESR/U-series teeth samples; (14) Luminescence samples (this study).

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Table 1.

Allostratigraphic units and lithological levels (same nomenclature used to describe archaeo-palaeontological levels) for Galería, together with the position of the luminescence dating samples analysed in this study.

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Table 2.

Final luminescence ages obtained for the Galería samples in this study.

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Figure 3.

Photos showing the location of the luminescence dating samples and the types of deposits investigated at Galería.

(a) and (c) show the sampling positions in unit GIII; (b) shows the stratigraphic sequence sampled at Covacha Zarpazos (northern wall); (d) sampling of the upper guano in unit GIIa (level TN2A); (e) and (f) shows sampling of the lower part of unit GIIa (level TG7).

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Table 3.

Environmental dose rate values for the quartz and K-feldspar fractions measured in this study.

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Table 4.

SAR protocols used in this study to obtain ages from quartz (protocol A) and K-feldspars (protocol B).

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Figure 4.

Selected examples of dose-response curves and signal decay curves.

(a-d) TT-OSL single-grain measurements and (e-f) pIR-IR225 measurements of the Galería samples.

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Table 5.

Summary of single-grain TT-OSL and multi-grain pIR-IR225 De values for the Galería samples.

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Figure 5.

Examples of single-grain TT-OSL De distributions plotted as histograms (logarithmic x-axis) and radial plots.

Data is shown for selected Galería samples. See Figure S4 in File S1 for the De datasets of all other samples.

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Figure 6.

Radial plots showing pIR-IR225 De distributions of representative Galería samples.

See Figure S5 in File S1 for the De datasets of all other samples.

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Figure 7.

Published ages obtained using different dating methods (including this study) for the various allostratigraphic units and lithologic/archaeo-palaeontological levels at Galería.

The data included here has been derived from combined ESR/U-series dating of teeth [15], TL and IRSL dating of sediment [14], ESR dating of calcite/speleothems [11], [104], U-series dating of calcite/speleothems [11], [15]. The numerical age estimates are shown against the Marine Oxygen Isotope curve record [94]. Two additional TL ages of 1340±170 ka (unit GIV) and 3000±1800 ka (unit GI) [14] are not shown on this plot as they lie beyond the x-axis limits (see Table 2 for a full summary of the dataset in [14]).

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