Table 1 OSL results and sample information

From: Fraser Island (K'gari) and initiation of the Great Barrier Reef linked by Middle Pleistocene sea-level change

Map code

Lab code

Metres above sea level

No. of aliquotsa

Total dose rate (Gy kyr–1)b

DE ± 2σ s.e. (Gy)c

D0 ± 1σ (Gy)d

OSL age ± 1σ s.e. (ka)

Dune package 1

RB7e

USU-2256

5

14 (32)

0.21 ± 0.01

158.8 ± 19.5

111.8 ± 51.9

750 ± 80

RB12e

USU-2261

6

15 (28)

0.26 ± 0.01

230.8 ± 29.1

115.9 ± 29.0

880 ± 90

RB5e

USU-2013

10

17 (33)

0.17 ± 0.01

220.6 ± 31.3

112.3 ± 25.6

1,260 ± 140

RB10e

USU-2259

58

18 (34)

0.25 ± 0.01

277.1 ± 47.7

(125.1 ± 40.7)

1,130 ± 140

Dune package 2

RB1

USU-2004

5

17 (25)

0.43 ± 0.02

215.0 ± 31.5

111.9 ± 61.8

500 ± 50

RB2

USU-2005

8

20 (31)

0.40 ± 0.02

224.8 ± 31.0

112.4 ± 56.9

570 ± 70

RB9

USU-2258

8

18 (25)

0.21 ± 0.01

150.2 ± 22.2

90.6 ± 38.9

710 ± 80

RB6 f

USU-2014

16

18 (31)

0.24 ± 0.01

205.2 ± 31.3

122.7 ± 53.7

860 ± 100

RB8

USU-2257

22

20 (27)

0.23 ± 0.01

155.3 ± 18.4

92.5 ± 31.2

680 ± 70

RB11

USU-2260

60

17 (28)

0.26 ± 0.01

173.6 ± 22.2

121.7 ± 56.5

670 ± 70

RB13

USU-2262

65

18 (24)

0.28 ± 0.01

202.5 ± 28.3

103.0 ± 31.6

720 ± 80

Dune package 3

RB14

USU-2264

68

17 (29)

0.61 ± 0.03

283.6 ± 42.7

106.3 ± 48.2

470 ± 50

RB16

USU-2015

72

25 (37)

0.30 ± 0.01

160.2 ± 11.2

117.0 ± 60.2

530 ± 50

RB15

USU-2009

74

17 (24)

0.11 ± 0.01

48.6 ± 4.7

76.5 ± 25.6

430 ± 50

Dune package 4

RB19

USU-2008

75

19 (25)

0.26 ± 0.01

42.1 ± 4.4

58.7 ± 19.6

160 ± 20

RB18

USU-2007

80

20 (22)

0.34 ± 0.01

52.3 ± 4.6

67.0 ± 19.1

150 ± 10

RB17

USU-2263

82

16 (21)

0.86 ± 0.04

90.7 ± 8.6

86.5 ± 25.8

100 ± 10

Dune package 5

RB20f

USU-2017

85

20 (24)

0.17 ± 0.01

10.3 ± 1.4

62.2 ± 38.1

61 ± 8

RB21f

USU-2016

87

21 (28)

0.20 ± 0.01

10.7 ± 1.7

67.0 ± 37.3

53 ± 7

Fraser Island cliffs

SRG4

USU-2391

14

15 (34)

0.32 ± 0.01

243.3 ± 34.6

155.5 ± 93.3

780 ± 80

SRG3

USU-2392

17

23 (33)

0.19 ± 0.01

144.5 ± 16.1

102.7 ± 36.9

770 ± 80

SRG2

USU-2393

18

17 (37)

0.23 ± 0.01

180.9 ± 25.8

95.8 ± 20.0

790 ± 90

SRG1

USU-2394

23

19 (37)

0.29 ± 0.01

184.8 ± 11.7

92.3 ± 19.0

650 ± 60

  1. For sample location and stratigraphical information, see Extended Data Figs. 1–5. Dose–response and signal–decay luminescence curves are provided in Extended Data Fig 6. Radial plots displaying DE values and distributions for all samples are provided in Extended Data Fig. 7.
  2. aAge analysis using the single-aliquot regenerative-dose procedure of Murray and Wintle25 on 1 mm small aliquots of 180–250 μm quartz sand. Number of aliquots used in age calculation and number of aliquots analysed in parentheses.
  3. bSee Table 2 for contributing radio-elemental data for external dose rate and Extended Data Table 1 for internal dose rate. Internal dose rate is assumed to be 0.018 ± 0.001 for all samples that are not presented in Extended Data Table 1. Total dose rate is derived from concentrations by conversion factors from Guérin et al.52 and beta-attenuation factors of Brennan53 and includes cosmic dose (Prescott and Hutton54) and attenuation from water.
  4. cEquivalent dose (DE) calculated using the Central Age Model of Galbraith and Roberts55. Uncertainty reported at two sigma standard error (s.e.).
  5. dMean characteristic dose of saturation (D0) and 1 s.d. range calculated from the dose–response curves of all accepted aliquots. DE values greater than 2 × D0 may be underestimated due to interpolation onto a saturating exponential. Parentheses around the D0 value indicate it is >2DE. Only sample USU-2259 fit this category, but the 2D0 and DE values are within error, suggesting the DE and age from this sample might be underestimated slightly.
  6. eSamples are stratigraphically near reversed palaeomagnetic samples (Extended Data Table 2).
  7. fThese samples were collected above the cliff from exposed units in the Carlo Blowout. Originally published in ref. 22