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Table 1 Age results of Site U1463

From: The pteropod species Heliconoides inflatus as an archive of late Pleistocene to Holocene environmental conditions on the Northwest Shelf of Australia

Laboratory Code

Sample Name

Depth CSF-A [m]

Depth CCSF-A [m]

Radiocarbon age [year BP]

Calendar age [cal year BP] 95% highest density regions

YAUT-034202

356-U1463B-1H-1A 0/4

0.02

0.02

1216 ± 37

501

730

YAUT-034203

356-U1463B-1H-1A 68/72

0.7

0.7

1775 ± 34

1029

1297

YAUT-034204

356-U1463B-1H-2A 18/22

1.7

1.7

2887 ± 31

2326

2662

YAUT-034205

356-U1463B-1H-2A 118/122

2.7

2.7

3632 ± 29

3215

3514

YAUT-034206

356-U1463B-1H-3A 68/72

3.7

3.7

4789 ± 29

4689

5034

YAUT-051514

356-U1463C-2H-3A 17/21

7.31

8.31

6552 ± 53

6635

7026

YAUT-055628

356-U1463C-2H-3A 55/59

7.69

8.69

7136 ± 28

7306

7563

YAUT-056104

356-U1463C-2H-3A 130/134

8.44

9.44

9143 ± 36

9522

9883

YAUT-056105

356-U1463C-2H-5A 17/21

10.31

11.31

10,626 ± 47

11,506

11,997

YAUT-051515

356-U1463C-2H-5A 130/134

11.44

12.44

13,914 ± 85

15,667

16,269

  1. Calibration of calendar years was based on a Bayesian age modeling approach (Ramsey, 2009) using the Marine20 database (Heaton et al., 2020). Depth of individual samples is given as core depth below sea floor (CSF-A) and core composite depth below sea floor (CCSF-A), as defined by the IODP Depth Scale Terminology (IODP-MI 2011). Calendar ages are represented by the lower and upper boundary of the highest density region