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Swiss Journal of Geosciences

Table 3 Equivalent doses (De), dose rates (Dr), and ages for all samples

From: Multiple Quaternary erosion and infill cycles in overdeepened basins of the northern Alpine foreland

Core

Depth (m)

Sample

Fraction (µm)

We (%)

Polymineral fraction (K-Feldspar for coarse-grained samples)

Quartz fraction

Comments

Dr (Gy/ka)

±

nacc/ntot

De IRSL50 (Gy)

±

Age (ka)

±

Dr (Gy/ka)

±

nacc/ntot

De (Gy)

±

Age (ka)

±

Lower Glatt valley

B1/12

44.00

B1-44

11–25

20 ± 5

2.19

0.17

5/5

419

40

191

23

2.07

0.21

5/5

359

15

173

19

Lens of fines (LFA3) in LFA8

58.00

B1-58

4–11

25 ± 5

1.74

0.14

5/5

330

23

190

20

1.65

0.19

5/5

238

7

144

17

 

60.40

B1-60

4–11

25 ± 5

2.26

0.18

3/3

550

21

243**

21

2.16

0.24

4/5

360

9

167

19

 

65.30

B1-65

4–11

25 ± 5

2.17

0.16

3/3

525

3

242**

18

1.98

0.22

5/5

383

12

193*

22

 

72.25

B1-72

4–11

25 ± 5

1.32

0.11

5/5

(188

10

143

14)

1.24

0.15

4/5

157

10

126

17

IRSL not considered

79.50

B1-79

4–11

25 ± 5

2.27

0.17

3/3

612

52

269**

31

2.17

0.24

5/5

467

15

215**

25

 

87.70

B1-87

4–11

25 ± 5

2.26

0.17

3/3

631

24

280**

23

2.16

0.24

5/5

433

9

201**

22

 

99.00

B1-99

4–11

25 ± 5

2.05

0.16

3/5

830

46

405**

38

1.95

0.22

5/5

461

28

236**

30

 

130.00

B1-130

4–11

25 ± 5

1.57

0.13

9/10

545

13

348**

30

1.48

0.18

–

    

No Q left after etching

164.00

B1-164

4–11

25 ± 5

1.55

0.13

9/10

488

6

315**

27

1.46

0.19

10/10

342

11

234*

31

 

171.80

B1-2

200–250

20 ± 5

1.80

0.13

10/12

582

26

324

27

0.96

0.05

20/24

191

20

199*

23

KFS: nsat = 1, OD = 12;Q: nsat = 1, OD = 45;

B2/12

51.30

B2-51

4–11

25 ± 5

2.19

0.18

5/5

96

2

44

4

2.09

0.24

4/4

85

1

41

5

 

54.50

B2-54

4–11

25 ± 5

2.13

0.17

5/5

393

6

184

15

2.04

0.23

4/4

267

6

131

15

 

67.40

B2-67

4–11

25 ± 5

2.09

0.16

5/5

445

2

213*

16

2.00

0.22

3/4

340

15

170

20

 

79.70

B2-79

4–11

25 ± 5

2.42

0.18

9/9

(137

2

56

4)

2.32

0.25

4/4

(221

6

96

10)

Not considered

100.00

B2-100

4–11

25 ± 5

2.07

0.16

5/5

586

17

284**

24

1.97

0.22

4/4

461

32

234**

31

 

B3/12

40.00

B3-40

4–11

25 ± 5

1.89

0.15

5/5

154

3

82

7

1.80

0.20

7/8

127

7

71

9

 

47.10

B3-47B

4–11

25 ± 5

2.36

0.19

3/3

480

19

203**

18

2.25

0.26

4/4

273

19

121

17

 

47.80

B3-47

4–11

25 ± 5

1.74

0.13

5/5

307

8

176

14

1.66

0.19

4/5

208

5

126

14

 

48.50

B3-48

4–11

25 ± 5

1.76

0.14

3/3

241

3

137

11

1.67

0.19

4/4

170

8

102

12

 

51.00

B3-51

4–11

25 ± 5

2.46

0.18

5/5

(212

3

86

6)

2.35

0.25

4/4

(134

4

57

6)

Not considered

64.00

B3-64

4–11

25 ± 5

2.30

0.17

5/5

535

10

233**

18

2.20

0.24

7/8

406

5

185**

20

 

85.00

B3-85

4–11

25 ± 5

2.25

0.16

5/5

628

22

279**

23

2.15

0.23

4/4

412

20

191**

22

 

101.00

B3-101

4–11

25 ± 5

2.14

0.29

4/4

574

6

268**

36

2.04

0.34

4/4

432

10

212**

35

 

B4/12

57.80

Ho-B2-2

4–11

25 ± 5

1.85

0.16

5/5

550

19

297**

28

1.76

0.22

12/12

375

6

213*

26

 

B5/12

26.00

Ho-B1-9

4–11

25 ± 5

2.45

0.19

4/5

468

10

191**

16

2.35

0.26

8/8

347

12

147

17

 

29.00

Ho-B1-29

4–11

25 ± 5

2.57

0.21

4/4

551

9

215**

18

2.46

0.28

5/5

375

10

152

17

 

37.50

Ho-B1-37

4–11

25 ± 5

2.52

0.18

7/7

522

21

207**

17

2.42

0.25

10/10

370

7

153

16

 

55.95

Ho-B1-8

4–11

25 ± 5

1.84

0.15

8/8

512

12

278**

23

1.75

0.20

8/8

354

6

202*

24

 

66.50

Ho-B1-7

4–11

25 ± 5

2.14

0.16

7/7

540

6

253**

19

2.04

0.22

8/8

417

9

204**

23

 

80.00

Ho-B1-6

4–11

25 ± 5

1.94

0.15

5/5

539

5

277**

21

1.85

0.21

8/8

392

8

212*

24

 

93.22

Ho-B1-5

4–11

25 ± 5

1.77

0.14

7/7

509

18

288**

25

1.68

0.19

7/7

380

12

226*

27

 

113.35

Ho-B1-3

4–11

25 ± 5

2.01

0.16

5/5

508

8

253**

20

1.91

0.21

7/8

393

6

206*

23

 

122.80

Ho-B1-2

4–11

25 ± 5

1.83

0.14

8/8

505

9

276**

22

1.73

0.19

12/12

370

8

214*

25

 

132.80

Ho-B1-1

200–250

20 ± 5

2.20

0.14

39/40

515

25

234

19

1.36

0.07

12/26

290

22

213*

20

KFS: nsat = 0, OD = 30; Q: nsat = 7, OD = 24

145.90

Ho-B1-10

200–250

20 ± 5

2.17

0.14

16/16

530

40

244

24

1.33

0.07

9/10

205

20

154*

17

KFS: nsat = 0, OD = 30; Q: nsat = 1, OD = 26

Hardwald, middle Glatt valley

KB08-4

52.35

HDB4

4–11

25 ± 5

2.38

0.17

5/5

597

34

251**

14

2.28

0.24

5/5

396

28

174**

12

 

KB08-5

54.50

HDB1

4–11

25 ± 5

2.50

0.18

5/5

677

22

271**

9

2.39

0.25

5/5

394

57

165**

24

 

53.75

HDB2

4–11

25 ± 5

2.65

0.20

5/5

568

69

214**

26

2.48

0.25

5/5

430

20

173**

8

 

KB08-7

48.72

HDB3

4–11

25 ± 5

2.30

0.17

5/5

649

29

282**

13

2.20

0.23

5/5

412

21

187**

10

 
  1. Bold: reliable ages, type 1, *Age overestimation, type 2, **Saturation limit within error, type 3 (IRSL50 at 470 Gy, quartz OSL at 400 Gy according to Buechi et al. 2017b)
  2. Values in brakets are outliers, not considered, see text. Italic: coarse-grained samples (see text)
  3. W e estimated paleo-water content, n tot total number of aliquots measured, n acc number of accepted aliquots, n sat number of saturated aliquots, OD overdispersion
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