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Table 1 Concentrations, δ13C values, and typical indices based on n-alkanes in the subsamples with different sediment depth of core R23. The relative contribution of long chain n-alkanes from C3 and C4 plants are calculated by carbon isotopes of the C31 n-alkane

From: A potential suite of climate markers of long-chain n-alkanes and alkenones preserved in the top sediments from the Pacific sector of the Southern Ocean

Depth

(cm)

δ13C23

(‰)

δ13C24

(‰)

δ13C25

(‰)

δ13C26

(‰)

δ13C27

(‰)

δ13C28

(‰)

δ13C29

(‰)

δ13C31

(‰)

n-alkanesa

(ng/g)

C4

(%)

C3

(%)

ACLb

CPIc

16

−29.6

−28.8

−29.9

−33.2

−28.5

−32.2

−27.4

−28.3

445

55

45

30.1

1.6

88

−29.5

−31.8

−27.3

−30.0

−26.3

−33.1

−25.1

−25.5

328

75

25

30.3

2.0

166

−25.4

−26.4

−26.7

−32.5

−28.3

−38.0

−27.1

−27.8

295

59

41

30.1

2.1

243

−27.1

−26.8

−26.8

−30.4

−26.7

−33.3

−29.8

−28.3

362

55

45

30.3

2.5

323

−29.8

−31.2

−30.6

−35.0

−28.3

−32.1

−29.4

−27.9

324

58

42

29.3

1.3

398

−31.5

−35.9

−30.0

−36.7

−28.6

−34.6

−25.0

−24.8

787

80

20

29.6

1.3

482

−26.8

−28.4

−29.3

−30.3

−26.8

−30.1

−27.4

−26.6

411

67

33

30.7

1.9

550

−27.1

−30.7

−29.3

−35.1

−27.8

−31.2

−27.8

−25.4

420

76

24

30.1

1.6

626

−30.4

−32.2

−31.7

−34.6

−29.6

−30.9

−26.4

−25.8

344

73

27

29.6

1.6

698

−28.6

−30.6

−29.0

−32.7

−27.8

−31.8

−27.0

−25.8

490

73

27

29.3

1.1

762

−28.8

−29.3

−30.0

−35.3

−26.7

−32.1

−30.4

−29.4

455

47

53

29.8

1.6

818

−28.8

−28.7

−32.3

−37.4

−30.1

−35.8

−27.7

−27.2

503

63

37

30.1

1.7

  1. aTotal concentrations of C23-C35 n-alkanes
  2. bACL27-35 =∑(i × Xi)/∑Xi, where X is abundance and i ranges from C27 to C35 odd n-alkanes
  3. cCPI27-33 = 0.5 × ∑(C27–C33)/(C26–C32) + 0.5 × ∑(C27–C33)/(C28–C34)