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Table 4 Soil properties of the Collins’ Outcrop temporal gradient

From: Successional patterns along soil development gradients formed by glacier retreat in the Maritime Antarctic, King George Island

Plot/Est. age [BP]

Horizon

Horizon Depth [cm]

Texture

Skeleton [%]

Color (moist)

pH

C org [%]

C/N

δ13C [‰]

Classification

C1/< 200

CA

0–1

LS

-

10 YR 2/3

6.42

0.47

9.8

−22.60

Skeletic

C1

1–8

LS

65

10 YR 3/3

6.42

0.28

10.1

−23.34

EutricRegosol

C2

> 8

LS

48

10 YR 3/3

7.13

0.20

11.1

−22.13

(Ochric)

C2/2000

A

0–1

SL

-

10 YR 2/2

4.58

8.90

11.6

−23.19

Skeletic

AC1

1–6

SL

14

10 YR 2/3

4.70

2.09

9.5

−22.39

Dystric

AC2

6–12

LS

36

10 YR 2/3

5.07

1.94

9.7

−22.32

Regosol

C3/3500

A

0–6

SL

18

10 YR 2/2

4.76

13.8

10.7

−23.38

DystricLepto-

R

> 6

       

sol (Stagnic)

C4/7200

O

0–3

 

2.3

 

5.58

20.7

10.3

−25.59

Eutric

A

3–11

SL

50

10 YR 2/3

5.29

3.84

9.3

−22.18

Regosol

AB

11–16

SiL

30

10 YR 3/1

5.62

4.31

9.5

−22.36

(Ornithic)