Table 1 Summary of data from individual foraminifera analysis.

From: Modulation of late Pleistocene ENSO strength by the tropical Pacific thermocline

Interval Name

Core

Depth (cm)

Age (ky)

Mean T (°C)

MAD

Q94-98T

N

ENSO change

Mid-Holocene

14MC

4.5

3.4

28.18

1.00

0.56

150

+

MIS 2

17PC

60

25

26.5

0.96

1.04

65

+

MIS 3

17PC

72

29.6

26.38

1.08

0.61

82

+

MIS 5d

17PC

286

111.8

27.1

0.75

0.30

63

0

MIS 5e

17PC

322

126.9

28.12

1.14

0.74

77

+

MIS 6.1

17PC

378

152.2

26.7

1.21

0.57

79

+

MIS 6.2

17PC

400

162.2

27.18

1.08

0.41

79

0

MIS 6.3

17PC

442

181.3

27.05

1.00

−0.02

80

0

MIS 7a

17PC

475

197.1

28.04

0.83

−0.17

82

−*

MIS 7d

17PC

530

229.7

27.61

0.93

0.43

82

0

MIS 7e

17PC

552

239.9

28.5

0.74

−0.54

78

MIS 8.1

17PC

595

268.2

27.97

0.97

0.09

81

+

MIS 8.2

17PC

614

282.4

26.89

0.96

0.47

78

0

  1. Columns are sample interval reference names and Marine Isotope Stage (MIS) names, core ID, sample depth (cm), sample age (ky), mean individual foraminifera temperature (°C), median absolute deviation (MAD), mean of the 94th–98th quantile normalized temperature (Q94-98T), number of foraminifera analyzed (N), and change in El Niño amplitude. For glacial periods MIS 6 and MIS 8, decimal notation refers to the indexed number of sampled intervals from that stage. El Niño amplitude change was determined by Q–Q analysis. Plus-signs indicate increased El Niño amplitude, minus signs reduced El Niño amplitude. The asterisk denotes an interval that displays significantly reduced El Niño amplitude at the 90% confidence level but may be a false positive result.