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Singh, Dharmendra Pratap (2026): Basin-scale Arabian Sea denitrification reconstruction based on δ¹⁵N records, Southern Arabian Sea Stack [dataset]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.993906 (DOI registration in progress), In: Singh, DP (2026): Basin-scale Arabian Sea denitrification reconstruction based on δ¹⁵N records including core SSD004 GC11 [dataset bundled publication]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.993898 (DOI registration in progress)

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Published: 2026-04-29

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Abstract:
The new δ¹⁵N record of sediment core SSD004_GC11 is combined with published regional datasets to produce a basin-wide Arabian Sea denitrification stack. Spectral and cross-wavelet analyses reveal dominant orbital-scale variability, with stronger obliquity influence in the southern basin and precession dominance in northern records. Coherent variability between δ¹⁵N records and atmospheric N₂O concentrations highlights orbital forcing as a key driver of long-term nitrogen cycling and greenhouse gas variability.
Keyword(s):
Arabian Sea; d15N; Sedimentary geochemistry; Stack; TN
Related to:
Pawar, Rahul; Singh, Dharmendra Pratap; Saraswat, Rajeev; Maurya, A S (2026): Orbital forcing regulated Arabian Sea denitrification during the late Pleistocene. Global and Planetary Change, 259, 105373, https://doi.org/10.1016/j.gloplacha.2026.105373
References:
Isaji, Yuta; Kawahata, Hodaka; Ohkouchi, Naohiko; Ogawa, Nanako O; Murayama, Masafumi; Inoue, Kazuki; Tamaki, Kensaku (2015): Varying responses to I ndian monsoons during the past 220 kyr recorded in deep‐sea sediments in inner and outer regions of the G ulf of A den. Journal of Geophysical Research: Oceans, 120(11), 7253-7270, https://doi.org/10.1002/2015JC010982
Ivanochko, Tara S; Ganeshram, Raja S; Brummer, Geert-Jan A; Ganssen, Gerald M; Jung, S J A; Moreton, Stephen; Kroon, Dick (2005): Variations in tropical convection as an amplifier of global climate change at the millennial scale. Earth and Planetary Science Letters, 235(1-2), 302-314, https://doi.org/10.1016/j.epsl.2005.04.002
Suthhof, Andreas; Ittekkot, Venugopalan; Gaye-Haake, Birgit (2001): Millennial‐scale oscillation of denitrification intensity in the Arabian Sea during the Late Quaternary and its potential influence on atmospheric N 2 O and global climate. Global Biogeochemical Cycles, 15(3), 637-649, https://doi.org/10.1029/2000GB001337
Tesdal, J-E; Galbraith, Eric Douglas; Kienast, Markus (2013): NOAA/WDS Paleoclimatology - NICOPP Global Ocean Sediment Nitrogen Isotope Database [dataset]. NOAA National Centers for Environmental Information, https://doi.org/10.25921/W9CA-1Z10
Tiwari, Manish; Ramesh, R; Bhushan, Ravi; Sheshshayee, Madavalm S; Somayajulu, Bammidipati L K; Jull, A J Timothy; Burr, George S (2010): Did the Indo‐Asian summer monsoon decrease during the Holocene following insolation? Journal of Quaternary Science, 25(7), 1179-1188, https://doi.org/10.1002/jqs.1398
Funding:
Science and Engineering Research Board (SERB), grant/award no. SRG/2021/000620
Coverage:
Median Latitude: 12.070917 * Median Longitude: 57.029083 * South-bound Latitude: 6.000000 * West-bound Longitude: 46.932300 * North-bound Latitude: 14.983000 * East-bound Longitude: 78.931200
Date/Time Start: 1986-05-24T00:00:00 * Date/Time End: 1986-05-24T00:00:00
Minimum Elevation: -3212.0 m * Maximum Elevation: -1474.0 m
Event(s):
GOA4 * Latitude: 12.821500 * Longitude: 46.932300 * Elevation: -1474.0 m * Method/Device: Sediment corer (SEDCO)
GOA6 * Latitude: 14.983000 * Longitude: 53.767000 * Elevation: -2416.0 m * Method/Device: Sediment corer (SEDCO)
NIOP_905 * Latitude: 10.920000 * Longitude: 51.940000 * Location: Arabian Sea
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
AGEAgeka BPSingh, Dharmendra PratapGeocode
δ15N, bulk sedimentδ15N bulk‰ airSingh, Dharmendra PratapStackedSouthern Arabian Sea Stack
δ15N, standard deviationδ15N std dev±Singh, Dharmendra Pratapcalculated, 1 sigma
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
349 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Age [ka BP]

δ15N bulk [‰ air]

δ15N std dev [±]
0.10.93
1.10.460.60
2.10.290.56
3.10.560.17
4.10.490.63
5.10.620.37
6.10.490.53
7.10.700.35
8.10.710.42
9.10.840.51
10.11.120.66
11.11.060.90
12.10.760.74
13.10.460.84
14.10.540.63
15.1-0.070.86
16.1-0.030.77
17.1-0.440.24
18.1-0.690.29
19.1-0.510.27
20.1-0.290.40
21.1-0.370.45
22.1-0.440.30
23.1-0.470.25
24.1-0.680.56
25.1-0.570.12
26.1-0.340.24
27.1-0.380.38
28.1-0.420.16
29.1-0.420.40
30.1-0.620.75
31.1-0.430.44
32.10.160.37
33.1-0.120.28
34.1-0.340.52
35.10.110.30
36.1-0.060.26
37.10.280.29
38.10.330.49
39.1-0.380.51
40.1-0.250.26
41.10.240.55
42.10.400.60
43.10.020.27
44.10.370.48
45.10.650.78
46.10.420.54
47.10.420.52
48.10.650.43
49.10.640.19
50.10.760.37
51.10.820.27
52.10.560.35
53.10.550.31
54.10.500.33
55.10.500.65
56.10.680.60
57.1-0.140.69
58.1-0.560.94
59.1-0.450.56
60.1-0.790.68
61.1-0.990.73
62.1-1.110.77
63.1-1.040.62
64.1-1.090.63
65.1-1.210.66
66.1-0.900.33
67.1-0.550.69
68.1-0.480.78
69.1-1.030.41
70.1-0.361.14
71.1-0.351.20
72.1-0.380.84
73.1-0.460.28
74.1-0.190.17
75.1-0.030.31
76.10.260.24
77.10.330.54
78.10.320.49
79.10.340.58
80.10.550.47
81.10.520.36
82.10.370.15
83.10.380.23
84.1-0.130.48
85.1-0.230.62
86.1-0.250.77
87.1-0.110.68
88.10.150.74
89.10.240.76
90.10.340.75
91.10.420.77
92.10.490.57
93.10.550.49
94.10.420.65
95.10.560.51
96.10.500.60
97.10.200.56
98.10.250.57
99.1-0.210.70
100.1-0.410.79
101.1-0.510.79
102.1-0.570.72
103.1-0.580.62
104.1-0.550.51
105.1-0.490.49
106.1-0.390.43
107.1-0.290.39
108.1-0.380.59
109.1-0.230.46
110.1-0.240.57
111.10.050.27
112.10.110.36
113.10.240.35
114.10.440.21
115.10.270.46
116.10.300.38
117.10.410.18
118.10.280.39
119.10.460.14
120.10.440.12
121.10.360.06
122.10.280.07
123.10.140.19
124.10.030.28
125.10.120.30
126.1-0.020.39
127.1-0.070.52
128.1-0.080.68
129.10.140.75
130.10.210.64
131.10.260.53
132.10.200.43
133.10.210.68
134.10.330.29
135.10.140.31
136.10.120.54
137.10.120.77
138.10.000.90
139.10.060.74
140.10.060.64
141.10.090.60
142.10.190.61
143.10.110.58
144.10.250.95
145.1-0.020.85
146.1-0.350.69
147.1-0.430.99
148.1-0.750.86
149.1-0.810.77
150.1-0.780.83
151.1-0.511.18
152.1-0.900.54
153.1-0.920.55
154.1-0.720.85
155.1-0.780.77
156.1-0.540.83
157.1-0.390.75
158.1-0.370.66
159.1-0.150.87
160.1-0.030.96
161.1-0.040.90
162.10.050.95
163.1-0.140.73
164.10.371.08
165.10.330.90
166.10.571.04
167.10.370.78
168.10.240.90
169.10.230.72
170.10.210.55
171.10.190.37
172.10.190.21
173.10.190.06
174.10.180.06