/* DATA DESCRIPTION:
Citation:	Novak, Joseph B; Abell, Jordan; Kinsley, Christopher (2026): Timeseries of binned benthic stable carbon isotope from ODP Site 162-982,130-807 and ODP Site 162-982 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.993222, 
	In: Novak, JB et al. (2026): 4.5 million years of deep ocean carbon isotope gradients and trace metals redox data [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.983612
Abstract:	This dataset contains C. wuellerstorfi stable carbon isotope values binned by marine isotope stage from ODP Site 162-807 and ODP Site 162-982 that span the last 4.5 million years (Feng et al. 2022; Venz et al. 1999, 2002; Hodell & Venz-Curtis 2006). This isotope gradient reflects the accumulation of respired and disequilibrium carbon in the deep Pacific ocean relative to the North Atlantic. Also included are binned probstack δ18O (Ahn et al., 2017) and ΔGMST (Clark et al., 2024) values for comparison to the binned stable carbon isotope values.
Keyword(s):	Carbon cycle; carbon isotope gradients; trace metals
Original version:	Novak, Joseph B; Abell, Jordan; Kinsley, Christopher (2026): Timeseries of binned benthic stable carbon isotope from ODP Site 162-982,130-807 and IODP Site 306-U1313 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.983608
References:	Ahn, Seonmin; Khider, D; Lisiecki, Lorraine E; Lawrence, Charles E (2017): A probabilistic Pliocene–Pleistocene stack of benthic δ18O using a profile hidden Markov model. Dynamics and Statistics of the Climate System, 2(1), https://doi.org/10.1093/climsys/dzx002
	Clark, Peter U; Shakun, Jeremy D; Rosenthal, Yair; Pollard, David; Hostetler, Steven W; Köhler, Peter; Bartlein, Patrick J; Gregory, Jonathan M; Zhu, Chenyu; Schrag, Daniel P; Liu, Zhengyu; Pisias, Nicklas G (2025): Global mean sea level over the past 4.5 million years. Science, 390(6770), eadv8389, https://doi.org/10.1126/science.adv8389
	Feng, Hua; Tian, Jun; Lyle, Mitchell W; Westerhold, Thomas; Wilkens, Roy H (2022): High resolution benthic foraminiferal δ18O and δ13C records at ODP site 807 over the past 5 Ma, Ontong Java Plateau: Evolution of North Pacific ventilation, Pliocene to Holocene. Global and Planetary Change, 217, 103945, https://doi.org/10.1016/j.gloplacha.2022.103945
	Hodell, David A; Venz-Curtis, Kathryn A (2006): Late Neogene history of deepwater ventilation in the Southern Ocean. Geochemistry, Geophysics, Geosystems, 7(9), Q09001, https://doi.org/10.1029/2005GC001211
	Lisiecki, Lorraine E; Raymo, Maureen E (2005): A Pliocene-Pleistocene stack of 57 globally distributed benthic d18O records. Paleoceanography, 20, PA1003, https://doi.org/10.1029/2004PA001071
	Venz, Kathryn A; Hodell, David A (2002): New evidence for changes in Plio-Pleistocene deep water circulation from Southern Ocean ODP Leg 177 Site 1090. Palaeogeography, Palaeoclimatology, Palaeoecology, 182(3-4), 197-220, https://doi.org/10.1016/S0031-0182(01)00496-5
	Venz, Kathryn A; Hodell, David A; Stanton, Cathy; Warnke, Detlef A (1999): A 1.0 myr record of glacial North Atlantic Intermediate Water variability from ODP Site 982 in the northeast Atlantic. Paleoceanography, 14(1), 42-52, https://doi.org/10.1029/1998PA900013
Coverage:	MEDIAN LATITUDE: 30.559667 * MEDIAN LONGITUDE: 70.385408 * SOUTH-BOUND LATITUDE: 3.606667 * WEST-BOUND LONGITUDE: -15.854183 * NORTH-BOUND LATITUDE: 57.512667 * EAST-BOUND LONGITUDE: 156.625000
	DATE/TIME START: 1990-02-26T00:00:00 * DATE/TIME END: 1995-07-19T00:00:00
	MINIMUM ELEVATION: -2805.2 m * MAXIMUM ELEVATION: -1134.2 m
Event(s):	130-807 * LATITUDE: 3.606667 * LONGITUDE: 156.625000 * DATE/TIME START: 1990-02-26T00:00:00 * DATE/TIME END: 1990-03-02T00:00:00 * ELEVATION: -2805.2 m * Penetration: 2629.9 m * Recovery: 1249.8 m * LOCATION: North Pacific Ocean * CAMPAIGN: Leg130 (URI: https://doi.org/10.2973/odp.proc.ir.130.1991) * BASIS: Joides Resolution (URI: https://www-odp.tamu.edu:443/resolutn.html) * METHOD/DEVICE: Composite Core (COMPCORE) * COMMENT: 209 cores; 1849.9 m cored; 0 m drilled; 67.6% recovery
	162-982 * LATITUDE: 57.512667 * LONGITUDE: -15.854183 * DATE/TIME START: 1995-07-15T00:00:00 * DATE/TIME END: 1995-07-19T00:00:00 * ELEVATION: -1134.2 m * Penetration: 1143.9 m * Recovery: 1008 m * LOCATION: North Atlantic Ocean * CAMPAIGN: Leg162 (URI: https://doi.org/10.2973/odp.proc.ir.162.1996) * BASIS: Joides Resolution (URI: https://www-odp.tamu.edu:443/resolutn.html) * METHOD/DEVICE: Composite Core (COMPCORE) * COMMENT: 120 cores; 1123.9 m cored; 0 m drilled; 89.7% recovery
Comment:	Methods:
	Cibicidoides δ13C data from each site were binned by marine isotope stage (MIS) as defined by Lisiecki & Raymo (2005) before calculating their difference to minimize data artefacts due to minor differences in age model assignment. 
	For comparison to the derived Δδ13C982-807 (‰) values, we also calcualted binned probstack benthic δ18O (Ahn et al., 2017) and ΔGMST (Clark et al., 2024).
	The code that automates data binning by marine isotope stage is available in the supplementary materials of the manuscript.
Parameter(s):	Marine isotope stage (MIS) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: See description in dataset comment
	Age, dated, range, minimum [ka] (Age dated min) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: Age model according to Lisiecki & Raymo (2005) [LR04] (URI: https://doi.org/10.1029/2004PA001071) * COMMENT: Start of marine isotope stage
	Age, dated [ka] (Age dated) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: Age model according to Lisiecki & Raymo (2005) [LR04] (URI: https://doi.org/10.1029/2004PA001071) * COMMENT: Midpoint of marine isotope stage. This is included in the spreadsheet for ease of making plots.
	Age, dated, range, maximum [ka] (Age dated max) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: Age model according to Lisiecki & Raymo (2005) [LR04] (URI: https://doi.org/10.1029/2004PA001071) * COMMENT: End of marine isotope stage
	δ13C [‰] (δ13C) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: Age model according to Lisiecki & Raymo (2005) [LR04] (URI: https://doi.org/10.1029/2004PA001071) * COMMENT: Binned ODP Site 162-982, mean
	δ13C [‰] (δ13C) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: Age model according to Lisiecki & Raymo (2005) [LR04] (URI: https://doi.org/10.1029/2004PA001071) * COMMENT: Binned ODP Site 130-807, mean
	Δ13C [‰] (Δ13C) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: Age model according to Lisiecki & Raymo (2005) [LR04] (URI: https://doi.org/10.1029/2004PA001071) * COMMENT: Difference between mean binned ODP 162-982 and ODP 130-807 benthic stable carbon isotope data in per mille
	δ18O [‰] (δ18O) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: Age model according to Ahn et al. (2017) [Probstack] (URI: https://doi.org/10.1093/climsys/dzx002) * COMMENT: Binned probstack benthic stable oxygen isotope data, mean
	Sea surface temperature, anomaly [°C] (SST anomaly) * PI: Novak, Joseph B (https://orcid.org/0000-0002-8569-2645, jobnovak@ucsc.edu) * METHOD/DEVICE: Calculated according to Clark et al. (2024) (URI: https://doi.org/10.5194/cp-20-2081-2024) * COMMENT: Binned global mean surface temperature, mean
Change history:	2026-03-26T07:36:01 - Version 2: Previous version doi:10.1594/PANGAEA.983608 contains errors.
License:	Creative Commons Attribution 4.0 International (CC-BY-4.0) (URI: https://creativecommons.org/licenses/by/4.0/)
Status:	Curation Level: Basic curation (URI: https://wiki.pangaea.de/wiki/Curation_levels)
Size:	1755 data points
*/
MIS (See description in dataset co...)	Age dated min [ka] (Start of marine isotope stage...)	Age dated [ka] (Midpoint of marine isotope st...)	Age dated max [ka] (End of marine isotope stage, ...)	δ13C [‰] (Binned ODP Site 162-982, mean...)	δ13C [‰] (Binned ODP Site 130-807, mean...)	Δ13C [‰] (Difference between mean binne...)	δ18O [‰] (Binned probstack benthic stab...)	SST anomaly [°C] (Binned global mean surface te...)
1	0.0	7.00	14.0	0.93	0.07	0.86	3.49	-0.54
1/2	14.0	21.50	29.0	1.31	-0.05	1.37	4.70	-5.32
2/3	29.0	43.00	57.0	1.23	0.04	1.19	4.52	-5.20
3/4	57.0	64.00	71.0	1.27	-0.17	1.45	4.42	-5.08
4/5	71.0	76.50	82.0	1.27	0.10	1.17	4.23	-2.85
5.1(peak)	82.0	84.50	87.0	1.08	0.19	0.89	3.96	-2.05
5.2(peak)	87.0	91.50	96.0	0.84	0.13	0.71	4.08	-1.88
5.3(peak)	96.0	102.50	109.0	0.94	0.11	0.83	3.89	-1.06
5.4(peak)	109.0	116.00	123.0	0.39	0.06	0.33	3.68	-0.59
5.5(peak)	123.0	126.50	130.0	0.45	0.07	0.39	3.42	0.69
5.5/6	130.0	160.50	191.0	0.90	-0.28	1.18	4.53	-3.98
6/7	191.0	217.00	243.0	0.86	-0.16	1.03	3.85	-1.95
7/8	243.0	271.50	300.0	0.97	-0.20	1.17	4.30	-3.95
8/9	300.0	318.50	337.0	0.74	-0.05	0.80	3.70	-1.58
9/10	337.0	355.50	374.0	1.08	-0.33	1.41	4.47	-4.87
10/11	374.0	399.00	424.0	0.99	-0.02	1.01	3.69	-1.85
11/12	424.0	451.00	478.0	1.17	0.01	1.17	4.55	-5.91
12/13	478.0	505.50	533.0	1.32	0.14	1.18	3.92	-3.21
13/14	533.0	548.00	563.0	1.11	-0.03	1.14	4.39	-4.39
14/15	563.0	592.00	621.0	0.97	0.10	0.87	3.87	-1.88
15/16	621.0	648.50	676.0	0.81	-0.23	1.04	4.68	-4.37
16/17	676.0	694.00	712.0	1.00	-0.03	1.02	3.93	-2.47
17/18	712.0	736.50	761.0	0.78	-0.32	1.09	4.32	-4.00
18/19	761.0	775.50	790.0	0.76	-0.18	0.95	3.77	-2.62
19/20	790.0	802.00	814.0	0.87	-0.37	1.24	4.37	-5.96
20/21	814.0	840.00	866.0	0.65	-0.18	0.84	3.75	-2.62
21/22	866.0	883.00	900.0	0.66	-0.49	1.15	4.40	-5.48
22/23	900.0	908.50	917.0	0.43	-0.48	0.91	4.06	-3.94
23/24	917.0	926.50	936.0	0.82	-0.37	1.19	4.19	-5.16
24/25	936.0	947.50	959.0	0.74	-0.02	0.76	3.49	-1.93
25/26	959.0	964.50	970.0	0.79	-0.25	1.04	4.25	-2.37
26/27	970.0	976.00	982.0	0.97	-0.02	0.99	3.88	-2.54
27/28	982.0	998.00	1014.0	0.91	0.16	0.75	4.03	-2.40
28/29	1014.0	1022.50	1031.0	1.04	0.00	1.04	3.76	-1.23
29/30	1031.0	1046.50	1062.0	0.89	-0.05	0.94	4.20	-2.15
30/31	1062.0	1071.50	1081.0	0.92	0.12	0.79	3.43	0.23
31/32	1081.0	1092.50	1104.0	0.93	0.17	0.76	3.94	-1.04
32/33	1104.0	1109.00	1114.0	1.06	-0.08	1.14	3.80	-1.28
33/34	1114.0	1127.50	1141.0	0.98	-0.13	1.12	4.17	-2.50
34/35	1141.0	1165.50	1190.0	1.01	0.12	0.90	3.66	0.06
35/36	1190.0	1202.50	1215.0	0.84	-0.19	1.03	4.26	-1.10
36/37	1215.0	1229.50	1244.0	0.77	0.13	0.64	3.56	-0.53
37/38	1244.0	1254.00	1264.0	0.86	-0.23	1.09	4.14	-2.73
38/39	1264.0	1275.00	1286.0	0.92	0.02	0.90	3.77	-1.35
39/40	1286.0	1295.00	1304.0	0.71	-0.15	0.86	4.05	-1.32
40/41	1304.0	1312.00	1320.0	0.99	-0.01	1.01	3.63	0.05
41/42	1320.0	1332.00	1344.0	0.86	-0.26	1.11	3.99	-0.45
42/43	1344.0	1353.00	1362.0	1.02	0.12	0.90	3.48	0.97
43/44	1362.0	1372.50	1383.0	0.93	0.15	0.78	4.02	-0.49
44/45	1383.0	1394.00	1405.0	0.99	0.18	0.80	3.64	-0.11
45/46	1405.0	1414.50	1424.0	0.82	-0.09	0.91	4.05	-0.05
46/47	1424.0	1438.00	1452.0	0.78	0.06	0.72	3.40	1.10
47/48	1452.0	1460.50	1469.0	0.69	-0.17	0.86	4.03	-0.69
48/49	1469.0	1480.50	1492.0	0.63	0.23	0.40	3.43	0.95
49/50	1492.0	1501.00	1510.0	0.93	0.09	0.83	4.14	-0.04
50/51	1510.0	1520.00	1530.0	0.91	0.21	0.70	3.84	0.38
51/52	1530.0	1538.75	1547.5	0.91	-0.07	0.97	4.21	-0.91
52/53	1547.5	1558.75	1570.0	0.94	0.09	0.85	3.75	0.38
53/54	1570.0	1577.50	1585.0	0.75	-0.05	0.80	4.07	0.02
54/55	1585.0	1596.50	1608.0	1.02	0.19	0.83	3.71	0.61
55/56	1608.0	1618.25	1628.5	0.92	0.13	0.79	3.77	0.85
56/57	1628.5	1635.50	1642.5	1.03	0.14	0.88	3.66	0.60
57/58	1642.5	1656.25	1670.0	0.93	0.11	0.81	4.08	-0.70
58/59	1670.0	1683.75	1697.5	0.84	-0.11	0.94	3.74	0.24
59/60	1697.5	1706.25	1715.0	0.80	-0.06	0.85	3.93	-0.01
60/61	1715.0	1729.00	1743.0	0.77	-0.08	0.85	3.73	0.51
61/62	1743.0	1750.50	1758.0	0.52	0.00	0.52	3.86	-0.11
62/63	1758.0	1770.00	1782.0	0.84	-0.01	0.85	3.52	0.96
63/64	1782.0	1792.25	1802.5	0.77	-0.11	0.88	3.94	0.14
64/65	1802.5	1809.25	1816.0	0.93	0.13	0.80	3.67	0.73
65/66	1816.0	1821.00	1826.0	0.96	0.11	0.85	3.61	0.61
66/67	1826.0	1829.25	1832.5	0.89	-0.03	0.92	3.58	1.34
67/68	1832.5	1840.75	1849.0	0.92	-0.17	1.09	3.74	1.28
68/69	1849.0	1854.25	1859.5	0.69	0.04	0.66	3.61	0.67
69/70	1859.5	1867.25	1875.0	0.63	0.12	0.51	3.82	0.61
70/71	1875.0	1886.50	1898.0	0.95	0.13	0.82	3.62	1.05
71/72	1898.0	1906.50	1915.0	0.77	-0.10	0.87	3.98	1.06
72/73	1915.0	1928.00	1941.0	0.57	0.08	0.49	3.59	1.68
73/74	1941.0	1953.00	1965.0	0.68	-0.20	0.88	3.89	0.73
74/75	1965.0	1977.50	1990.0	1.18	0.06	1.12	3.47	1.50
75/76	1990.0	2003.50	2017.0	1.12	0.17	0.95	3.74	1.39
76/77	2017.0	2030.00	2043.0	1.13	0.28	0.84	3.54	1.59
77/78	2043.0	2065.50	2088.0	0.92	-0.09	1.01	3.93	0.40
78/79	2088.0	2095.50	2103.0	0.56	0.01	0.55	3.65	0.66
79/80	2103.0	2114.00	2125.0	0.64	-0.14	0.77	3.63	1.07
80/81	2125.0	2135.50	2146.0	0.79	-0.03	0.81	3.43	1.81
81/82	2146.0	2157.00	2168.0	0.82	-0.26	1.08	4.07	0.28
82/83	2168.0	2180.00	2192.0	0.94	-0.21	1.16	3.55	1.33
83/84	2192.0	2199.75	2207.5	0.82	-0.32	1.14	3.77	1.37
84/85	2207.5	2221.75	2236.0	0.83	-0.04	0.87	3.50	1.70
85/86	2236.0	2243.00	2250.0	0.75	-0.25	0.99	3.83	1.05
86/87	2250.0	2261.50	2273.0	0.87	0.12	0.75	3.44	1.59
87/88	2273.0	2282.00	2291.0	0.78	-0.26	1.04	3.83	1.63
88/89	2291.0	2300.00	2309.0	0.77	-0.01	0.78	3.41	1.97
89/90	2309.0	2321.00	2333.0	0.79	-0.07	0.86	3.68	1.57
90/91	2333.0	2341.50	2350.0	0.81	-0.08	0.89	3.35	2.07
91/92	2350.0	2361.50	2373.0	1.07	-0.04	1.10	3.75	1.26
92/93	2373.0	2380.00	2387.0	1.14	0.10	1.03	3.32	1.78
93/94	2387.0	2397.00	2407.0	1.08	0.21	0.87	3.52	2.11
94/95	2407.0	2417.00	2427.0	0.95	0.17	0.78	3.43	2.53
95/96	2427.0	2439.50	2452.0	0.74	-0.11	0.85	3.99	1.22
96/97	2452.0	2464.50	2477.0	0.68	0.12	0.56	3.45	1.83
97/98	2477.0	2485.50	2494.0	0.42	-0.09	0.51	3.91	1.28
98/99	2494.0	2502.00	2510.0	0.56	0.04	0.52	3.51	2.05
99/100	2510.0	2525.00	2540.0	0.36	-0.05	0.41	3.94	0.93
100/101	2540.0	2547.00	2554.0	0.70	0.17	0.53	3.32	2.49
101/102	2554.0	2564.50	2575.0	0.49	0.05	0.44	3.48	2.28
102/103	2575.0	2585.00	2595.0	0.65	0.02	0.63	3.32	2.47
103/104	2595.0	2604.50	2614.0	0.59	0.10	0.49	3.74	1.81
104/G1	2614.0	2626.00	2638.0	0.56	0.23	0.33	3.41	1.94
G1/G2	2638.0	2645.00	2652.0	0.67	0.02	0.65	3.68	1.70
G2/G3	2652.0	2666.50	2681.0	0.89	0.24	0.65	3.28	2.62
G3/G4	2681.0	2685.50	2690.0	0.90	0.28	0.62	3.81	2.29
G4/G5	2690.0	2697.00	2704.0	1.00	0.11	0.89	3.64	2.24
G5/G6	2704.0	2717.00	2730.0	0.72	0.06	0.67	3.76	1.85
G6/G7	2730.0	2744.50	2759.0	0.91	-0.17	1.09	3.26	2.21
G7/G8	2759.0	2768.00	2777.0	0.84	0.10	0.75	3.34	2.22
G8/G9	2777.0	2787.50	2798.0	1.00	0.17	0.83	3.26	2.74
G9/G10	2798.0	2809.00	2820.0	0.78	0.24	0.54	3.65	2.49
G10/G11	2820.0	2829.00	2838.0	1.21	0.18	1.03	3.28	3.08
G11/G12	2838.0	2848.00	2858.0	0.95	0.17	0.77	3.46	2.69
G12/G13	2858.0	2867.00	2876.0	1.13	0.34	0.79	3.33	2.69
G13/G14	2876.0	2884.50	2893.0	1.19	0.25	0.94	3.46	2.51
G14/G15	2893.0	2903.00	2913.0	0.98	0.33	0.65	3.25	2.65
G15/G16	2913.0	2925.00	2937.0	0.73	0.22	0.51	3.52	2.20
G16/G17	2937.0	2951.50	2966.0	0.90	0.17	0.72	3.15	3.06
G17/G18	2966.0	2974.25	2982.5	0.96	0.04	0.93	3.46	2.49
G18/G19	2982.5	2990.75	2999.0	0.96	0.15	0.81	3.29	2.34
G19/G20	2999.0	3012.00	3025.0	0.74	0.00	0.73	3.46	2.12
G20/G21	3025.0	3032.00	3039.0	0.58	0.02	0.55	3.22	2.30
G21/G22	3039.0	3047.00	3055.0	0.37	-0.05	0.42	3.32	2.46
G22/K1	3055.0	3071.00	3087.0	0.67	0.25	0.42	3.18	3.13
K1/K2	3087.0	3092.00	3097.0	0.52	0.29	0.23	3.14	3.41
K2/KM1	3097.0	3108.00	3119.0	0.72	0.19	0.53	3.19	3.40
KM1/KM2	3119.0	3134.50	3150.0	0.71	-0.03	0.74	3.36	2.86
KM2/KM3	3150.0	3158.50	3167.0	0.77	0.22	0.55	3.05	3.32
KM3/KM4	3167.0	3175.50	3184.0	0.59	0.36	0.23	3.15	2.85
KM4/KM5	3184.0	3198.00	3212.0	0.67	0.38	0.28	3.12	3.15
KM5/KM6	3212.0	3225.00	3238.0	0.80	0.40	0.39	3.09	2.93
KM6/M1	3238.0	3251.00	3264.0	0.79	0.27	0.51	3.13	3.04
M1/M2	3264.0	3288.00	3312.0	0.68	0.01	0.67	3.41	2.62
M2/MG1	3312.0	3322.00	3332.0	0.64	0.05	0.59	3.13	2.76
MG1/MG2	3332.0	3339.50	3347.0	0.79	0.06	0.72	3.22	2.83
MG2/MG3	3347.0	3359.50	3372.0	0.12	0.02	0.10	3.19	3.39
MG3/MG4	3372.0	3379.50	3387.0	0.70	0.10	0.59	3.25	3.20
MG4/MG5	3387.0	3415.50	3444.0	0.55	0.07	0.48	3.12	3.51
MG5/MG6	3444.0	3457.50	3471.0	0.62	0.15	0.47	3.08	3.51
MG6/MG7	3471.0	3494.00	3517.0	0.76	0.31	0.46	2.98	3.97
MG7/MG8	3517.0	3524.50	3532.0	0.68	0.32	0.36	3.00	3.75
MG8/MG9	3532.0	3539.00	3546.0	0.86	0.32	0.54	3.08	3.67
MG9/MG10	3546.0	3556.00	3566.0	0.90	0.27	0.63	3.01	3.70
MG10/MG11	3566.0	3572.00	3578.0	0.89	0.32	0.58	2.85	3.68
MG11/MG12	3578.0	3585.00	3592.0	0.77	0.21	0.55	3.12	3.68
MG12/Gi1	3592.0	3605.50	3619.0	0.84	0.26	0.58	2.91	4.16
Gi1/Gi2	3619.0	3628.00	3637.0	0.65	0.30	0.35	3.23	4.11
Gi2/Gi3	3637.0	3648.50	3660.0	0.70	0.28	0.42	3.07	4.03
Gi3/Gi4	3660.0	3668.00	3676.0	0.46	0.13	0.34	3.27	3.98
Gi4/Gi5	3676.0	3690.50	3705.0	0.49	0.16	0.33	3.00	4.03
Gi5/Gi6	3705.0	3712.00	3719.0	0.54	0.10	0.44	3.16	3.76
Gi6/Gi7	3719.0	3730.50	3742.0	0.52	0.22	0.31	2.97	4.06
Gi7/Gi8	3742.0	3747.00	3752.0	0.16	0.16	0.00	3.14	4.14
Gi8/Gi9	3752.0	3760.00	3768.0	0.86	0.20	0.66	2.91	4.28
Gi9/Gi10	3768.0	3783.00	3798.0	0.66	0.07	0.59	2.99	4.29
Gi10/Gi11	3798.0	3810.00	3822.0	0.61	0.08	0.53	3.01	4.17
Gi11/Gi12	3822.0	3828.50	3835.0	0.03	-0.04	0.06	3.06	4.15
Gi12/Gi13	3835.0	3848.50	3862.0	0.36	0.15	0.21	2.92	4.43
Gi13/Gi14	3862.0	3870.50	3879.0	0.25	0.12	0.13	3.17	4.30
Gi14/Gi15	3879.0	3895.50	3912.0	0.51	0.17	0.34	2.94	4.49
Gi15/Gi16	3912.0	3917.50	3923.0	0.29	-0.02	0.31	3.07	4.14
Gi16/Gi17	3923.0	3931.00	3939.0	0.64	0.19	0.44	2.92	4.47
Gi17/Gi18	3939.0	3945.50	3952.0	0.65	0.19	0.46	3.00	4.71
Gi18/Gi19	3952.0	3965.00	3978.0	0.62	0.19	0.43	2.93	4.45
Gi19/Gi20	3978.0	3992.50	4007.0	0.62	0.15	0.47	3.14	3.90
Gi20/Gi21	4007.0	4018.00	4029.0	0.71	0.14	0.56	3.00	4.31
Gi21/Gi22	4029.0	4038.50	4048.0	0.39	-0.03	0.42	3.17	4.16
Gi22/Gi23	4048.0	4066.50	4085.0	0.64	0.05	0.59	3.06	4.44
Gi23/Gi24	4085.0	4091.50	4098.0	0.73	0.05	0.67	2.95	4.21
Gi24/Gi25	4098.0	4122.00	4146.0	0.68	0.06	0.63	2.94	4.08
Gi25/Gi26	4146.0	4160.50	4175.0	0.87	0.14	0.73	3.03	4.23
Gi26/Gi27	4175.0	4183.50	4192.0	0.81	0.30	0.50	2.91	4.32
Gi27/Gi28	4192.0	4201.50	4211.0	0.42	0.28	0.14	2.99	3.79
Gi28/Co1	4211.0	4221.50	4232.0	0.55	0.22	0.32	2.93	4.19
Co1/Co2	4232.0	4245.50	4259.0	0.56	0.32	0.23	3.01	4.31
Co2/Co3	4259.0	4272.50	4286.0	0.67	0.18	0.49	2.94	4.39
Co3/Co4	4286.0	4294.50	4303.0	0.70	0.13	0.57	2.99	4.43
Co4/CN1	4303.0	4315.00	4327.0	0.60	0.08	0.52	2.90	4.27
CN1/CN2	4327.0	4331.00	4335.0	0.58	0.11	0.46	2.90	3.95
CN2/CN3	4335.0	4345.50	4356.0	0.63	0.16	0.47	2.95	3.86
CN3/CN4	4356.0	4363.50	4371.0	0.73	0.39	0.33	3.04	4.02
CN4/CN5	4371.0	4383.00	4395.0	0.60	0.35	0.25	2.99	4.21
CN5/CN6	4395.0	4407.50	4420.0	0.54	0.21	0.33	3.00	3.83
CN6/CN7	4420.0	4433.00	4446.0	0.73	0.21	0.52	3.02	3.97
CN7/CN8	4446.0	4451.50	4457.0	0.62	0.10	0.52	3.00	3.93
CN8/N1	4457.0	4472.00	4487.0	0.81	0.14	0.67	2.95	3.95
N1/N2	4487.0	4497.50	4508.0	0.62	0.27	0.35	3.14	3.88