# North Atlantic Ocean Western Boundary Current Globorotalia truncatulinoides Coiling Ratio Data for the past 700 kyr
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#               World Data Service for Paleoclimatology, Boulder
#                                   and
#                      NOAA Paleoclimatology Program
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# Template Version 3.0
# Encoding: UTF-8
# NOTE: Please cite original publication, online resource and date accessed when using this data.
# If there is no publication information, please cite Investigator, title, online resource and date accessed.
#
# Description/Documentation lines begin with #
# Data lines have no #
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# Online_Resource: https://www.ncdc.noaa.gov/paleo/study/30952
#      Description: NOAA Landing Page
# Online_Resource: https://www.ncei.noaa.gov/pub/data/paleo/contributions_by_author/billups2020-pp/billups2020-pp-1063.txt
#      Description: NOAA location of the template
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# Data_Type: Paleoceanography
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# Dataset_DOI:
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# Parameter_Keywords: population abundance
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# Contribution_Date
#    Date: 2020-08-24
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# File_Last_Modified_Date
#    Date: 2020-08-24
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# Title
#    Study_Name: North Atlantic Ocean Western Boundary Current Globorotalia truncatulinoides Coiling Ratio Data for the past 700 kyr
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# Investigators
#      Investigators: Billups, Katharina; Vizcaíno, Maoli; Chiarelli, Josephine; Kaiser, Emily
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# Description_Notes_and_Keywords
#        Description: 
#         Provided Keywords: Pleistocene, Globorotalia truncatulinoides, subtropical gyre, water column structure, North Atlantic Ocean
#---------------------------------------
# Publication
# Authors: Billups, Katharina, Maoli Vizcaíno, Josephine Chiarelli, and Emily Kaiser
# Published_Date_or_Year: 2020
# Published_Title: Reconstructing western boundary current stability in the North Atlantic Ocean for the past 700 kyr from Globorotalia truncatulinoides coiling ratios
# Journal_Name: Paleoceanography and Paleoclimatology
# Volume: in review
# Edition: 
# Issue: 
# Pages: 
# Report_Number: 
# DOI: 
# Online_Resource: 
# Full_Citation: 
# Abstract: Down-core changes in the coiling direction of Globorotalia truncatulinoides in the northwestern subtropical Atlantic (KNR140-37PC and Ocean Drilling Program Sites 1063, 1059, 1056, 1058) provide a tracer for the hydrographic conditions in the western boundary current over the past 700 kyr (Marine Isotope Stage, MIS, 1-17). A consistent association between percent G. truncatulinoides (sinistral) abundances, total test counts, and bulk sediment CaCO3 content is established by MIS 11 suggesting a response to ocean-atmosphere interactions during the mid Brunhes event. Commencing with MIS 11, interglacial maxima are associated with high total test counts and either distinct sinistral test minima (MIS 9e, 11c) or maxima (MIS 1, 5e, 7a). High sinistral test abundances with relatively high test counts is similar to the late Holocene relationship at the study sites. Low sinistral test abundances despite high test counts means that coiling ratios are dominated by dextral forms. We interpret this pattern to indicate more intense flow in the subtropical gyre either via the western boundary current drawing toward the gyre center, or a more northern influence of the North Equatorial and Antilles Currents. This suggests that the western boundary current may have been more intense during MIS 11c and MIS 9e then during MIS 7a, MIS 5e, and MIS 1 consistent with climate warm anomalies in northern Europe at these times. Regardless of the mechanism, the observation that minima and maxima in sinistral test abundances are prolonged at these times indicates that the western gyre boundary remained stable during relative warm intervals.
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# Funding_Agency
#    Funding_Agency_Name: 
#    Grant: 
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# Site_Information
# Site_Name: ODP 1063
# Location: North Atlantic Ocean
# Northernmost_Latitude: 33.67
# Southernmost_Latitude: 33.67
# Easternmost_Longitude: -57.62
# Westernmost_Longitude: -57.62
# Elevation: -4595
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# Data_Collection
#   Collection_Name: ODP1063 G.trunc Billups2020
#   First_Year: 313040
#   Last_Year: 2740
#   Time_Unit: cal yr BP
#   Core_Length: 67.85
#   Notes: Ages are from Channell et al. (2012): Channell, J. E. T., Hodell, D. A., and Curtis, J. H. (2012), ODP Site 1063 (Bermuda Rise) revisited: Oxygen isotopes, excursions and paleointensity in the Brunhes Chron, Geochem. Geophys. Geosyst., 13, Q02001, doi:10.1029/2011GC003897. The Marine Isotope Stage 5 portion of the age model has been revised recently and the data are availble on pangaea.de (Channell, personal communication July 2020)
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# Chronology_Information 
# Chronology: 
# Ages are from Channell et al. (2012): Channell, J. E. T., Hodell, D. A., and Curtis, J. H. (2012), ODP Site 1063 (Bermuda Rise) revisited: Oxygen isotopes, excursions and paleointensity in the Brunhes Chron, Geochem. Geophys. Geosyst., 13, Q02001, doi:10.1029/2011GC003897. The Marine Isotope Stage 5 portion of the age model has been revised recently and the data are availble on pangaea.de (Channell, personal communication July 2020)
# Chronology Table (Use as many rows and columns are needed below this line)	NOTE: Additional Chronology tables should be put below the first one with no blank lines. 	
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# Variables
# Data variables follow that are preceded by "##" in columns one and two.
# Variables list, one per line, shortname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data)
## Depth	depth,,,meter,,paleoceanography,,,N,meters composite depth
## Age	age,,,calendar kiloyear before present,,paleoceanography,,,N,interval age
## sinistral	Globorotalia truncatulinoides,,,count,,paleoceanography,,microscopy,N,total number of Globorotalia truncatulinoides (sinistral) tests; visual counts using a microscope
## dextral	Globorotalia truncatulinoides,,,count,,paleoceanography,,microscopy,N,total number of Globorotalia truncatulinoides (dextral) tests; visual counts using a microscope
## total	Globorotalia truncatulinoides,,,count,,paleoceanography,,,N,total number of Globorotalia truncatulinoides (sinistral plus dextral) tests
## %sinistral	Globorotalia truncatulinoides,,,percent,,paleoceanography,,,N,percent sinistral test (number of sinistral tests/number of total tests*100
#------------------------
# Data:
# Data lines follow (have no #)
# Data line format - tab-delimited text, variable short name as header
# Missing_Values: NA
Depth	Age	sinistral	dextral	total	%sinistral	
0.35	2.74	66	3	69	95.7	
0.4	3.13	98	13	110	88.3	
0.45	3.52	116	17	133	87.2	
0.5	3.92	107	22	129	82.9	
0.65	5.09	840	134	194	86.2	
0.75	5.87	108	28	136	79.4	
0.9	7.05	110	41	151	72.8	
1.05	8.22	147	27	174	84.5	
1.2	9.40	118	40	158	74.7	
1.3	10.18	59	56	115	51.3	
1.45	11.36	29	11	40	72.5	
1.6	12.53	11	2	13	84.6	
1.75	13.15	0	0	0	0.0	
1.8	13.23	0	0	0	0.0	
2	13.56	10	2	12	83.3	
2.25	13.97	9	6	15	60.0	
2.45	14.30	7	7	14	50.0	
2.55	14.47	1	0	1	100.0	
2.8	14.88	1	12	13	7.7	
3.05	15.29	0	6	6	0.0	
3.2	15.54	1	23	24	4.2	
3.35	15.79	3	9	12	25.0	
3.55	16.12	0	0	0	0.0	
3.7	16.36	1	1	2	50.0	
3.95	16.78	0	5	5	0.0	
4.25	17.27	1	6	7	14.3	
4.4	17.52	1	23	24	4.2	
4.55	17.76	2	8	10	20.0	
4.65	17.93	0	0	0	0.0	
4.8	18.18	3	6	9	33.3	
4.95	18.42	0	1	1	0.0	
5.05	18.59	0	1	1	0.0	
5.15	18.75	0	3	3	0.0	
5.3	19.00	0	1	1	0.0	
5.35	19.08	0	9	9	0.0	
5.45	19.25	0	1	1	0.0	
5.55	19.41	0	2	2	0.0	
5.62	19.53	0	1	1	0.0	
5.75	19.74	0	4	4	0.0	
5.85	19.91	0	1	1	0.0	
5.9	19.99	25	8	33	75.8	
6	20.16	0	12	12	0.0	
6.1	20.32	0	6	6	0.0	
6.2	20.49	1	14	15	6.7	
6.3	20.65	1	6	7	14.3	
6.5	20.98	0	2	2	0.0	
6.6	21.14	1	3	4	25.0	
6.69	21.29	0	8	8	0.0	
6.79	21.46	0	2	2	0.0	
6.89	21.62	0	5	5	0.0	
7.09	21.95	0	12	12	0.0	
7.24	22.20	0	5	5	0.0	
7.39	22.45	0	1	1	0.0	
7.54	22.69	0	2	2	0.0	
7.59	22.78	0	7	7	0.0	
7.64	22.86	0	4	4	0.0	
7.74	23.02	0	5	5	0.0	
7.89	23.27	1	4	5	20.0	
7.99	23.44	0	0	0	0.0	
8.19	23.77	0	2	2	0.0	
8.29	23.93	0	2	2	0.0	
8.34	24.01	0	1	1	0.0	
8.44	24.18	0	1	1	0.0	
8.54	24.34	0	1	1	0.0	
8.69	24.59	0	3	3	0.0	
8.79	24.76	0	3	3	0.0	
8.89	24.92	0	0	0	0.0	
8.99	25.08	0	4	4	0.0	
9.04	25.17	9	1	10	90.0	
9.09	25.25	0	1	1	0.0	
9.19	25.41	0	1	1	0.0	
9.44	25.83	0	0	0	0.0	
9.54	25.99	0	0	0	0.0	
9.64	26.16	1	7	8	12.5	
9.89	26.57	7	0	7	100.0	
10.39	27.39	0	4	4	0.0	
10.49	27.56	4	1	5	80.0	
10.54	27.64	1	5	6	16.7	
10.64	27.81	0	1	1	0.0	
10.74	27.97	0	2	2	0.0	
10.84	28.13	0	0	0	0.0	
10.94	28.30	0	4	4	0.0	
11.14	28.63	9	3	12	75.0	
11.29	28.88	0	2	2	0.0	
11.49	29.21	0	0	0	0.0	
11.69	29.54	0	5	5	0.0	
11.99	30.03	13	4	17	76.5	
12.01	30.06	1	9	10	10.0	
12.16	30.31	0	0	0	0.0	
12.26	30.48	0	5	5	0.0	
12.36	30.64	0	2	2	0.0	
12.46	30.81	0	9	9	0.0	
12.56	30.97	5	3	8	62.5	
12.66	31.14	1	8	9	11.1	
12.76	31.30	0	2	2	0.0	
12.91	31.55	0	7	7	0.0	
13.01	31.71	0	2	2	0.0	
13.11	31.88	0	5	5	0.0	
13.21	32.04	1	2	3	33.3	
13.26	32.12	12	9	21	57.1	
13.31	32.21	0	9	9	0.0	
13.41	32.37	0	14	14	0.0	
13.61	32.70	2	2	4	50.0	
13.71	32.87	0	1	1	0.0	
13.81	33.03	1	0	1	100.0	
13.91	33.20	0	6	6	0.0	
13.96	33.28	7	7	14	50.0	
14.01	33.36	0	13	13	0.0	
14.11	33.53	0	1	1	0.0	
14.21	33.69	0	0	0	0.0	
14.36	33.94	0	5	5	0.0	
14.47	34.12	0	6	6	0.0	
14.52	34.20	1	5	6	16.7	
14.62	34.37	1	6	7	14.3	
14.67	34.45	8	5	13	61.5	
14.72	34.53	1	4	5	20.0	
14.82	34.70	0	30	30	0.0	
14.97	34.94	0	5	5	0.0	
15.07	35.11	0	0	0	0.0	
15.17	35.27	1	1	2	50.0	
15.32	35.52	0	1	1	0.0	
15.37	35.60	12	7	19	63.2	
15.42	35.69	0	8	8	0.0	
15.52	35.85	9	62	71	12.7	
16.07	36.76	0	1	1	0.0	
16.52	37.50	18	3	21	85.7	
16.87	38.08	25	2	27	92.6	
17.22	38.65	8	27	35	22.9	
17.62	39.31	4	4	8	50.0	
17.97	39.89	3	18	21	14.3	
18.42	40.63	3	5	8	37.5	
18.72	41.14	2	0	2	100.0	
19.12	42.48	38	3	41	92.7	
19.62	44.14	6	2	8	75.0	
19.82	44.81	23	6	29	79.3	
20.22	46.14	4	25	29	13.8	
20.77	47.97	1	0	1	100.0	
20.92	48.47	2	12	14	14.3	
21.32	49.80	3	52	55	5.5	
21.67	50.97	2	23	25	8.0	
22.12	52.47	0	4	4	0.0	
22.42	53.47	3	5	8	37.5	
22.82	54.80	1	31	32	3.1	
23.17	55.97	0	0	0	0.0	
23.57	57.30	0	1	1	0.0	
24.23	59.63	2	38	40	5.0	
24.67	61.26	2	5	7	28.6	
24.97	62.38	2	1	3	66.7	
25.02	62.56	0	2	2	0.0	
25.37	63.86	0	0	0	0.0	
25.52	64.42	0	1	1	0.0	
25.57	64.60	0	0	0	0.0	
26.82	69.24	0	0	0	0.0	
27.82	73.00	39	2	41	95.1	
28.07	74.18	4	1	5	80.0	
28.22	74.88	2	0	2	100.0	
28.37	75.59	0	0	0	0.0	
28.88	77.98	3	0	3	100.0	
29.08	78.92	34	14	48	70.8	
29.33	80.10	3	0	3	100.0	
29.53	81.04	18	1	19	94.7	
29.78	82.21	28	8	36	77.8	
29.98	83.15	61	15	76	80.3	
30.18	84.09	174	4	178	97.8	
30.33	84.79	108	5	113	95.6	
30.43	85.26	157	7	164	95.7	
30.53	85.73	91	15	106	85.8	
30.58	85.97	144	28	172	83.7	
30.68	86.44	29	28	57	50.9	
30.78	86.91	0	0	0	0.0	
30.88	87.37	43	0	43	100.0	
30.93	87.61	9	1	10	90.0	
31.03	88.08	29	0	29	100.0	
31.28	89.25	36	3	39	92.3	
31.53	90.43	11	5	16	68.8	
31.68	91.13	74	11	85	87.1	
31.88	92.07	113	8	121	93.4	
32.08	93.01	64	3	67	95.5	
32.28	93.95	97	10	107	90.7	
32.43	94.65	78	8	86	90.7	
32.63	95.59	41	1	42	97.6	
32.83	96.53	75	9	84	89.3	
33.03	97.47	133	15	148	89.9	
33.18	98.18	114	20	134	85.1	
33.38	99.21	305	22	327	93.3	
33.48	99.87	116	6	122	95.1	
33.63	100.87	102	8	110	92.7	
33.78	101.86	93	8	101	92.1	
33.88	102.53	145	15	160	90.6	
34.03	103.52	90	17	107	84.1	
34.18	104.52	61	12	73	83.6	
34.28	105.18	105	17	122	86.1	
34.43	106.17	1	0	1	100.0	
34.68	107.83	2	1	3	66.7	
34.78	108.49	36	6	42	85.7	
34.93	109.49	87	19	106	82.1	
35.03	110.15	60	16	76	78.9	
35.13	110.82	10	31	41	24.4	
35.23	111.48	25	67	92	27.2	
35.38	112.51	51	19	70	72.9	
35.43	112.87	232	43	275	84.4	
35.53	113.57	117	24	141	83.0	
35.63	114.28	249	49	298	83.6	
35.73	114.98	9	47	56	16.1	
35.88	116.04	1	9	10	10.0	
35.98	118.59	3	7	10	30.0	
36.13	122.72	2	6	8	25.0	
36.33	128.22	6	3	9	66.7	
36.53	131.37	66	87	153	43.1	
36.58	131.44	152	47	199	76.4	
36.78	131.71	67	31	98	68.4	
36.98	131.97	126	7	133	94.7	
37.03	132.04	165	15	180	91.7	
37.08	132.11	131	17	148	88.5	
37.18	132.24	1	5	6	16.7	
37.23	132.31	2	18	20	10.0	
37.28	132.38	1	9	10	10.0	
37.33	132.44	2	33	35	5.7	
37.38	132.51	3	49	52	5.8	
37.43	132.58	0	8	8	0.0	
37.48	132.65	0	11	11	0.0	
37.53	132.71	3	14	17	17.6	
37.58	132.78	0	2	2	0.0	
37.63	132.85	0	4	4	0.0	
37.68	132.91	0	13	13	0.0	
37.73	132.98	0	7	7	0.0	
37.78	133.05	0	7	7	0.0	
37.98	133.32	0	0	0	0.0	
38.21	133.62	0	6	6	0.0	
38.36	133.83	0	8	8	0.0	
38.56	134.15	0	2	2	0.0	
38.91	134.89	0	1	1	0.0	
39.21	135.53	0	4	4	0.0	
39.56	136.28	0	2	2	0.0	
39.71	136.60	0	2	2	0.0	
39.81	136.81	0	1	1	0.0	
39.91	137.02	2	3	5	40.0	
40.06	137.34	0	1	1	0.0	
40.26	137.77	0	2	2	0.0	
40.41	138.09	1	3	4	25.0	
40.56	138.40	5	5	10	50.0	
40.71	138.72	1	0	1	100.0	
40.91	139.15	1	0	1	100.0	
41.44	140.28	5	1	6	83.3	
41.54	140.49	4	2	6	66.7	
41.64	140.70	2	0	2	100.0	
41.74	140.91	2	1	3	66.7	
41.99	141.45	10	0	10	100.0	
42.14	141.77	0	2	2	0.0	
42.24	141.98	1	1	2	50.0	
42.34	142.20	8	0	8	100.0	
42.44	142.41	20	3	23	87.0	
42.54	142.63	12	13	25	48.0	
42.64	142.85	0	0	0	0.0	
42.79	143.22	11	3	14	78.6	
42.94	143.64	0	1	1	0.0	
43.09	144.06	0	1	1	0.0	
43.44	145.16	3	7	10	30.0	
43.64	145.81	4	23	27	14.8	
43.99	146.94	1	10	11	9.1	
44.39	148.19	0	6	6	0.0	
44.84	149.65	0	7	7	0.0	
45.44	151.55	0	5	5	0.0	
45.79	152.68	0	1	1	0.0	
46.24	154.10	0	3	3	0.0	
46.74	155.71	0	6	6	0.0	
47.24	157.29	0	41	41	0.0	
47.65	158.61	0	9	9	0.0	
47.9	159.41	0	4	4	0.0	
48.15	160.19	1	32	33	3.0	
48.4	161.00	0	2	2	0.0	
49.15	163.39	0	4	4	0.0	
49.35	164.03	0	4	4	0.0	
49.6	164.87	0	3	3	0.0	
49.8	165.57	1	23	24	4.2	
50.05	166.46	6	218	224	2.7	
50.3	167.36	0	3	3	0.0	
50.55	168.28	0	6	6	0.0	
50.75	169.08	0	13	13	0.0	
50.95	169.88	2	56	58	3.4	
51.15	170.71	0	23	23	0.0	
51.35	171.54	2	34	36	5.6	
51.55	172.39	2	12	14	14.3	
51.8	173.46	0	2	2	0.0	
52.2	175.60	0	30	30	0.0	
52.3	176.27	1	50	51	2.0	
52.4	176.93	0	8	8	0.0	
52.7	178.93	0	1	1	0.0	
52.85	180.00	2	38	40	5.0	
53.05	181.43	1	12	13	7.7	
52.48	177.47	1	99	100	1.0	
52.63	178.47	0	4	4	0.0	
52.78	179.50	1	5	6	16.7	
52.98	180.93	0	15	15	0.0	
53.08	181.64	1	15	16	6.3	
53.18	182.36	0	2	2	0.0	
53.28	183.07	0	1	1	0.0	
53.38	183.79	1	2	3	33.3	
53.48	184.50	1	12	13	7.7	
53.63	185.53	0	0	0	0.0	
53.73	186.21	0	0	0	0.0	
54.03	188.36	0	0	0	0.0	
54.08	188.71	0	6	6	0.0	
54.13	189.07	0	12	12	0.0	
54.18	189.43	0	8	8	0.0	
54.23	189.79	0	25	25	0.0	
54.28	190.14	1	13	14	7.1	
54.33	190.50	2	93	95	2.1	
54.43	191.21	0	22	22	0.0	
54.48	191.57	1	24	25	4.0	
54.53	191.93	0	1	1	0.0	
55.01	195.62	1	0	1	100.0	
55.08	196.17	2	1	3	66.7	
55.23	197.38	0	0	0	0.0	
55.38	198.64	108	14	122	88.5	
55.43	199.09	145	31	176	82.4	
55.48	199.55	230	41	271	84.9	
55.63	200.83	266	54	320	83.1	
55.81	202.45	4	1	5	80.0	
56.06	204.64	20	16	36	55.6	
56.13	205.27	13	6	19	68.4	
56.18	205.73	25	36	61	41.0	
56.33	207.08	14	84	98	14.3	
56.38	207.50	9	74	83	10.8	
56.48	208.36	18	81	99	18.2	
56.63	209.73	47	60	107	43.9	
56.73	210.64	134	124	258	51.9	
56.78	211.08	67	218	285	23.5	
56.93	212.36	6	107	113	5.3	
56.98	212.82	4	225	229	1.7	
57.03	213.27	4	198	202	2.0	
57.08	213.73	15	242	257	5.8	
57.13	214.17	0	47	47	0.0	
57.21	214.83	0	0	0	0.0	
57.31	215.73	0	0	0	0.0	
57.43	216.82	0	2	2	0.0	
57.51	217.55	0	1	1	0.0	
57.65	218.75	1	1	2	50.0	
57.78	219.91	0	0	0	0.0	
57.98	221.73	4	0	4	100.0	
58.03	222.17	1	1	2	50.0	
58.08	222.58	9	1	10	90.0	
58.13	223.00	0	0	0	0.0	
58.18	223.45	23	4	27	85.2	
58.23	223.91	14	3	17	82.4	
58.28	224.36	4	220	224	1.8	
58.33	224.82	101	12	113	89.4	
58.38	225.25	1	0	1	100.0	
58.43	225.67	4	0	4	100.0	
58.51	226.36	0	0	0	0.0	
58.85	229.42	1	6	7	14.3	
58.97	230.45	0	0	0	0.0	
59.05	231.18	0	0	0	0.0	
59.06	231.27	0	0	0	0.0	
59.43	234.55	3	1	4	75.0	
59.48	235.00	11	1	12	91.7	
59.53	235.45	52	9	61	85.2	
59.58	235.91	37	38	75	49.3	
59.63	236.33	17	71	88	19.3	
59.68	236.75	14	144	158	8.9	
59.73	237.18	14	354	368	3.8	
59.78	237.64	4	231	235	1.7	
59.81	237.91	3	175	178	1.7	
59.86	238.36	2	297	299	0.7	
59.91	238.82	1	142	143	0.7	
59.96	239.27	0	98	98	0.0	
60.01	239.73	0	75	75	0.0	
60.06	240.17	0	44	44	0.0	
60.11	240.58	1	4	5	20.0	
60.16	241.00	1	16	17	5.9	
60.21	241.45	0	3	3	0.0	
60.26	241.91	0	4	4	0.0	
60.31	242.36	0	84	84	0.0	
60.36	242.82	3	243	246	1.2	
60.41	243.25	4	183	187	2.1	
60.46	243.67	2	43	45	4.4	
60.51	244.09	1	45	46	2.2	
60.56	244.55	0	13	13	0.0	
60.61	245.00	0	1	1	0.0	
60.66	245.45	0	0	0	0.0	
60.71	245.91	0	17	17	0.0	
60.81	246.82	0	0	0	0.0	
60.91	247.67	0	9	9	0.0	
60.96	248.09	1	9	10	10.0	
61.01	248.55	1	49	50	2.0	
61.06	249.00	4	120	124	3.2	
61.11	249.45	4	47	51	7.8	
61.16	249.91	0	13	13	0.0	
61.21	250.44	0	3	3	0.0	
61.26	251.00	0	0	0	0.0	
61.31	251.50	0	0	0	0.0	
61.36	252.00	1	12	13	7.7	
61.41	252.56	0	9	9	0.0	
61.46	253.13	0	4	4	0.0	
61.51	253.75	4	25	29	13.8	
61.56	254.38	14	45	59	23.7	
61.61	255.00	22	94	116	19.0	
61.66	255.71	11	56	67	16.4	
61.71	256.38	11	32	43	25.6	
61.76	257.00	52	58	110	47.3	
61.81	257.71	53	56	109	48.6	
61.86	258.38	59	47	106	55.7	
61.96	259.71	19	5	24	79.2	
62.01	260.38	48	22	70	68.6	
62.06	261.00	42	36	78	53.8	
62.11	261.71	29	44	73	39.7	
62.16	262.38	12	33	45	26.7	
62.21	263.00	50	33	83	60.2	
62.26	263.71	31	25	56	55.4	
62.31	264.38	9	8	17	52.9	
62.36	265.00	18	4	22	81.8	
62.41	265.71	18	5	23	78.3	
62.46	266.38	51	18	69	73.9	
62.51	267.00	51	22	73	69.9	
62.56	267.71	23	7	30	76.7	
62.61	268.38	29	7	36	80.6	
62.66	269.00	40	4	44	90.9	
62.86	271.71	32	31	63	50.8	
62.91	272.38	19	13	32	59.4	
62.96	273.00	14	52	66	21.2	
63.01	273.71	3	117	120	2.5	
63.06	274.38	2	116	118	1.7	
63.11	275.00	1	150	151	0.7	
63.16	275.71	1	31	32	3.1	
63.21	276.38	0	5	5	0.0	
63.26	277.00	3	79	82	3.7	
63.31	277.71	0	91	91	0.0	
63.36	278.38	0	51	51	0.0	
63.41	279.00	1	105	106	0.9	
63.46	279.71	0	28	28	0.0	
63.66	282.29	1	48	49	2.0	
63.83	284.57	0	4	4	0.0	
64.03	287.25	5	196	201	2.5	
64.23	289.40	3	103	106	2.8	
64.43	291.27	3	0	3	100.0	
64.73	293.91	4	0	4	100.0	
64.93	295.50	0	0	0	0.0	
65.43	299.14	0	0	0	0.0	
66.03	303.13	0	1	1	0.0	
66.58	306.25	0	0	0	0.0	
67.28	309.35	1	2	3	33.3	
67.78	311.40	5	1	6	83.3	
68.2	313.04	1	0	1	100.0