# Partin et al. 2007 Northern Borneo Stalagmite Oxygen Isotope Data 
#----------------------------------------------------------------------- 
#                World Data Service for Paleoclimatology, Boulder 
#                                  and 
#                     NOAA Paleoclimatology Program 
#             National Centers for Environmental Information (NCEI)
#----------------------------------------------------------------------- 
# Template Version 4.0
# Encoding: UTF-8
# NOTE: Please cite original publication, NOAA Landing Page URL, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, study title, NOAA Landing Page URL, and date accessed. 
#
# Description/Documentation lines begin with #
# Data lines have no #
#
# NOAA_Landing_Page:  https://www.ncei.noaa.gov/access/paleo-search/study/5538
#   Landing_Page_Description: NOAA Landing Page of this file's parent study, which includes all study metadata.
#
# Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-cave-5538.json
#   Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata.
#
# Data_Type: Speleothems
#
# Dataset_DOI: 10.25921/vd61-pw29
#
# Science_Keywords: Last Glacial Maximum
#--------------------
# Resource_Links
#   
# Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/speleothem/pacific/gunung-buda2007-splice-noaa.txt
#   Data_Download_Description: NOAA Template File; Spliced SSC01, SCH02, and BA04 Isotope Data
#
#--------------------
# Contribution_Date
#   Date: 2011-06-01
#--------------------
# File_Last_Modified_Date
#   Date: 2025-01-31
#--------------------
# Title
#   Study_Name: Partin et al. 2007 Northern Borneo Stalagmite Oxygen Isotope Data 
#--------------------
# Investigators
#   Investigators: Partin, J.W.; Cobb, K.M.; Adkins, J.F.; Clark, B.; Fernandez, D.P.
#--------------------
# Description_Notes_and_Keywords
#   Description: Three stalagmite d18O records from Gunung Buda National Park, Northern Borneo, Malaysia (4º02'N, 114º48'E, elev. 150m), for the last 27ka. Samples SSC01 and SCH02 originate from Snail Shell Cave and formed ~250m from the cave entrance and ~20m from each other.  Sample BA04 formed >500m from the cave entrance in Bukit Assam Cave, which lies ~6km NNE from Snail Shell Cave. 
#
# The age model for each record is comprised of 24-26 U/Th Dates corrected using stalagmite specific 230Th/232Th (Suppl. Info in Partin et al., 2007; Adkins et al., 2007); breaks in the record are dated hiatuses. The average temporal resolution for each d18O record is 72, 56, and 60 yrs/sample for SCH02, SSC01, and BA04, respectively.  Rules for establishing the age models from U/Th dates, as well as known hiatuses, are provided below.  A "master d18O record" is constructed by splicing together portions of the three individual records. The master record is best used with error bars calculated from overlapping portions of all three stalagmites. For all records, d18O data are reported with respect to PDB, and ages are reported as years before present. Two rules were used for establishing the final age model: 1) For ages older than 11,000 years, individual age errors for a U-series point must be less than 2% (2s), 2) For ages younger than 11,000 years we only keep points with uncertainties of less than 400 years. Two additional rules used to pick dates: 1) Use only one point per isochron – that with the lowest error bar, 2) When there is overlap between two ages within error, take the age with the smallest error bar. 
#
# Rules for establishing length of a hiatus: After visually examining the stalagmites for indications of a hiatus, all potential bands were checked for missing years by extending the young part of the adjacent age constraints downward and the older age constraints upward. If there is a difference in predicted age at the visual band's depth that is larger than 400 years and the age difference is larger than the propagated uncertainty, we declare that band a hiatus. A hiatus' duration is taken to be the difference in age between the upper and lower age model constraints. 
#
# UPDATE: 6/2008 (substitute revised age model) Corregendum, Nature 4 June 2009: A recalibration of the Caltech 236U and 229Th spike has determined that the original spike value used for the stalagmite chronologies yielded U-Th ages that were too old by a margin of ~2-3%. U-Th ages and subsequent age models have been recalculated using the new spike value for all stalagmites. The new age models alter the absolute timing of certain events, but do not alter any major conclusions of the original manuscript. The highest d18O values (inferred driest conditions) now occur at 16.0 +/- 0.3 kyr ago. A late deglacial d18O plateau in the Borneo stalagmite records is now centered at 13.0 +/- 0.2 kyr ago. The lowest d18O values (inferred wettest conditions) now occur at 5.0 +/- 0.1 kyr ago. Examples of original and adjusted dates, respectively, at 5 kyr intervals are as follows: 5280 versus 5141 (SSC01); 10581 versus 10293 (SSC01); 15673 versus 15231 (BA04); 20937 versus 20322 (BA04); and 26387 versus 25602 (SCH02).
#
# UPDATE: 6/16/2011 (add spliced record)
#
# LAST UPDATE: 8/4/2022 (updated spliced "master" record added) ** Both original citations Partin et al. 2007 (doi:10.1038/nature06164) and Buckingham et al. 2022 (doi:10.1029/2021GL096937) should be cited when using this updated spliced record! ** Notes for updated spliced "master" record: Spliced master record updated to include Mulu Secret Chamber stalagmite SC02 d18O, published in Buckingham et al., 2022 (doi:10.1029/2021GL096937). SC02 replaces SCH02 at the end of the deglaciation (12-15ka) in this updated spliced record as SC02 has the most reliable age model during that time period (see Buckingham et al., 2022). SC02 d18O values have been adjusted by +0.2 permil for the splice record, following the methods of Carolin et al., 2016 (doi:10.1016/j.epsl.2016.01.028).
#--------------------
# Publication 
#   Authors: Partin, J.W., K.M. Cobb, J.F. Adkins, B. Clark, and D.P. Fernandez
#   Published_Date_or_Year: 2007-03-01
#   Published_Title: Millennial-scale trends in west Pacific warm pool hydrology since the Last Glacial Maximum
#   Journal_Name: Nature
#   Volume: 449
#   Edition: 
#   Issue: 7161
#   Pages: 452-455
#   Report_Number: 
#   DOI: 10.1038/nature06164
#   Online_Resource: 
#   Full_Citation:
#   Abstract: Models and palaeoclimate data suggest that the tropical Pacific climate system plays a key part in the mechanisms underlying orbital-scale and abrupt climate change. Atmospheric convection over the western tropical Pacific is a major source of heat and moisture to extratropical regions, and may therefore influence the global climate response to a variety of forcing factors. The response of tropical Pacific convection to changes in global climate boundary conditions, abrupt climate changes and radiative forcing remains uncertain, however. Here we present three absolutely-dated oxygen isotope records from stalagmites in northern Borneo that reflect changes in west Pacific warm pool hydrology over the past 27,000 years. Our results suggest that convection over the western tropical Pacific weakened 18,000-20,000 years ago, as tropical Pacific and Antarctic temperatures began to rise during the early stages of deglaciation. Convective activity, as inferred from oxygen isotopes, reached a minimum during Heinrich event 1, when the Atlantic meridional overturning circulation was weak, pointing to feedbacks between the strength of the overturning circulation and tropical Pacific hydrology. There is no evidence of the Younger Dryas event in the stalagmite records, however, suggesting that different mechanisms operated during these two abrupt deglacial climate events. During the Holocene epoch, convective activity appears to track changes in spring and autumn insolation, highlighting the sensitivity of tropical Pacific convection to external radiative forcing. Together, these findings demonstrate that the tropical Pacific hydrological cycle is sensitive to high-latitude climate processes in both hemispheres, as well as to external radiative forcing, and that it may have a central role in abrupt climate change events.
#--------------------
# Publication 
#   Authors: Buckingham, F.; Carolin, S.A.; Partin, J.W.; Adkins, J.F.; Cobb, K.M.; Day, C.C.; Ding, Q.; He, C.; Liu, Z.; Otto-Bliesner, B.; Roberts, W.H.G.; Lejau, S.; Malang, J.
#   Published_Date_or_Year: 2022-03-16
#   Published_Title: Termination 1 Millennial-scale Rainfall Events over the Sunda Shelf
#   Journal_Name: Geophysical Research Letters
#   Volume: 49
#   Edition: 
#   Issue: 5
#   Pages: 
#   Report_Number: e2021GL096937
#   DOI: 10.1029/2021GL096937
#   Online_Resource: 
#   Full_Citation:
#   Abstract: Recent paleoclimate reconstructions have suggested millennial-scale variability in the Indo-Pacific Warm Pool region coincident with events of the last deglaciation. Here we present a new stalagmite oxygen isotope record from northern Borneo, which today is located near the center of the region’s mean annual inter-tropical convergence zone. The record spans the full deglaciation, and reveals for the first time distinct oxygen isotope variations at this location connected with the Bølling-Allerød onset and the Younger Dryas event. The full deglaciation in the Borneo stalagmite proxy reconstruction appears remarkably similar to a 20-11 ka transient simulation of rainfall over the area produced using the isotope-enabled Community Earth System Model. In this model, periods of weakened Atlantic Ocean meridional overturning circulation are associated with an anomalous Western North Pacific anticyclone, which is produced in boreal autumn and shifts south over Borneo during boreal winter, causing dry conditions.
#--------------------
# Funding_Agency 
#   Funding_Agency_Name: US National Science Foundation
#   Grant: 
#--------------------
# Funding_Agency 
#   Funding_Agency_Name: Comer Abrupt Climate Change Fellowship
#   Grant: 
#--------------------
# Site_Information 
#   Site_Name: Gunung Buda National Park
#   Location: Malaysia
#   Northernmost_Latitude: 4.03
#   Southernmost_Latitude: 4.03
#   Easternmost_Longitude: 114.8
#   Westernmost_Longitude: 114.8
#   Elevation_m: 150
#--------------------
# Data_Collection  
#   Collection_Name: Gunung Splice
#   First_Year: 26420
#   Last_Year: 0
#   Time_Unit: cal yr BP
#   Core_Length_m: 
#   Parameter_Keywords: 
#   Notes: Spliced "master" record added 6/16/2011: SSC01 was chosen as the basis for the majority of the spliced record as it is the most continuous dataset. SCH02 was used during the end of the deglaciation (12-15ka) as it is the most continuous during that time period and for the end of the record where dating measurements are more frequent (23-26ka). Sample BA04 was used to fill in portions from 15-20ka and 24-27ka, where SSC01 has gaps in the record (note that BA04 data have been offset by -0.4permil prior to splicing). 
#--------------------
# Chronology_Information
#   Chronology: 
#--------------------
# Variables  
#
# PaST_Thesaurus_Download_Resource:  https://www.ncei.noaa.gov/pub/data/paleo/PaST-thesaurus/SKOS/past-thesaurus-v1.0.rdf
#   PaST_Thesaurus_Download_Description: Paleoenvironmental Standard Terms (PaST) Thesaurus terms, definitions, and relationships in SKOS format.
#
# Data variables follow that are preceded by "##" in columns one and two.
# Variables list, one per line, shortname-tab-var components: what, material, error, units, seasonality, data type, detail, method, C or N for Character or Numeric data)
#
## core_id	sample identification,,,,,speleothems,,,C,stalagmite name
## age_calBP	age,,,calendar year before present,,speleothems,,,N,updated age model
## d18O	delta 18O,calcium carbonate,,per mil VPDB,,speleothems,raw,isotope ratio mass spectrometry,N,
#
#--------------------
# Data:
# Data lines follow (have no #)
# Data line format - tab-delimited text, variable short name as header
# Missing_Values:
core_id	age_calBP	d18O
SSC01	0	-9.16
SSC01	65	-9.29
SSC01	130	-9.38
SSC01	195	-9.54
SSC01	260	-9.46
SSC01	325	-9.48
SSC01	390	-9.50
SSC01	455	-9.28
SSC01	520	-9.38
SSC01	582	-9.52
SSC01	622	-9.61
SSC01	662	-9.51
SSC01	703	-9.47
SSC01	743	-9.51
SSC01	783	-9.54
SSC01	823	-9.64
SSC01	863	-9.53
SSC01	903	-9.33
SSC01	943	-9.60
SSC01	983	-9.44
SSC01	1023	-9.37
SSC01	1064	-9.59
SSC01	1104	-9.79
SSC01	1144	-9.77
SSC01	1184	-9.49
SSC01	1224	-9.42
SSC01	1264	-9.60
SSC01	1304	-9.51
SSC01	1344	-9.50
SSC01	1384	-9.64
SSC01	1424	-9.55
SSC01	1465	-9.45
SSC01	1505	-9.58
SSC01	1545	-9.54
SSC01	1585	-9.54
SSC01	1625	-9.51
SSC01	1665	-9.40
SSC01	1705	-9.67
SSC01	1745	-9.25
SSC01	1785	-9.48
SSC01	1826	-9.93
SSC01	1866	-9.68
SSC01	1906	-9.51
SSC01	1946	-9.88
SSC01	1986	-9.53
SSC01	2026	-9.40
SSC01	2066	-9.48
SSC01	2106	-9.44
SSC01	2146	-9.87
SCH02	2332	-10.03
SCH02	2591	-9.43
SCH02	2699	-9.28
SCH02	2790	-9.27
SCH02	2882	-9.54
SCH02	2973	-9.33
SCH02	3064	-9.51
SCH02	3155	-9.62
SCH02	3247	-9.66
SCH02	3338	-9.51
SCH02	3429	-9.67
SCH02	3520	-9.48
SCH02	3611	-9.71
SCH02	3664	-10.06
SCH02	3707	-10.17
SCH02	3750	-9.83
SCH02	3793	-9.73
SCH02	3836	-9.72
SCH02	3879	-9.71
SCH02	3922	-10.19
SCH02	3965	-9.90
SCH02	4008	-9.78
SSC01	4037	-10.17
SSC01	4067	-10.13
SSC01	4096	-10.15
SSC01	4125	-10.05
SSC01	4155	-9.97
SSC01	4184	-9.86
SSC01	4213	-9.90
SSC01	4243	-9.79
SSC01	4272	-9.93
SSC01	4302	-9.98
SSC01	4331	-10.19
SSC01	4360	-9.76
SSC01	4390	-9.97
SSC01	4419	-10.03
SSC01	4448	-10.09
SSC01	4478	-9.82
SSC01	4507	-9.91
SSC01	4537	-9.84
SSC01	4566	-10.00
SSC01	4595	-10.06
SSC01	4625	-10.09
SSC01	4654	-10.07
SSC01	4683	-9.99
SSC01	4713	-10.01
SSC01	4742	-9.96
SSC01	4772	-9.94
SSC01	4801	-10.07
SSC01	4830	-9.95
SSC01	4860	-10.04
SSC01	4889	-9.88
SSC01	4918	-9.92
SSC01	4948	-10.06
SSC01	4977	-10.12
SSC01	5006	-10.21
SSC01	5036	-10.06
SSC01	5065	-9.96
SSC01	5095	-9.79
SSC01	5124	-9.99
SSC01	5164	-9.69
SSC01	5219	-9.77
SSC01	5274	-9.72
SSC01	5329	-9.81
SSC01	5384	-9.70
SSC01	5439	-9.72
SSC01	5493	-9.76
SSC01	5548	-9.89
SSC01	5603	-9.65
SSC01	5658	-9.74
SSC01	5713	-9.78
SSC01	5768	-9.82
SSC01	5823	-9.79
SSC01	5878	-9.65
SSC01	5933	-9.72
SSC01	5988	-9.64
SSC01	6043	-9.66
SSC01	6098	-9.60
SSC01	6153	-9.41
SSC01	6208	-9.36
SSC01	6263	-9.73
SSC01	6318	-9.95
SSC01	6373	-9.64
SSC01	6428	-9.40
SSC01	6482	-9.63
SSC01	6534	-9.84
SSC01	6585	-9.84
SSC01	6636	-9.38
SSC01	6688	-9.50
SSC01	6739	-9.39
SSC01	6790	-9.34
SSC01	6842	-9.25
SSC01	6893	-9.18
SSC01	6944	-9.27
SSC01	6995	-9.39
SSC01	7047	-9.49
SSC01	7098	-9.17
SSC01	7149	-9.08
SSC01	7201	-9.12
SSC01	7252	-9.07
SSC01	7303	-9.19
SSC01	7355	-9.53
SSC01	7406	-9.56
SSC01	7457	-9.52
SSC01	7509	-9.23
BA04	7514	-9.24
BA04	7553	-9.26
BA04	7593	-9.13
BA04	7633	-9.30
BA04	7673	-9.16
BA04	7712	-9.23
SSC01	7745	-9.76
SSC01	7796	-9.12
SSC01	7847	-9.24
SSC01	7898	-9.01
SSC01	7950	-9.11
SSC01	8001	-8.74
SSC01	8052	-8.92
SSC01	8104	-9.15
SSC01	8155	-8.95
SSC01	8206	-8.79
SSC01	8258	-9.00
SSC01	8309	-9.11
SSC01	8360	-9.06
SSC01	8412	-8.83
SSC01	8463	-8.91
SSC01	8514	-8.91
SSC01	8553	-8.86
SSC01	8592	-9.05
SSC01	8631	-8.73
SSC01	8670	-8.70
SSC01	8709	-8.73
SSC01	8748	-8.74
SSC01	8787	-8.69
SSC01	8826	-8.79
SSC01	8865	-8.79
SSC01	8904	-8.93
SSC01	8943	-8.90
SSC01	8982	-9.17
SSC01	9022	-8.91
SSC01	9061	-9.13
SSC01	9100	-8.85
SSC01	9139	-8.75
SSC01	9178	-8.69
SSC01	9217	-8.83
SSC01	9256	-8.95
SSC01	9295	-8.82
SSC01	9334	-8.49
SSC01	9373	-8.45
SSC01	9412	-9.01
SSC01	9451	-8.72
SSC01	9486	-8.65
SSC01	9517	-8.59
SSC01	9548	-8.69
SSC01	9579	-8.66
SSC01	9611	-8.59
SSC01	9642	-8.61
SSC01	9673	-8.67
SSC01	9704	-8.72
SSC01	9735	-8.68
SSC01	9767	-8.80
SSC01	9798	-8.62
SSC01	9829	-8.56
SSC01	9860	-8.57
SSC01	9892	-8.46
SSC01	9923	-8.56
SSC01	9954	-8.37
SSC01	9985	-8.25
SSC01	10017	-8.10
SSC01	10048	-8.45
SSC01	10079	-8.55
SSC01	10110	-8.43
SSC01	10141	-8.48
SSC01	10173	-8.43
SSC01	10204	-8.39
SSC01	10235	-8.71
SSC01	10266	-8.62
SSC01	10305	-8.41
SSC01	10384	-8.51
SSC01	10464	-8.37
SSC01	10544	-8.60
SSC01	10623	-8.34
SSC01	10703	-8.44
SSC01	10782	-8.14
SSC01	10862	-8.01
SSC01	10941	-8.00
SSC01	11021	-8.34
SSC01	11100	-8.46
SSC01	11180	-8.34
SSC01	11260	-8.18
SSC01	11339	-8.33
SSC01	11419	-8.22
SSC01	11498	-8.32
SSC01	11578	-8.33
SSC01	11657	-8.15
SSC01	11737	-8.02
SCH02	11743	-8.49
SCH02	11789	-8.48
SCH02	11836	-8.61
SCH02	11882	-8.48
SCH02	11928	-8.09
SCH02	11974	-8.24
SCH02	12020	-8.21
SCH02	12066	-8.16
SCH02	12112	-8.21
SCH02	12158	-8.14
SCH02	12204	-8.16
SCH02	12251	-7.92
SCH02	12297	-8.16
SCH02	12343	-7.79
SCH02	12389	-7.66
SCH02	12435	-7.46
SCH02	12481	-7.51
SCH02	12527	-7.65
SCH02	12573	-7.90
SCH02	12635	-7.55
SCH02	12712	-7.72
SCH02	12789	-7.82
SCH02	12866	-7.85
SCH02	12943	-7.51
SCH02	13020	-7.74
SCH02	13085	-7.64
SCH02	13150	-7.38
SCH02	13215	-7.67
SCH02	13281	-7.70
SCH02	13346	-8.07
SCH02	13411	-7.80
SCH02	13453	-7.92
SCH02	13480	-8.02
SCH02	13508	-8.05
SCH02	13535	-8.02
SCH02	13562	-7.98
SCH02	13590	-7.81
SCH02	13617	-8.02
SCH02	13644	-8.16
SCH02	13672	-8.12
SCH02	13699	-8.14
SCH02	13726	-7.99
SCH02	13753	-7.50
SCH02	13808	-7.47
SCH02	13869	-7.99
SCH02	13930	-7.97
SCH02	13991	-7.76
SCH02	14052	-7.97
SCH02	14114	-7.86
SCH02	14175	-8.11
SCH02	14236	-7.79
SCH02	14297	-7.61
SCH02	14358	-7.90
SCH02	14419	-7.84
SCH02	14480	-7.50
SCH02	14541	-7.88
SCH02	14594	-7.50
SCH02	14646	-7.48
SCH02	14699	-7.39
SCH02	14752	-7.12
SCH02	14805	-7.40
SCH02	14858	-7.24
SCH02	14911	-7.14
BA04	14960	-7.13
BA04	14990	-7.15
BA04	15020	-7.05
BA04	15050	-7.09
BA04	15080	-7.10
BA04	15110	-6.92
BA04	15140	-6.87
BA04	15170	-6.87
BA04	15201	-6.78
BA04	15231	-6.76
BA04	15261	-6.77
BA04	15291	-6.64
BA04	15321	-6.77
BA04	15351	-6.89
BA04	15381	-6.93
BA04	15411	-6.65
BA04	15441	-6.79
BA04	15471	-6.85
BA04	15501	-6.87
BA04	15531	-6.80
BA04	15561	-6.71
BA04	15592	-6.91
BA04	15622	-6.78
BA04	15652	-6.59
BA04	15682	-6.72
BA04	15712	-6.61
BA04	15742	-6.60
BA04	15772	-6.48
BA04	15802	-6.75
BA04	15832	-6.83
BA04	15862	-6.91
BA04	15892	-6.94
BA04	15922	-6.97
BA04	15982	-6.86
BA04	16072	-6.82
BA04	16161	-6.83
BA04	16251	-7.10
BA04	16340	-7.16
BA04	16430	-7.14
BA04	16519	-7.08
BA04	16609	-7.05
BA04	16698	-7.13
BA04	16788	-7.15
BA04	16877	-7.10
BA04	16967	-7.04
BA04	17056	-7.16
BA04	17146	-7.21
BA04	17235	-7.21
BA04	17325	-7.36
BA04	17414	-7.19
BA04	17492	-7.26
BA04	17541	-7.36
BA04	17590	-7.26
BA04	17639	-7.28
BA04	17688	-7.34
BA04	17737	-7.39
BA04	17786	-7.55
BA04	17836	-7.57
BA04	17885	-7.59
BA04	17934	-7.65
BA04	17983	-7.87
BA04	18032	-7.65
BA04	18081	-7.50
BA04	18130	-7.44
BA04	18179	-7.42
BA04	18228	-7.45
BA04	18277	-7.47
BA04	18327	-7.51
BA04	18376	-7.50
BA04	18425	-7.58
BA04	18474	-7.60
BA04	18523	-7.59
BA04	18572	-7.47
BA04	18621	-7.62
BA04	18670	-7.66
BA04	18719	-7.47
BA04	18768	-7.55
BA04	18818	-7.52
BA04	18867	-7.46
BA04	18916	-7.47
BA04	18965	-7.55
BA04	19014	-7.61
BA04	19063	-7.68
BA04	19112	-7.69
BA04	19161	-7.65
BA04	19210	-7.61
BA04	19259	-7.60
BA04	19309	-7.63
BA04	19358	-7.63
BA04	19407	-7.99
BA04	19456	-7.76
SSC01	19518	-7.68
SSC01	19598	-7.78
SSC01	19677	-7.87
SSC01	19757	-7.81
SSC01	19837	-7.76
SSC01	19916	-7.74
SSC01	19996	-7.72
SSC01	20076	-7.76
SSC01	20156	-7.61
SSC01	20235	-7.94
SSC01	20315	-7.85
SSC01	20395	-7.96
SSC01	20474	-7.65
SSC01	20554	-7.74
SSC01	20634	-7.85
SSC01	20714	-7.88
SSC01	20793	-7.58
SSC01	20873	-7.67
SSC01	20953	-7.53
SSC01	21032	-7.58
SSC01	21112	-7.78
SSC01	21192	-7.44
SSC01	21272	-7.60
SSC01	21351	-7.79
SSC01	21431	-7.63
SSC01	21510	-7.90
SSC01	21586	-7.64
SSC01	21661	-7.44
SSC01	21736	-7.32
SSC01	21812	-7.43
SSC01	21887	-7.64
SSC01	21963	-7.64
SSC01	22038	-7.66
SSC01	22113	-7.65
SSC01	22189	-7.55
SSC01	22264	-7.65
SSC01	22340	-7.81
SSC01	22415	-7.86
SSC01	22490	-7.80
SSC01	22566	-7.75
SSC01	22641	-7.67
SSC01	22717	-7.66
SSC01	22792	-7.67
SSC01	22868	-7.74
SSC01	22943	-7.78
SSC01	23018	-7.66
SSC01	23094	-7.77
SSC01	23169	-7.77
SSC01	23245	-7.67
SSC01	23320	-7.73
SSC01	23395	-7.85
SCH02	23417	-7.93
SCH02	23417	-7.93
SCH02	23514	-7.82
SCH02	23610	-7.74
SCH02	23706	-7.83
SCH02	23803	-7.79
SCH02	23899	-7.88
SCH02	23995	-7.87
SCH02	24092	-7.94
SCH02	24188	-7.80
SCH02	24289	-8.02
SCH02	24430	-7.89
SCH02	24571	-7.94
SCH02	24712	-7.78
SCH02	24853	-7.80
SCH02	24995	-7.67
SCH02	25136	-7.40
SCH02	25277	-7.51
SCH02	25418	-7.51
SCH02	25559	-7.79
SCH02	25674	-7.81
SCH02	25777	-8.03
SCH02	25880	-7.86
SCH02	25983	-8.03
SCH02	26086	-8.27
SCH02	26150	-8.19
SCH02	26174	-8.02
SCH02	26199	-8.03
SCH02	26248	-7.98
SCH02	26273	-7.98
SCH02	26297	-8.27
SCH02	26322	-8.20
SCH02	26347	-7.71
SCH02	26371	-7.87
SCH02	26396	-8.01
SCH02	26420	-7.89
SCH02	26420	-7.89