# Haozhu Cave, China 10-30 ka Stalagmite Oxygen Isotope Data
#----------------------------------------------------------------------- 
#                World Data Service for Paleoclimatology, Boulder 
#                                  and 
#                     NOAA Paleoclimatology Program 
#             National Centers for Environmental Information (NCEI)
#----------------------------------------------------------------------- 
# Template Version 3.0
# Encoding: UTF-8
# NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. 
# If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. 
#
# Online_Resource: https://www.ncdc.noaa.gov/paleo/study/26873 
#       Description: NOAA Landing Page
# Online_Resource: https://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/asia/china/haozhu2016d18o.txt
#       Description: NOAA location of the template
#
# Original_Source_URL:  
#       Description:
# 
# Description/Documentation lines begin with #
# Data lines have no #
#
# Archive: Speleothems
#
# Dataset DOI: 
#
# Parameter_Keywords: oxygen isotopes
#---------------------------------------
# Contribution_Date
#    Date: 2019-05-21
#---------------------------------------
# File_Last_Modified_Date
#    Date: 2019-05-21
#---------------------------------------
# Title
#    Study_Name: Haozhu Cave, China 10-30 ka Stalagmite Oxygen Isotope Data
#---------------------------------------
# Investigators
#      Investigators: Zhang, H.; Griffiths, M.L.
#---------------------------------------
# Description_Notes_and_Keywords
#        Description: Speleothem oxygen isotope (d18O) data from Haozhu Cave, central China during last deglaciation.
#         Provided Keywords: Heinrich Stadial 1, last deglaciation
#---------------------------------------
# Publication
# Authors: Hongbin Zhang, Michael L. Griffiths, Junhua Huang, Yanjun Cai, Canfa Wang, Fan Zhang, Hai Cheng, Youfeng Ning, Chaoyong Hu, Shucheng Xie
# Published_Date_or_Year: 2016-11-01
# Published_Title: Antarctic link with East Asian summer monsoon variability during the Heinrich Stadial-Bolling interstadial transition
# Journal_Name: Earth and Planetary Science Letters
# Volume: 453
# Edition: 
# Issue: 
# Pages: 243-251
# Report Number: 
# DOI: 10.1016/j.epsl.2016.08.008
# Online_Resource: https://www.sciencedirect.com/science/article/pii/S0012821X16304289 
# Full_Citation: 
# Abstract: Previous research has shown a strong persistence for direct teleconnections between the East Asian summer monsoon (EASM) and high northern latitude climate variability during the last glacial and deglaciation, in particular between monsoon weakening and a reduced Atlantic meridional overturning circulation (AMOC). However, less attention has been paid to EASM strengthening as the AMOC was reinvigorated following peak Northern Hemisphere (NH) cooling. Moreover, climate model simulations have suggested a strong role for Antarctic meltwater discharge in modulating northward heat transport and hence NH warming, yet the degree to which Southern Hemisphere (SH) climate anomalies impacted the Asian monsoon region is still unclear.
# Here we present a new stalagmite oxygen-isotope record from the EASM affected region of central China, which documents two prominent stages of increased 18O-depleted moisture delivery to the region through the transition from Heinrich Stadial 1 (HS1) to the Bølling-Allerod (B-A) interstadial; this is in general agreement with the other monsoonal records from both NH and SH mid to low latitudes. Through novel comparisons with a recent iceberg-rafted debris (IRD) record from the Southern Ocean, we propose that the two-stage EASM intensification observed in our speleothem records were linked with two massive Antarctic icesheet discharge (AID) events at ~16.0 ka and ~14.7 ka, immediately following the peak HS1 stadial event. Notably, the large increase in EASM intensity at the beginning of the HS1/B-A transition (~16 ka) is relatively muted in the NH higher latitudes, and better aligns with the changes observed in the SH, indicating the Antarctic and Southern Ocean perturbations could have an active role in driving the initial EASM strengthening at this time. Indeed, Antarctic freshwater input to the Southern Ocean during these AID events would have cooled the surrounding surface waters and caused an expansion of sea ice, restricting the southern extent of the SH westerlies. Moreover, increased meltwater flux during IRD events would have freshened Antarctic Intermediate Water, leading to the increased formation of North Atlantic Deep Water and enhanced North Atlantic subsurface heat release, and causing a strengthening of the AMOC during the HS1-Bolling transition. The result of this sequence-of-events would have been warming in the North Atlantic whilst at the same time cooling in the Antarctic. The ensuing interhemispheric temperature gradient would have acted to push the ITCZ northward, weakening the Australian-Indonesian summer monsoon (AISM) whilst intensifying the EASM.
#---------------------------------------
# Funding_Agency
#    Funding_Agency_Name: National Science Foundation of China
#    Grant: 41130207
#---------------------------------------
# Funding_Agency
#    Funding_Agency_Name: Key R&D Project of Ministry of Science and Technology
#    Grant: 2016YFA0601100
#---------------------------------------
# Funding_Agency
#    Funding_Agency_Name: 111 Program
#    Grant: B08030
#---------------------------------------
# Site Information
# Site_Name: Haozhu Cave
# Location: Asia>Eastern Asia>China
# Country: China
# Northernmost_Latitude: 30.6833
# Southernmost_Latitude: 30.6833
# Easternmost_Longitude: 109.9833
# Westernmost_Longitude: 109.9833
# Elevation: 950m
#---------------------------------------
# Data_Collection
#   Collection_Name: Haozhu2016d18O
#   First_Year: 30433
#   Last_Year: 8558
#   Time_Unit: cal yr BP
#   Core_Length: 
#   Notes: 
#---------------------------------------
# Chronology_Information 
# Chronology: 
# 
# 230Th dating results.  The error is 2s error.	
# Sample 	Depth	238U 		232Th		230Th / 232Th		d234U*		230Th / 238U		230Th Age (yr)		230Th Age (yr)		d234UInitial**		230Th Age (yr BP)	
# Number	(mm)	(ppb)		(ppt)		(atomic x10-6)		(measured)		(activity)		(uncorrected)		(corrected)		(corrected)		(corrected )	
# HZZ11-1	191	150	±0.1	449	±9	1058 	±22	1334.8	±2.0	0.1917 	±0.0008	9270	±43	9234	±50	1370 	±2	9170	±50
# HZZ11-2	165	101	±0.1	3785	±76	97 	±2	1327.6	±2.7	0.2220 	±0.0020	10833	±102	10370	±343	1367 	±3	10306	±343
# HZZ11-3	143	121.2	±0.1	641	±13	724 	±15	1322.1	±2.1	0.2324 	±0.0009	11390	±46	11325	±65	1365 	±2	11261	±65
# HZZ11-4	129	125.3	±0.1	4382	±88	120 	±2	1305.5	±2.2	0.2550 	±0.0013	12649	±69	12215	±314	1351 	±3	12151	±314
# HZZ11-5	120	130.6	±0.1	1624	±33	346 	±7	1307.3	±1.9	0.2608 	±0.0009	12939	±47	12785	±118	1355 	±2	12721	±118
# HZZ11-6	113	130.3	±0.1	2005	±40	283 	±6	1303.2	±2.2	0.2640 	±0.0014	13128	±72	12937	±153	1352 	±2	12873	±153
# HZZ11-7	95	138.8	±0.1	2760	±55	240 	±5	1293.7	±1.9	0.2890 	±0.0008	14506	±45	14259	±180	1347 	±2	14195	±180
# HZZ11-8	93	148.4	±0.1	5481	±110	133 	±3	1284.9	±2.3	0.2974 	±0.0012	15013	±66	14553	±332	1339 	±3	14489	±332
# HZZ11-9	87	131.4	±0.1	9574	±192	72 	±1	1279.9	±2.2	0.3165 	±0.0015	16076	±85	15166	±650	1336 	±3	15102	±650
# HZZ11-10	79	107.3	±0.1	651	±13	831 	±17	1275.4	±2.3	0.3061 	±0.0011	15550	±62	15474	±82	1332 	±2	15410	±82
# HZZ11-11	70	164.4	±0.2	1557	±31	561 	±11	1262.8	±2.1	0.3223 	±0.0007	16527	±41	16408	±93	1323 	±2	16344	±93
# HZZ11-12	63	88.8	±0.1	757	±15	640 	±13	1256.2	±2.6	0.3311 	±0.0014	17060	±82	16953	±112	1318 	±3	16889	±112
# HZZ11-13	54	101.0	±0.1	203	±4	2923 	±63	1242.6	±2.1	0.3570 	±0.0013	18614	±74	18588	±76	1310 	±2	18524	±76
# HZZ11-14	44	105.8	±0.1	134	±4	5110 	±137	1225.3	±2.5	0.3933 	±0.0018	20840	±107	20824	±108	1299 	±3	20760	±108
# HZZ11-15	30	129.1	±0.1	395	±8	2308 	±47	1216.6	±2.0	0.4281 	±0.0010	22950	±64	22912	±70	1298 	±2	22848	±70
# HZZ11-16	1	105.6	±0.1	1362	±27	702 	±14	1172.6	±2.3	0.5490 	±0.0016	30933	±107	30768	±158	1279 	±3	30704	±158
# HZZ27-1	254	129	±0.1	4368	±88	100 	±2	1252.7	±2.3	0.2057	±0.0009	10353	±47	9922	±308	1288 	±3	9858	±308
# HZZ27-2	213	218	±0.3	1631	±33	511 	±10	1249.0	±2.1	0.2319	±0.0006	11753	±36	11658	±76	1291 	±2	11594	±76
# HZZ27-3	211	149	±0.2	2986	±60	195 	±4	1246.8	±2.6	0.2369	±0.0007	12029	±39	11775	±184	1289 	±3	11710	±184
# HZZ27-4	200	161	±0.2	1545	±31	457 	±9	1228.2	±2.3	0.2656	±0.0007	13688	±42	13565	±96	1276 	±2	13501	±96
# HZZ27-5	181	197	±0.2	1274	±26	705 	±14	1223.1	±2.4	0.2759	±0.0006	14279	±37	14197	±69	1273 	±2	14132	±69
# HZZ27-6	169	160	±0.2	418	±8	1811 	±37	1217.8	±2.3	0.2871	±0.0008	14932	±47	14898	±53	1270 	±2	14834	±53
# HZZ27-7	157	158	±0.2	186	±4	4216 	±88	1205.6	±2.4	0.3009	±0.0007	15790	±43	15774	±44	1260 	±3	15709	±44
# HZZ27-8	126	131	±0.1	250	±5	3218 	±67	1142.5	±2.0	0.3712	±0.0009	20406	±58	20381	±61	1210 	±2	20317	±61
# HZZ27-9	107	152	±0.2	1295	±26	1406	±28	1013.8	±1.8	0.7284	0.0015 	47031	±129	46916	±152	1157	±2	46852	±152
# HZZ27-10	92	164	±0.2	34	±1	60468	±2089	1054.4	±2.3	0.7549	0.0013 	47902	±117	47899	±117	1207	±3	47834	±117
# HZZ27-11	43	144	±0.2	83	±2	23431	±564	1116.9	±2.4	0.825798441	0.0015 	51456	±134	51448	±135	1291.5	±3	51383	±135
# HZZ27-12	13	123	±0.1	174	±4	9945	±213	1145.7	±2.0	0.8545	0.0016 	52749	±139	52731	±140	1330	±2	52667	±140
# 
# U decay constants: l238 = 1.55125x10-10 (Jaffey et al., 1971) and l234 = 2.82206x10-6 (Cheng et al., 2013). Th decay constant:  l230 = 9.1705x10-6 (Cheng et al., 2013).
# * d234U = ([234U/238U]activity – 1)x1000.  
# ** d234Uinitial was calculated based on 230Th age (T), i.e., d234Uinitial = d234Umeasured x el234xT. 
# Corrected 230Th ages assume the initial 230Th/232Th atomic ratio of 4.4  ±2.2 x10-6.   Those are the values for a material at secular 
# equilibrium, with the bulk earth 232Th/238U value of 3.8.  The errors are arbitrarily assumed to be 50%.
# *** B.P. stands for "Before Present" where the "Present" is defined as the year 1950 A.D.
# 
#---------------------------------------
# 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)
#
## core	core name,,,,,,,,C,
## depth	depth,,,millimeter,,,,,N,
## age	age,,,calendar year before present,,,,,N,
## d18O	delta 18O,calcium carbonate,,per mil VPDB,,speleothems,raw,dual-inlet isotope ratio mass spectrometry,N,
#
#------------------------
# Data
# Data lines follow (have no #)
# Data line format - tab-delimited text, variable short name as header
# Missing Value: 
core	depth	age	d18O
HZZ-11	205.00	8558	-9.36
HZZ-11	204.00	8602	-9.53
HZZ-11	203.00	8645	-9.79
HZZ-11	202.00	8689	-9.85
HZZ-11	201.00	8733	-9.78
HZZ-11	200.00	8776	-9.51
HZZ-11	199.00	8820	-9.74
HZZ-11	198.00	8864	-9.34
HZZ-11	197.00	8907	-9.93
HZZ-11	196.00	8951	-9.95
HZZ-11	195.00	8995	-9.7
HZZ-11	194.00	9039	-9.77
HZZ-11	193.00	9082	-9.7
HZZ-11	192.00	9126	-9.62
HZZ-11	191.00	9170	-9.38
HZZ-11	190.00	9213	-9.83
HZZ-11	189.00	9257	-9.99
HZZ-11	188.00	9301	-9.9
HZZ-11	187.00	9344	-9.8
HZZ-11	186.00	9388	-9.57
HZZ-11	185.00	9432	-9.48
HZZ-11	184.00	9476	-9.55
HZZ-11	183.00	9519	-9.73
HZZ-11	182.00	9563	-9.84
HZZ-11	181.00	9607	-10.1
HZZ-11	180.00	9650	-9.75
HZZ-11	179.00	9694	-9.75
HZZ-11	178.00	9738	-9.57
HZZ-11	177.00	9781	-9.62
HZZ-11	176.00	9825	-9.63
HZZ-11	175.00	9869	-9.89
HZZ-11	174.00	9913	-9.59
HZZ-11	173.00	9956	-9.74
HZZ-11	172.00	10000	-9.41
HZZ-11	171.00	10044	-9.59
HZZ-11	170.00	10087	-9.77
HZZ-11	169.00	10131	-9.95
HZZ-11	168.00	10175	-9.61
HZZ-11	167.00	10219	-9.33
HZZ-11	166.00	10262	-9.35
HZZ-11	165.00	10306	-9.41
HZZ-11	164.00	10349	-9.76
HZZ-11	163.00	10393	-9.93
HZZ-11	162.00	10436	-9
HZZ-11	161.00	10480	-9.33
HZZ-11	160.00	10523	-9.33
HZZ-11	159.00	10566	-9.41
HZZ-11	158.00	10610	-9.06
HZZ-11	157.00	10653	-9.04
HZZ-11	156.00	10697	-9
HZZ-11	155.00	10740	-9.09
HZZ-11	154.00	10784	-9.19
HZZ-11	153.00	10827	-9.1
HZZ-11	152.00	10870	-9.12
HZZ-11	151.00	10914	-9.09
HZZ-11	150.00	10957	-8.98
HZZ-11	149.00	11001	-9.11
HZZ-11	148.00	11044	-9.46
HZZ-11	147.00	11088	-9.18
HZZ-11	146.00	11131	-9.04
HZZ-11	145.00	11174	-9.09
HZZ-11	144.00	11218	-8.88
HZZ-11	143.00	11261	-8.8
HZZ-11	142.00	11325	-8.48
HZZ-11	141.00	11388	-8.39
HZZ-11	140.00	11452	-8.75
HZZ-11	139.00	11515	-8.42
HZZ-11	138.00	11579	-8.18
HZZ-11	137.00	11643	-7.89
HZZ-11	136.00	11706	-7.56
HZZ-11	135.00	11770	-7.76
HZZ-11	134.00	11833	-7.61
HZZ-11	133.00	11897	-7.53
HZZ-11	132.00	11960	-7.91
HZZ-11	131.00	12024	-7.83
HZZ-11	130.00	12087	-7.78
HZZ-11	129.00	12151	-7.5
HZZ-11	128.00	12214	-7.65
HZZ-11	127.00	12278	-7.58
HZZ-11	126.00	12341	-7.6
HZZ-11	125.00	12404	-7.79
HZZ-11	124.00	12468	-7.67
HZZ-11	123.00	12531	-8.11
HZZ-11	122.00	12594	-7.99
HZZ-11	121.00	12658	-7.98
HZZ-11	120.00	12721	-8.21
HZZ-11	119.00	12743	-8.57
HZZ-11	118.00	12765	-8.64
HZZ-11	117.00	12786	-7.9
HZZ-11	116.00	12808	-8.71
HZZ-11	115.00	12830	-9.28
HZZ-11	114.00	12851	-9.23
HZZ-11	113.00	12873	-9.02
HZZ-11	112.00	12946	-8.89
HZZ-11	111.00	13020	-8.8
HZZ-11	110.00	13093	-9.05
HZZ-11	109.00	13167	-8.87
HZZ-11	108.00	13240	-9.03
HZZ-11	107.00	13314	-9.09
HZZ-11	106.00	13387	-8.94
HZZ-11	105.00	13461	-9.2
HZZ-11	104.00	13534	-9.06
HZZ-11	103.00	13608	-8.88
HZZ-11	102.00	13681	-8.85
HZZ-11	101.00	13755	-8.43
HZZ-11	100.00	13828	-8.49
HZZ-11	99.00	13901	-8.49
HZZ-11	98.00	13975	-8.24
HZZ-11	97.00	14048	-7.95
HZZ-11	96.00	14122	-8.06
HZZ-11	95.00	14195	-8.1
HZZ-11	94.00	14242	-8.28
HZZ-11	93.00	14289	-8.41
HZZ-11	92.67	14297	-8.43
HZZ-11	92.33	14306	-8.61
HZZ-11	92.00	14314	-8.33
HZZ-11	91.67	14323	-8.44
HZZ-11	91.33	14332	-8.53
HZZ-11	91.00	14340	-8.31
HZZ-11	90.67	14349	-8.49
HZZ-11	90.33	14357	-8.34
HZZ-11	90.00	14366	-8.4
HZZ-11	89.67	14375	-8.36
HZZ-11	89.33	14383	-8.29
HZZ-11	89.00	14392	-8.64
HZZ-11	88.67	14400	-8.27
HZZ-11	88.33	14409	-8.36
HZZ-11	88.00	14418	-8.2
HZZ-11	87.78	14426	-8.36
HZZ-11	87.56	14435	-8.39
HZZ-11	87.33	14443	-8.58
HZZ-11	87.11	14452	-8.31
HZZ-11	86.89	14472	-8.34
HZZ-11	86.67	14491	-8.62
HZZ-11	86.44	14511	-8.41
HZZ-11	86.22	14530	-8.4
HZZ-11	86.00	14550	-8.75
HZZ-11	85.67	14579	-8.31
HZZ-11	85.33	14608	-7.95
HZZ-11	85.00	14638	-8.28
HZZ-11	84.67	14667	-7.82
HZZ-11	84.33	14696	-7.72
HZZ-11	84.00	14726	-7.48
HZZ-11	83.67	14755	-7.48
HZZ-11	83.33	14784	-6.74
HZZ-11	83.00	14814	-6.97
HZZ-11	82.67	14843	-6.71
HZZ-11	82.33	14872	-6.6
HZZ-11	82.00	14902	-6.48
HZZ-11	81.67	14931	-6.61
HZZ-11	81.33	14960	-6.5
HZZ-11	81.00	14980	-6.23
HZZ-11	80.67	15052	-6.26
HZZ-11	80.33	15123	-6.29
HZZ-11	80.00	15195	-6.21
HZZ-11	79.67	15267	-6.24
HZZ-11	79.33	15338	-6.48
HZZ-11	79.00	15410	-6.64
HZZ-11	78.75	15436	-6.57
HZZ-11	78.50	15462	-6.5
HZZ-11	78.25	15488	-6.49
HZZ-11	78.00	15514	-6.4
HZZ-11	77.75	15540	-6.41
HZZ-11	77.50	15566	-6.35
HZZ-11	77.25	15592	-6.33
HZZ-11	77.00	15618	-6.05
HZZ-11	76.75	15644	-5.84
HZZ-11	76.50	15669	-5.93
HZZ-11	76.25	15695	-5.98
HZZ-11	76.00	15721	-5.93
HZZ-11	75.75	15747	-5.95
HZZ-11	75.50	15773	-5.9
HZZ-11	75.25	15799	-5.87
HZZ-11	75.00	15825	-5.89
HZZ-11	74.75	15851	-5.79
HZZ-11	74.50	15877	-5.83
HZZ-11	74.25	15903	-5.62
HZZ-11	74.00	15929	-5.44
HZZ-11	73.75	15955	-5.39
HZZ-11	73.50	15981	-5.35
HZZ-11	73.25	16007	-5.39
HZZ-11	73.00	16033	-5.15
HZZ-11	72.71	16062	-5.72
HZZ-11	72.43	16092	-5.95
HZZ-11	72.14	16122	-6.29
HZZ-11	71.86	16151	-6.51
HZZ-11	71.57	16181	-6.69
HZZ-11	71.29	16211	-6.71
HZZ-11	71.00	16240	-6.95
HZZ-11	70.60	16282	-6.61
HZZ-11	70.20	16323	-6.8
HZZ-11	69.80	16360	-6.55
HZZ-11	69.40	16391	-6.55
HZZ-11	69.00	16422	-6.49
HZZ-11	68.60	16453	-6.57
HZZ-11	68.20	16484	-6.6
HZZ-11	67.80	16515	-6.55
HZZ-11	67.40	16547	-6.52
HZZ-11	67.00	16578	-6.41
HZZ-11	66.60	16609	-6.34
HZZ-11	66.20	16640	-6.4
HZZ-11	65.80	16671	-6.43
HZZ-11	65.40	16702	-6.39
HZZ-11	65.00	16733	-6.41
HZZ-11	64.74	16754	-6.36
HZZ-11	64.48	16774	-6.43
HZZ-11	64.23	16794	-6.78
HZZ-11	63.97	16814	-6.84
HZZ-11	63.71	16834	-6.94
HZZ-11	63.45	16854	-7
HZZ-11	63.19	16874	-7.15
HZZ-11	62.94	16901	-7.27
HZZ-11	62.68	16948	-7.18
HZZ-11	62.42	16995	-7.09
HZZ-11	62.16	17042	-7.04
HZZ-11	61.90	17088	-7.02
HZZ-11	61.65	17135	-7.17
HZZ-11	61.39	17182	-7.19
HZZ-11	61.13	17229	-7.21
HZZ-11	60.87	17276	-7.25
HZZ-11	60.61	17323	-7.37
HZZ-11	60.35	17370	-7.34
HZZ-11	60.10	17417	-7.62
HZZ-11	59.84	17463	-7.93
HZZ-11	59.58	17510	-7.49
HZZ-11	59.32	17557	-7.89
HZZ-11	59.06	17604	-7.93
HZZ-11	58.81	17651	-8.04
HZZ-11	58.55	17698	-7.98
HZZ-11	58.29	17745	-7.99
HZZ-11	58.03	17792	-8.07
HZZ-11	57.77	17839	-8.07
HZZ-11	57.52	17885	-8.08
HZZ-11	57.26	17932	-7.92
HZZ-11	57.00	17979	-8.17
HZZ-11	56.75	18025	-8.17
HZZ-11	56.50	18070	-8.17
HZZ-11	56.25	18115	-8.13
HZZ-11	56.00	18161	-7.91
HZZ-11	55.75	18206	-8.03
HZZ-11	55.50	18252	-7.9
HZZ-11	55.25	18297	-7.82
HZZ-11	55.00	18342	-8.1
HZZ-11	54.00	18524	-7.81
HZZ-11	53.00	18748	-8.04
HZZ-11	52.00	18971	-7.76
HZZ-11	51.00	19195	-7.83
HZZ-11	50.00	19418	-7.63
HZZ-11	49.00	19642	-7.5
HZZ-11	48.00	19865	-7.73
HZZ-11	47.00	20089	-7.84
HZZ-11	46.00	20313	-7.82
HZZ-11	45.00	20536	-7.88
HZZ-11	44.00	20760	-7.72
HZZ-11	43.00	20909	-7.79
HZZ-11	42.00	21058	-7.52
HZZ-11	41.00	21207	-7.39
HZZ-11	40.00	21356	-7.9
HZZ-11	39.00	21505	-7.94
HZZ-11	38.00	21654	-7.54
HZZ-11	37.00	21804	-7.6
HZZ-11	36.00	21953	-7.64
HZZ-11	35.00	22102	-7.83
HZZ-11	34.00	22251	-7.69
HZZ-11	33.00	22400	-8.02
HZZ-11	32.00	22549	-8.23
HZZ-11	31.00	22698	-7.72
HZZ-11	30.00	22848	-8.26
HZZ-11	29.00	23118	-8.28
HZZ-11	28.00	23389	-7.83
HZZ-11	27.00	23660	-7.48
HZZ-11	26.00	23931	-7.62
HZZ-11	25.00	24202	-7.83
HZZ-11	24.00	24473	-7.75
HZZ-11	23.00	24744	-7.84
HZZ-11	22.00	25015	-7.72
HZZ-11	21.00	25286	-7.86
HZZ-11	20.00	25557	-8.15
HZZ-11	19.00	25828	-8.26
HZZ-11	18.00	26099	-8.46
HZZ-11	17.00	26369	-8.37
HZZ-11	16.00	26640	-8.46
HZZ-11	15.00	26911	-8.69
HZZ-11	14.00	27182	-8.62
HZZ-11	13.00	27453	-8.76
HZZ-11	12.00	27724	-8.76
HZZ-11	11.00	27995	-9.21
HZZ-11	10.00	28266	-9.3
HZZ-11	9.00	28537	-8.24
HZZ-11	8.00	28808	-8.49
HZZ-11	7.00	29079	-8.44
HZZ-11	6.00	29350	-8.91
HZZ-11	5.00	29620	-9.55
HZZ-11	4.00	29891	-8.25
HZZ-11	3.00	30162	-7.94
HZZ-11	2.00	30433	-8.04
HZZ-27	266	9350	-9.48
HZZ-27	264	9435	-9.53
HZZ-27	262	9519	-9.87
HZZ-27	260	9604	-10.00
HZZ-27	258	9689	-9.56
HZZ-27	256	9773	-9.59
HZZ-27	254	9858	-9.63
HZZ-27	252	9943	-9.61
HZZ-27	250	10027	-9.50
HZZ-27	248	10112	-9.48
HZZ-27	246	10197	-9.40
HZZ-27	244	10281	-9.37
HZZ-27	242	10366	-9.44
HZZ-27	240	10451	-9.33
HZZ-27	238	10536	-10.00
HZZ-27	236	10620	-9.79
HZZ-27	234	10705	-9.19
HZZ-27	232	10790	-9.64
HZZ-27	230	10874	-9.46
HZZ-27	228	10959	-9.35
HZZ-27	226	11044	-9.18
HZZ-27	225	11086	-9.05
HZZ-27	224	11128	-9.19
HZZ-27	223	11171	-9.17
HZZ-27	222	11213	-9.18
HZZ-27	221	11255	-9.12
HZZ-27	220	11298	-9.47
HZZ-27	219	11340	-9.04
HZZ-27	218	11382	-8.79
HZZ-27	217	11425	-8.52
HZZ-27	216	11467	-8.54
HZZ-27	215	11509	-9.02
HZZ-27	214	11552	-8.98
HZZ-27	213	11594	-8.77
HZZ-27	212	11652	-8.57
HZZ-27	211	11710	-8.06
HZZ-27	210	11873	-7.80
HZZ-27	209	12036	-7.52
HZZ-27	208	12198	-7.73
HZZ-27	207	12361	-7.70
HZZ-27	206	12524	-7.45
HZZ-27	205	12687	-7.44
HZZ-27	204.5	12768	-7.91
HZZ-27	204	12850	-8.66
HZZ-27	203	13013	-8.70
HZZ-27	202	13176	-9.05
HZZ-27	201	13338	-9.18
HZZ-27	200	13501	-8.95
HZZ-27	199	13534	-9.10
HZZ-27	198	13568	-8.71
HZZ-27	197	13601	-9.02
HZZ-27	196	13634	-8.89
HZZ-27	195	13667	-8.92
HZZ-27	194	13700	-8.92
HZZ-27	193	13733	-9.00
HZZ-27	192	13767	-8.70
HZZ-27	191	13800	-8.48
HZZ-27	190	13833	-8.40
HZZ-27	189	13866	-8.19
HZZ-27	188	13899	-8.10
HZZ-27	187	13933	-8.10
HZZ-27	186	13966	-8.08
HZZ-27	185	13999	-7.90
HZZ-27	184	14032	-8.15
HZZ-27	183	14065	-8.01
HZZ-27	182	14098	-8.36
HZZ-27	181	14132	-8.22
HZZ-27	180	14190	-8.13
HZZ-27	179	14249	-8.16
HZZ-27	178	14307	-8.55
HZZ-27	177	14366	-8.31
HZZ-27	176	14424	-7.90
HZZ-27	175	14483	-8.00
HZZ-27	174	14542	-8.30
HZZ-27	173	14600	-7.80
HZZ-27	172	14659	-7.37
HZZ-27	171	14717	-6.58
HZZ-27	170	14776	-6.63
HZZ-27	169	14834	-6.53
HZZ-27	168	14907	-6.50
HZZ-27	167	14980	-5.97
HZZ-27	166	15053	-6.27
HZZ-27	165	15126	-5.80
HZZ-27	164	15199	-6.52
HZZ-27	163	15272	-6.27
HZZ-27	162	15345	-6.23
HZZ-27	161	15418	-6.13
HZZ-27	160	15491	-5.89
HZZ-27	159	15564	-5.61
HZZ-27	158	15636	-5.60
HZZ-27	157	15709	-5.67
HZZ-27	156	15814	-5.19
HZZ-27	155	15918	-4.93
HZZ-27	154	16022	-5.86
HZZ-27	153	16127	-6.12
HZZ-27	152	16231	-6.38
HZZ-27	151	16336	-6.50
HZZ-27	150	16440	-6.45
HZZ-27	149	16544	-6.29
HZZ-27	148	16649	-6.32
HZZ-27	147	16753	-6.28
HZZ-27	146	16903	-6.57
HZZ-27	145	17052	-6.70
HZZ-27	144	17202	-7.07
HZZ-27	143	17352	-7.10
HZZ-27	142	17501	-7.39
HZZ-27	141	17651	-7.92
HZZ-27	140	17829	-8.04
HZZ-27	139	18006	-7.98
HZZ-27	138	18184	-7.81
HZZ-27	137	18362	-7.87
HZZ-27	136	18540	-8.01
HZZ-27	135	18717	-7.63
HZZ-27	134	18895	-8.12
HZZ-27	133	19073	-8.04
HZZ-27	132	19251	-7.88
HZZ-27	131	19428	-8.25
HZZ-27	130	19606	-7.74
HZZ-27	129	19784	-7.73
HZZ-27	128	19961	-7.59
HZZ-27	127	20139	-7.60
HZZ-27	126	20317	-7.83
HZZ-27	125	20476	-7.783
HZZ-27	124	20635	-8.087
HZZ-27	123	20794	-7.798
HZZ-27	122	20952	-7.368