# Leviathan Chronology, Nevada 175KYr Stalagmite d18O Data
#----------------------------------------------------------------------- 
#                World Data Center for Paleoclimatology, Boulder 
#                                  and 
#                     NOAA Paleoclimatology Program 
#----------------------------------------------------------------------- 
# 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: http://hurricane.ncdc.noaa.gov/pls/paleox/f?p=519:1:::::P1_STUDY_ID:16517
#
# Original_Source_URL: ftp://ftp.ncdc.noaa.gov/pub/data/paleo/speleothem/northamerica/usa/nevada/leviathan2014lmc14.txt
# 
# Description/Documentation lines begin with #
# Data lines have no #
#
# Archive: Speleothems
#--------------------
# Contribution_Date
#	Date: 2014-05-29 
#--------------------
# Title
#	Study_Name: Leviathan Chronology, Nevada 175KYr Stalagmite d18O Data
#--------------------
# Investigators
#       Investigators: Lachniet, M.S.; Denniston, R.F.; Asmerom, Y.; Polyak, V.J.
#--------------------
# Description_and_Notes
#	Description: This file contains the contains the 50-yr interpolated raw d18O values, 
#	with no corrections applied, for Lehman Cave Stalagmite LMC14.
#
#	Age yr B2K means years before CE 2000. 
#	d18O is in permil relative to the VPDB scale, based on calibrated internal standards. 
#
#--------------------
# Publication 
#       Authors: Matthew S. Lachniet, Rhawn F. Denniston, Yemane Asmerom, Victor J. Polyak
#       Published_Date_or_Year: 2014-05-02      
#       Published_Title: Orbital control of western North America atmospheric circulation and climate over two glacial cycles
#       Journal_Name: Nature Communications
#       Volume: 5
#       Edition: 
#       Issue: 
#       Pages: 
#       DOI: 10.1038/ncomms4805 
#       Online_Resource: http://www.nature.com/ncomms/2014/140502/ncomms4805/full/ncomms4805.html
#       Full_Citation: 
#       Abstract: The now arid Great Basin of western North America hosted expansive late Quaternary pluvial lakes, yet the climate forcings that sustained large ice age hydrologic variations remain controversial. Here we present a 175,000 year oxygen isotope record from precisely-dated speleothems that documents a previously unrecognized and highly sensitive link between Great Basin climate and orbital forcing. Our data match the phasing and amplitudes of 65°N summer insolation, including the classic saw-tooth pattern of global ice volume and on-time terminations. Together with the observation of cold conditions during the marine isotope substage 5d glacial inception, our data document a strong precessional-scale Milankovitch forcing of southwestern paleoclimate. Because the expansion of pluvial lakes was associated with cold glacial conditions, the reappearance of large lakes in the Great Basin is unlikely until ca. 55,000 years into the future as climate remains in a mild non-glacial state over the next half eccentricity cycle.
#------------------
# Publication 
#       Authors: Jeremy D. Shakun, Stephen J. Burns, Peter U. Clark, Hai Cheng and R. Lawrence Edwards
#       Published_Date_or_Year: 2011-09-28      
#       Published_Title: Milankovitch-paced Termination II in a Nevada speleothem?
#       Journal_Name: Geophysical Research Letters
#       Volume: 38
#       Edition: 
#       Issue: 18
#       Pages: 
#       DOI: 10.1029/2011GL048560
#       Online_Resource: http://onlinelibrary.wiley.com/doi/10.1029/2011GL048560/abstract
#       Full_Citation: 
#       Abstract: The Devils Hole (DH) calcite record from the Great Basin, Nevada, provided the first radiometrically dated time series of late-Pleistocene climate fluctuations. In doing so, DH suggested that the penultimate deglaciation, Termination II (T-II), occurred at 142 ± 3 ka, which is ~10 kyr before the associated rise in summer insolation, helping to launch the "causality problem" for Milankovitch. The interpretation of the DH record has been subject to considerable discussion ever since. We present the first attempt to reproduce the DH record of an early T-II in the Great Basin based on a stalagmite from Lehman Caves, Nevada, which is ~400 km northeast of Devils Hole. Our speleothem records at least the latter part of T-II over its period of growth from ~133-129 ka, which appears to disagree with the early timing of T-II in DH. DH also exhibits important differences from many other paleoclimate records over the past two deglaciations, though these are reduced somewhat after ice-volume correcting DH d18O. We suggest that the climatic signal in the DH record remains to be fully explained.
#------------------
# Funding_Agency 
#       Funding_Agency_Name: US National Science Foundation
#       Grant: EPSCoR 0814372, EAR 0521196, EAR 0326902, ATM 0703353
#------------------
# Site_Information 
#       Site_Name: Lehman Cave
#       Location: North America>United States Of America>Nevada
#	Country: United States Of America
#	Northernmost_Latitude: 39.0
# 	Southernmost_Latitude: 39.0
# 	Easternmost_Longitude: -114.2
# 	Westernmost_Longitude: -114.2
# 	Elevation: 2080 m  
#------------------
# Data_Collection   
#	Collection_Name: Leviathan2014LMC14
#	Earliest_Year: 129300
#	Most_Recent_Year: 105700
#	Time_Unit: calendar years before 2000AD
#	Core_Length: m
#	Notes: 
#------------------
# Chronology: 
# 
# Table 1A. U-series data for stalagmite LC-1
#
# Depth (mm)	238U (ng/g)		232Th  (pg/g)		230Th/232Th activity ratio		230Th/238U activity ratio 		Measured d234U (‰) 		Initial d234U (‰)		Uncorrected age (yr BP)		Corrected age (yr BP)	
# 7	362	± 0.3	696	± 23	16	± 0.6	0.0006291	± 0.0000208	2226	± 3.2	2228	± 3.2	335	± 7	317	± 11	
# 14	340	± 0.3	584	± 38	27	± 1.8	0.0005616	± 0.0000362	2213	± 3.2	2216	± 3.2	507	± 11	491	± 13	
# 23	339	± 0.2	710	± 57	32	± 2.7	0.0006865	± 0.0000549	2190	± 3.2	2195	± 3.2	757	± 17	738	± 19	
# 27	358	± 0.2	488	± 30	51	± 3.2	0.0004456	± 0.0000272	2155	± 3.2	2160	± 3.2	794	± 9	782	± 11	
# 32	328	± 0.3	706	± 58	39	± 3.3	0.0007041	± 0.0000580	2199	± 3.2	2205	± 3.2	938	± 17	919	± 20	
# 41	360	± 0.4	502	± 47	72	± 6.8	0.0004561	± 0.0000425	2264	± 3.3	2271	± 3.3	1102	± 13	1090	± 14	
# 49	408	± 0.3	544	± 44	94	± 7.7	0.0004366	± 0.0000357	2240	± 3.2	2248	± 3.3	1389	± 11	1377	± 13	
# 60	408	± 0.2	930	± 28	66	± 2.1	0.0007456	± 0.0000226	2244	± 3.2	2255	± 3.3	1660	± 13	1639	± 16	
# 75	392	± 0.3	448	± 47	151	± 15.9	0.0003747	± 0.0000394	2260	± 3.3	2272	± 3.3	1902	± 14	1891	± 15	
# 84	420	± 0.4	364	± 46	219	± 27.8	0.0002840	± 0.0000359	2250	± 3.2	2263	± 3.3	2103	± 15	2095	± 16	
# 106	436	± 0.3	512	± 23	203	± 9.2	0.0003845	± 0.0000173	2248	± 3.2	2265	± 3.3	2656	± 9	2645	± 10	
# 134	458	± 0.8	432	± 28	356	± 22.8	0.0003086	± 0.0000197	2221	± 3.2	2245	± 3.3	3774	± 15	3765	± 16	
# 155	525	± 0.3	826	± 24	315	± 9.0	0.0005153	± 0.0000147	2329	± 3.3	2365	± 3.4	5436	± 13	5423	± 15	
# 166	388	± 0.2	1394	± 25	210	± 3.7	0.0011771	± 0.0000208	2250	± 3.2	2305	± 3.3	8566	± 21	8534	± 27	
# 181	187	± 1.0	635	± 75	266	± 31.6	0.0011098	± 0.0001318	1899	± 3.8	1962	± 3.9	11586	± 94	11553	± 96	
# 185	204	± 0.2	416	± 91	583	± 128.1	0.0006684	± 0.0001468	2306	± 3.5	2395	± 3.7	13507	± 71	13489	± 72	
# 188	170	± 1.1	383	± 81	935	± 198.5	0.0007358	± 0.0001562	1569	± 3.4	1722	± 4.2	32973	± 378	32949	± 378	
# 200	212	± 0.3	243	± 132	2418	± 1315.6	0.0003738	± 0.0002034	2024	± 4.7	2248	± 5.4	37210	± 181	37200	± 181	
# 210	262	± 0.2	723	± 54	1155	± 87.3	0.0009009	± 0.0000670	2105	± 3.1	2373	± 5.7	42433	± 680	42409	± 680	
# 223	175	± 0.2	346	± 50	1544	± 222.3	0.0006458	± 0.0000930	1896	± 2.9	2145	± 3.4	43870	± 131	43852	± 131	
# 230	172	± 0.2	542	± 59	976	± 105.6	0.0010310	± 0.0001115	1811	± 4.0	2062	± 4.8	45965	± 235	45935	± 235	
# 248	216	± 0.2	405	± 32	1742	± 136.9	0.0006125	± 0.0000481	1622	± 2.6	1888	± 3.2	53775	± 165	53756	± 165	
# 265	153	± 0.1	727	± 63	734	± 64.0	0.0015527	± 0.0001352	1624	± 2.7	1914	± 3.4	58305	± 250	58257	± 251	
# 280	246	± 0.3	443	± 67	2017	± 304.3	0.0005882	± 0.0000887	1689	± 2.9	1997	± 3.6	59388	± 194	59371	± 194	
# 296	322	± 0.3	338	± 31	3869	± 350.6	0.0003443	± 0.0000312	1543	± 2.5	1902	± 3.4	74293	± 246	74282	± 247	
# 320	283	± 0.1	333	± 44	3486	± 459.0	0.0003853	± 0.0000507	1490	± 2.5	1853	± 3.3	77341	± 243	77329	± 243	
# 352	271	± 0.2	305	± 24	3697	± 297.0	0.0003675	± 0.0000295	1466	± 2.5	1835	± 3.4	79617	± 264	79605	± 264	
# 373	269	± 0.2	294	± 23	3735	± 291.2	0.0003575	± 0.0000279	1402	± 2.4	1761	± 3.3	80708	± 265	80697	± 265	
# 410	310	± 0.1	464	± 47	2717	± 273.6	0.0004890	± 0.0000492	1334	± 2.3	1689	± 3.2	83523	± 268	83507	± 268	
# 432	248	± 0.2	522	± 29	2064	± 116.3	0.0006892	± 0.0000388	1402	± 2.4	1798	± 3.5	88116	± 341	88094	± 341	
# 456	365	± 0.2	219	± 27	8063	± 985.6	0.0001960	± 0.0000240	1513	± 2.5	1983	± 3.8	95748	± 328	95742	± 328	
# 470	395	± 0.2	216	± 40	8564	± 1569.8	0.0001791	± 0.0000328	1395	± 2.4	1843	± 3.6	98753	± 343	98748	± 343	
# 493	341	± 0.3	117	± 27	13958	± 3210.9	0.0001119	± 0.0000257	1421	± 2.4	1883	± 3.7	99659	± 352	99655	± 352	
# 515	362	± 0.3	383	± 31	4927	± 400.6	0.0003463	± 0.0000281	1595	± 2.6	2127	± 4.1	102034	± 361	102024	± 361	
# 535	227	± 0.1	635	± 47	1774	± 130.5	0.0009145	± 0.0000673	1248	± 2.2	1747	± 3.9	119305	± 450	119275	± 451	
# 546	324	± 0.1	1506	± 42	1066	± 29.8	0.0015221	± 0.0000424	1232	± 2.2	1732	± 3.8	120792	± 455	120742	± 455	
# Table 1B. U-series data for stalagmite LMC-14																	
# 5	243	± 0.1	4915	± 45	145	± 1.3	0.0066178	± 0.0000602	463	± 1.5	627	± 2.1	107522	± 347	107160	± 390	
# 27	493	± 0.5	2004	± 47	820	± 19.4	0.0013301	± 0.0000309	584	± 1.6	809	± 3.0	115370	± 920	115304	± 920	
# 43	571	± 0.4	2964	± 29	644	± 6.3	0.0016999	± 0.0000166	576	± 1.6	802	± 2.3	117114	± 325	117030	± 327	
# 52	1049	± 1.0	1621	± 38	1873	± 43.4	0.0005057	± 0.0000117	341	± 1.3	484	± 2.0	124044	± 388	124013	± 388	
# 60	965	± 1.1	12549	± 35	224	± 0.7	0.0042570	± 0.0000129	338	± 1.3	482	± 2.0	126389	± 426	126134	± 444	
# 64	1180	± 0.5	6436	± 25	548	± 2.2	0.0017846	± 0.0000069	370	± 1.4	528	± 2.0	125874	± 348	125770	± 351	
# 72	864	± 0.8	5442	± 39	502	± 3.7	0.0020615	± 0.0000150	429	± 1.4	615	± 2.2	128073	± 403	127959	± 407	
# Table 1C. U-series data for stalagmite LMC-21																	
# 6	163	± 0.1	1344	± 47	340	± 11.9	0.0026922	± 0.0000941	246	± 1.3	360	± 2.0	135184	± 521	135008	± 527	
# 15	144	± 0.1	132	± 46	3076	± 1070.6	0.0003004	± 0.0001046	246	± 1.2	363	± 1.9	137919	± 556	137899	± 556	
# 23	140	± 0.1	402	± 32	1011	± 81.5	0.0009429	± 0.0000760	259	± 1.4	388	± 2.2	143259	± 581	143199	± 581	
# 34	294	± 0.2	564	± 41	1726	± 126.7	0.0006275	± 0.0000461	347	± 1.3	543	± 2.3	158404	± 578	158368	± 578	
# 42	332	± 0.3	578	± 30	1927	± 101.2	0.0005701	± 0.0000299	355	± 1.4	559	± 2.5	160794	± 825	160762	± 825	
# 54	774	± 1.1	330	± 35	7961	± 840.3	0.0001394	± 0.0000147	342	± 1.3	550	± 2.5	168163	± 758	168155	± 758	
# 63	1038	± 0.8	221	± 27	16182	± 1978.1	0.0000697	± 0.0000085	357	± 1.4	576	± 2.6	169751	± 840	169748	± 840	
# 73	1270	± 0.6	234	± 33	18583	± 2632.1	0.0000604	± 0.0000086	341	± 1.3	555	± 2.4	172692	± 619	172688	± 619	
# Corrected ages use an average crustal value for the initial 230Th/232Th atomic ratio = 4.4 ± 2.2 ppm. Years before present = yrs BP, where present is AD 2010. 
# All errors are absolute 2sigma. 
# d234U = ([234U/238U]activity -1) x 1000. 
# [230Th/238U]activity = 1 - e-Lamda230T + (d234Umeasured/1000)[Lamda230/(Lamda230 - Lamda234)](1 - e-(Lamda230 - Lamda234)T), where T is the age. 
# Decay constants (Lamda) are 9.1577 ×10-6 year-1 for 230Th, 2.8263 × 10-6 year-1 for 234U, and 1.55125 × 10-10 year-1 for 238U. 																	
#
#
# 	
#----------------	
# Variables 
#
# Data variables follow that are preceded by "##" in columns one and two.
# Data line variables format:  Variables list, one per line, shortname-tab-longname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) 
#
##age_calBP2000	age, , , calendar years before 2000AD, , , , ,N
##d18OcarbVPDB	delta18O, calcium carbonate, , per mil VPDB, ,speleothem, , ,N 
#
#----------------
# Data:
# Data lines follow (have no #)
# Data line format - tab-delimited text, variable short name as header
# Missing Values:  
#
age_calBP2000	d18OcarbVPDB
105700	-13.82
105750	-13.79
105800	-13.76
105850	-13.73
105900	-13.70
105950	-13.67
106000	-13.64
106050	-13.62
106100	-13.62
106150	-13.62
106200	-13.62
106250	-13.63
106300	-13.63
106350	-13.63
106400	-13.63
106450	-13.57
106500	-13.50
106550	-13.44
106600	-13.37
106650	-13.30
106700	-13.24
106750	-13.17
106800	-13.17
106850	-13.25
106900	-13.33
106950	-13.41
107000	-13.49
107050	-13.57
107100	-13.65
107150	-13.73
107200	-13.81
107250	-13.90
107300	-13.98
107350	-14.07
107400	-14.15
107450	-14.23
107500	-14.32
107550	-14.47
107600	-14.67
107650	-14.87
107700	-15.07
107750	-15.27
107800	-15.46
107850	-15.66
107900	-15.82
107950	-15.83
108000	-15.84
108050	-15.85
108100	-15.86
108150	-15.87
108200	-15.88
108250	-15.89
108300	-15.85
108350	-15.81
108400	-15.76
108450	-15.71
108500	-15.67
108550	-15.62
108600	-15.57
108650	-15.52
108700	-15.45
108750	-15.37
108800	-15.30
108850	-15.23
108900	-15.16
108950	-15.09
109000	-15.02
109050	-14.99
109100	-14.96
109150	-14.93
109200	-14.90
109250	-14.86
109300	-14.83
109350	-14.80
109400	-14.81
109450	-14.84
109500	-14.88
109550	-14.91
109600	-14.94
109650	-14.98
109700	-15.01
109750	-15.02
109800	-14.93
109850	-14.84
109900	-14.75
109950	-14.66
110000	-14.57
110050	-14.48
110100	-14.39
110150	-14.38
110200	-14.39
110250	-14.39
110300	-14.40
110350	-14.41
110400	-14.42
110450	-14.43
110500	-14.43
110550	-14.42
110600	-14.42
110650	-14.41
110700	-14.40
110750	-14.40
110800	-14.39
110850	-14.38
110900	-14.41
110950	-14.44
111000	-14.47
111050	-14.50
111100	-14.53
111150	-14.56
111200	-14.59
111250	-14.62
111300	-14.66
111350	-14.70
111400	-14.74
111450	-14.78
111500	-14.82
111550	-14.86
111600	-14.87
111650	-14.81
111700	-14.74
111750	-14.67
111800	-14.61
111850	-14.54
111900	-14.47
111950	-14.41
112000	-14.41
112050	-14.44
112100	-14.47
112150	-14.50
112200	-14.53
112250	-14.56
112300	-14.59
112350	-14.59
112400	-14.56
112450	-14.52
112500	-14.49
112550	-14.45
112600	-14.42
112650	-14.38
112700	-14.35
112750	-14.37
112800	-14.40
112850	-14.42
112900	-14.45
112950	-14.48
113000	-14.50
113050	-14.53
113100	-14.58
113150	-14.64
113200	-14.71
113250	-14.78
113300	-14.85
113350	-14.91
113400	-14.98
113450	-15.03
113500	-15.00
113550	-14.97
113600	-14.94
113650	-14.91
113700	-14.87
113750	-14.84
113800	-14.81
113850	-14.76
113900	-14.71
113950	-14.65
114000	-14.59
114050	-14.54
114100	-14.48
114150	-14.42
114200	-14.37
114250	-14.31
114300	-14.26
114350	-14.21
114400	-14.15
114450	-14.10
114500	-14.05
114550	-13.99
114600	-13.97
114650	-13.95
114700	-13.92
114750	-13.90
114800	-13.88
114850	-13.86
114900	-13.83
114950	-13.84
115000	-13.88
115050	-13.92
115100	-13.96
115150	-14.00
115200	-14.04
115250	-14.07
115300	-14.12
115350	-14.24
115400	-14.35
115450	-14.30
115500	-14.24
115550	-14.48
115600	-14.78
115650	-14.80
115700	-14.69
115750	-14.48
115800	-14.18
115850	-14.08
115900	-14.32
115950	-14.42
116000	-13.95
116050	-13.51
116100	-13.61
116150	-13.70
116200	-13.56
116250	-13.39
116300	-13.54
116350	-13.81
116400	-13.94
116450	-13.98
116500	-13.97
116550	-13.91
116600	-13.90
116650	-14.03
116700	-14.16
116750	-14.35
116800	-14.54
116850	-14.50
116900	-14.44
116950	-14.42
117000	-14.40
117050	-14.40
117100	-14.41
117150	-14.42
117200	-14.43
117250	-14.44
117300	-14.45
117350	-14.46
117400	-14.47
117450	-14.48
117500	-14.49
117550	-14.50
117600	-14.51
117650	-14.52
117700	-14.53
117750	-14.54
117800	-14.55
117850	-14.54
117900	-14.54
117950	-14.54
118000	-14.53
118050	-14.53
118100	-14.52
118150	-14.52
118200	-14.51
118250	-14.51
118300	-14.50
118350	-14.50
118400	-14.49
118450	-14.49
118500	-14.48
118550	-14.48
118600	-14.47
118650	-14.45
118700	-14.43
118750	-14.41
118800	-14.40
118850	-14.38
118900	-14.36
118950	-14.34
119000	-14.33
119050	-14.31
119100	-14.29
119150	-14.27
119200	-14.26
119250	-14.24
119300	-14.22
119350	-14.20
119400	-14.11
119450	-14.03
119500	-13.94
119550	-13.85
119600	-13.77
119650	-13.68
119700	-13.60
119750	-13.51
119800	-13.42
119850	-13.34
119900	-13.25
119950	-13.17
120000	-13.08
120050	-13.00
120100	-12.91
120150	-12.85
120200	-12.82
120250	-12.79
120300	-12.76
120350	-12.73
120400	-12.70
120450	-12.67
120500	-12.63
120550	-12.60
120600	-12.57
120650	-12.54
120700	-12.51
120750	-12.48
120800	-12.45
120850	-12.41
120900	-12.38
120950	-12.37
121000	-12.36
121050	-12.34
121100	-12.33
121150	-12.32
121200	-12.30
121250	-12.29
121300	-12.28
121350	-12.26
121400	-12.25
121450	-12.24
121500	-12.22
121550	-12.21
121600	-12.20
121650	-12.18
121700	-12.17
121750	-12.17
121800	-12.16
121850	-12.15
121900	-12.14
121950	-12.14
122000	-12.13
122050	-12.12
122100	-12.12
122150	-12.11
122200	-12.10
122250	-12.09
122300	-12.09
122350	-12.08
122400	-12.07
122450	-12.07
122500	-12.09
122550	-12.11
122600	-12.13
122650	-12.15
122700	-12.17
122750	-12.19
122800	-12.21
122850	-12.23
122900	-12.26
122950	-12.28
123000	-12.30
123050	-12.32
123100	-12.34
123150	-12.36
123200	-12.38
123250	-12.36
123300	-12.28
123350	-12.21
123400	-12.14
123450	-12.06
123500	-11.99
123550	-11.92
123600	-11.84
123650	-11.77
123700	-11.70
123750	-11.62
123800	-11.55
123850	-11.48
123900	-11.40
123950	-11.33
124000	-11.26
124050	-11.41
124100	-11.56
124150	-11.70
124200	-11.33
124250	-10.97
124300	-10.66
124350	-10.77
124400	-10.88
124450	-10.94
124500	-10.77
124550	-10.60
124600	-10.58
124650	-10.96
124700	-11.35
124750	-11.59
124800	-11.55
124850	-11.50
124900	-11.34
124950	-10.98
125000	-10.63
125050	-10.48
125100	-10.57
125150	-10.66
125200	-10.91
125250	-11.29
125300	-11.68
125350	-11.88
125400	-11.95
125450	-12.03
125500	-11.89
125550	-11.64
125600	-11.39
125650	-11.40
125700	-11.49
125750	-11.58
125800	-11.48
125850	-11.34
125900	-11.21
125950	-11.07
126000	-10.93
126050	-10.84
126100	-10.84
126150	-10.83
126200	-10.83
126250	-10.83
126300	-10.83
126350	-10.96
126400	-11.12
126450	-11.27
126500	-11.43
126550	-11.59
126600	-11.57
126650	-11.33
126700	-11.09
126750	-10.85
126800	-10.61
126850	-10.36
126900	-10.41
126950	-10.47
127000	-10.54
127050	-10.60
127100	-10.66
127150	-10.76
127200	-10.91
127250	-11.05
127300	-11.19
127350	-11.34
127400	-11.48
127450	-11.43
127500	-11.38
127550	-11.33
127600	-11.28
127650	-11.23
127700	-11.27
127750	-11.38
127800	-11.49
127850	-11.60
127900	-11.71
127950	-11.81
128000	-11.73
128050	-11.64
128100	-11.56
128150	-11.47
128200	-11.39
128250	-11.42
128300	-11.53
128350	-11.65
128400	-11.77
128450	-11.88
128500	-11.97
128550	-11.87
128600	-11.76
128650	-11.66
128700	-11.55
128750	-11.45
128800	-11.28
128850	-11.07
128900	-10.87
128950	-10.66
129000	-10.45
129050	-10.31
129100	-10.52
129150	-10.72
129200	-10.92
129250	-11.13
129300	-11.33