# Santa Barbara Basin 640 Year Alkenone Sea Surface Temperature 
#-----------------------------------------------------------------------
#               World Data Center for Paleoclimatology, Boulder
#                                   and
#                      NOAA Paleoclimatology Program
#-----------------------------------------------------------------------
# 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.
#
#
# Online_Resource: http://ncdc.noaa.gov/paleo/study/17755
#
# Original_Source_URL: ftp://ftp.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/zhao2000/zhao2000.txt
#
# Description/Documentation lines begin with #
# Data lines have no #
#
# Archive: Paleoceanography
#---------------------------------------
# Contribution_Date
#    Date: 2015-01-12
#---------------------------------------
# Title
#    Study_Name: Santa Barbara Basin 640 Year Alkenone Sea Surface Temperature 
#---------------------------------------
# Investigators
#      Investigators: Zhao, M.; Eglinton, G.; Read, G.; Schimmelmann, A. 
#---------------------------------------
# Description and Notes
#       Description: High resolution (near-annual) alkenone-derived SST from varved sediments collected in the Santa Barbara Basin.
#	The data were originally published in Zhao et al., 2000, also presented with a recently thoroughly revised chronology 
#	fully detailed in Hendy et al., 2013, and in Schimmelmann et al., 2013. The alkenone-based SST record is a composite record 
#	of 2 marine sediment box cores, SABA87-2 and SABA88-1, retrieved from the same location. The data with revised chronology 
#	have been utilized in the PAGES Ocean2k synthesis effort (McGregor et al.). 
#
#---------------------------------------
# Publication
# Authors: McGregor, H.V.; Evans, M. N.; Goosse, H.; Leduc, G.; Martrat, B.; Addison, J.A.; Mortyn, P.G.; Oppo, D.W.; Seidenkrantz, M.S.; Sicre, M.A.; Phipps, S.J.; Selvaraj, K.; Thirumalai, K.; Filipsson, H.L.; Ersek, V.
# Published_Date_or_Year: submitted (Oct 2014)
# Published_Title: Robust global ocean cooling trend for the pre-industrial Common Era
# Journal_Name: Nature Geoscience
# Volume: 
# Issue: 
# Pages: 
# Report Number: 
# DOI: 
# Abstract: The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the Common Era (past 2000 years) global ocean sea surface temperature (SST) variations, and the underlying driving mechanisms, are poorly constrained. Here we present a global synthesis of Common Era SSTs derived solely from marine archives. The synthesis uses 57 individual SST reconstructions that meet strict quality control criteria. We find an SST cooling trend during 0-1800 CE that is robust against explicit tests for potential biases in the reconstructions. The surface cooling trend for 801-1800 CE is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with SST simulated by an ensemble of climate model simulations using best estimates of past forcings. Single and cumulative forcing climate model simulations suggest that the ocean SST cooling trend is not a response to orbital forcing, which is globally weak over this interval, but rather to increased frequency of explosive volcanism in recent centuries. This finding provides support for the hypothesis that ocean dynamics transform episodic volcanic forcing into a centennial and global-scale cooling trend.
#---------------------------------------
# Publication
# Authors: Zhao, M.; Eglinton, G.; Read, G.; Schimmelmann, A. 
# Published_Date_or_Year: 2000-09-01
# Published_Title: An alkenone (U37K') quasi-annual sea surface temperature record (A.D. 1440 to 1940) using varved sediments from the Santa Barbara Basin. 
# Journal_Name: Organic Geochemistry 
# Volume: 31
# Issue: 9
# Pages: 903-917
# Report Number: 
# DOI: 10.1016/S0146-6380(00)00034-6
# Abstract: Analyses for C37 alkenones (U37K') and total organic carbon (TOC) in a varved core from the depocenter of the Santa Barbara Basin (34deg13.5'N, 120deg01'W, 590 m water depth) have been made on an approximately 1-2 year basis from A.D. 1440 to 1940. The U37K'-based sea surface temperature (SST) record oscillates around 15.5C with an amplitude of less than 3C at approximately interannual, decadal, and centennial frequencies. Historical El Nino/Southern Oscillation (ENSO) events are matched only partially by warmer U37K' SSTs. Three records: our SST, a published Pacific coral d18O, and a published tree-ring temperature anomaly from the California valleys, show no evidence of colder temperatures during the Little Ice Age (ca. 1500 to 1840 A.D.). Significantly, there is a strong centennial-scale cyclicity in the U37K' SST record which approaches 1C in amplitude. TOC burial and alkenone fluxes are largely controlled by sedimentation rate as expressed in varve thickness.
#
#---------------------------------------
# Publication
# Authors: Ingrid L. Hendy, L. Dunn, A. Schimmelmann, D.K. Pak
# Published_Date_or_Year: 2013-10-15
# Published_Title: Resolving varve and radiocarbon chronology differences during the last 2000 years in the Santa Barbara Basin sedimentary record, California.
# Journal_Name: Quaternary International 
# Volume: 310
# Issue: 
# Pages: 155-168
# Report Number: 
# DOI: 10.1016/j.quaint.2012.09.006
# Abstract: Santa Barbara Basin (SBB) is well known for producing high quality paleoclimate reconstructions, but the validity of correlations between the basin and other regions rests upon age model accuracy. Yet, the two independent and well-established chronologies based on varve counting and radiocarbon dating do not consistently agree during the last two millennia. Here the validity of age model assumptions is tested including whether 1) the regional reservoir age of surface waters was invariably 641 +/- 119 years through time, and/or 2) SBB laminae couplets are consistently annual varves and counted with sufficient precision. This high-resolution 14C study of SBB sediments compares 49 mixed planktonic foraminiferal carbonate and 20 terrestrial organic carbon 14C dates to the varve chronology, to extend the high-resolution paleoclimate chronology of the basin back ~2000 years. Evidence indicates that regional reservoir ages do not remain constant through time with DeltaR, (i.e. regional reservoir age minus variations in the global mixed-layer ocean reservoir age) fluctuating between 80 and 350 years. Second, there is a consistent (R2 = 0.96) undercounting of the varves between 150 and ~1700 AD based on a new varying DeltaR14C chronology, indicating that some laminae couplets may not be annual. Loss of varves may occur when low riverine input and infrequent winter storm activity during drought intervals fail to supply a siliciclastic layer.
#
#---------------------------------------
# Publication
# Authors: Arndt Schimmelmann, Ingrid L. Hendy, Larianna Dunn, Dorothy K. Pak, and Carina B. Lange
# Published_Date_or_Year: 2013-05-31
# Published_Title: Revised ~2000-year chronostratigraphy of partially varved marine sediment in Santa Barbara Basin, California. 
# Journal_Name: GFF
# Volume: 135
# Issue: 3-4
# Pages: 258-264
# Report Number: 
# DOI: 10.1080/11035897.2013.773066
# Abstract: Sediment in the deep center of the Santa Barbara Basin (SBB) is almost completely laminated for the portion representing the past ~2000 years and has been utilized as an archive for high-resolution paleoceanography since the 1970s. Unequivocal proof of the presence of varves in SBB sediment throughout the 20th century has been uncritically used to assume that deeper laminations are varves as well and that they can be counted down-core to arrive at a reliable varve chronology for the past ~2000 years. The advent of radiocarbon accelerator mass-spectrometric (AMS) dating of sub-milligram-sized organic terrigenous plant fragments and charcoal enabled us to independently date SBB sediment without the underlying uncertainty of variable marine radiocarbon reservoir ages. It was determined that the traditional SBB varve-count ages remain valid from the present down to ~1700 AD, whereas not all deeper laminations represent varves. Depending on depth, the newly revised chronostratigraphy deviates from the traditional varve count by up to ~400 years. Here, we present (i) a historic overview of the SBB varve chronology, (ii) a critique of the extended, traditional "varve chronology" and (iii) the rationale behind our new chronology that overcomes the long-standing misunderstanding and bias in lamination counting that was assumed to be "varve counting" below the ~1700 AD level. Evidence from other California offshore locations indicates that the oxygenation of the deeper water column has been decreasing over the past few hundred years, and this facilitated a transition from laminated and possibly intermittently varved sediment to continuously varved sediment in the SBB.
#
#---------------------------------------
# Funding_Agency
#    Funding_Agency_Name: 
#    Grant: 
#---------------------------------------
# Site Information
# 	Site_Name: SABA87-2
# 	Location: Ocean>Pacific Ocean>Eastern Pacific Ocean
# 	Country: 
# 	Northernmost_Latitude: 34.2267
# 	Southernmost_Latitude: 34.2267
# 	Easternmost_Longitude: -120.0167
# 	Westernmost_Longitude: -120.0167
# 	Elevation: -590
#---------------------------------------
# Data_Collection   
#	Collection_Name: Zhao2000SBB
#	Earliest_Year: 1297
#	Most_Recent_Year: 1941
#	Time_Unit: AD
#	Core_Length: 
#	Notes:  
#------------------
# Chronology: 
#
# Data presented here with original Zhao 2000 chronology 
#
#---------------------------------------
# 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)
# 
##age_AD	age,,, year AD,,,,linear interpolation, N
##sst-uk37.p	sea-surface temperature, alkenone, , deg C, , Paleoceanography, , Prahl et al. (1988), N
##notes	notes-Core ID,,,,,,,,C
#
#----------------
# Data
# Data lines follow (have no #)
# Data line format - tab-delimited text, variable short name as header
# Missing Value: NA
# Original dataset from Zhao et al. (2000) 
#
age_AD	sst-uk37.p	notes
1941.3 	16.40 	SABA 87-2
1940.1 	16.40 	SABA 87-2
1938.7 	16.00 	SABA 87-2
1937.5 	15.70 	SABA 87-2
1936.9 	15.40 	SABA 87-2
1936.0 	15.50 	SABA 87-2
1934.7 	15.20 	SABA 87-2
1934.0 	15.10 	SABA 87-2
1933.4 	15.30 	SABA 87-2
1932.7 	14.90 	SABA 87-2
1931.7 	15.40 	SABA 87-2
1930.9 	15.10 	SABA 87-2
1930.3 	15.50 	SABA 87-2
1929.4 	14.90 	SABA 87-2
1928.6 	15.10 	SABA 87-2
1927.7 	15.40 	SABA 87-2
1927.0 	15.20 	SABA 87-2
1926.1 	15.10 	SABA 87-2
1925.2 	15.20 	SABA 87-2
1924.3 	15.40 	SABA 87-2
1923.5 	15.40 	SABA 87-2
1922.7 	15.30 	SABA 87-2
1922.3 	15.50 	SABA 87-2
1921.6 	15.30 	SABA 87-2
1920.9 	15.40 	SABA 87-2
1920.4 	15.00 	SABA 87-2
1919.9 	15.00 	SABA 87-2
1919.5 	15.50 	SABA 87-2
1919.2 	15.70 	SABA 87-2
1918.6 	15.60 	SABA 87-2
1918.1 	15.30 	SABA 87-2
1917.0 	15.60 	SABA 87-2
1916.2 	15.40 	SABA 87-2
1915.2 	15.30 	SABA 87-2
1914.2 	15.30 	SABA 87-2
1913.7 	15.80 	SABA 87-2
1913.3 	15.50 	SABA 87-2
1912.8 	14.90 	SABA 87-2
1912.6 	15.10 	SABA 87-2
1912.1 	14.70 	SABA 87-2
1911.6 	14.90 	SABA 87-2
1911.1 	15.10 	SABA 87-2
1910.8 	15.50 	SABA 87-2
1910.6 	15.00 	SABA 87-2
1910.3 	14.80 	SABA 87-2
1909.4 	14.90 	SABA 87-2
1908.3 	14.90 	SABA 87-2
1907.8 	15.00 	SABA 87-2
1907.3 	NA	SABA 87-2
1906.7 	NA	SABA 87-2
1905.9 	14.70 	SABA 87-2
1905.1 	14.80 	SABA 87-2
1904.6 	14.60 	SABA 87-2
1904.1 	14.60 	SABA 87-2
1902.9 	14.60 	SABA 87-2
1901.7 	14.50 	SABA 87-2
1900.9 	13.90 	SABA 87-2
1900.6 	14.50 	SABA 87-2
1900.3 	NA	SABA 87-2
1899.9 	14.50 	SABA 87-2
1899.5 	14.80 	SABA 87-2
1899.0 	14.90 	SABA 87-2
1898.4 	15.10 	SABA 87-2
1897.4 	15.40 	SABA 87-2
1896.4 	14.90 	SABA 87-2
1895.8 	15.00 	SABA 87-2
1895.3 	15.10 	SABA 87-2
1894.9 	14.60 	SABA 87-2
1894.7 	15.50 	SABA 87-2
1894.7 	NA	SABA 87-2
1894.7 	NA	SABA 87-2
1894.6 	15.30 	SABA 87-2
1894.4 	15.30 	SABA 87-2
1894.2 	15.10 	SABA 87-2
1894.0 	15.00 	SABA 87-2
1893.8 	15.30 	SABA 87-2
1892.9 	15.10 	SABA 87-2
1892.4 	15.60 	SABA 87-2
1892.0 	15.40 	SABA 87-2
1891.4 	15.40 	SABA 87-2
1891.0 	15.20 	SABA 87-2
1890.7 	15.40 	SABA 87-2
1890.0 	15.00 	SABA 87-2
1889.7 	15.50 	SABA 87-2
1889.4 	15.40 	SABA 87-2
1889.0 	15.20 	SABA 87-2
1888.5 	NA	SABA 87-2
1888.5 	NA	SABA 87-2
1888.5 	NA	SABA 87-2
1888.5 	NA	SABA 87-2
1888.5 	14.60 	SABA 87-2
1888.0 	14.90 	SABA 87-2
1887.5 	15.00 	SABA 87-2
1887.1 	14.70 	SABA 87-2
1886.8 	14.90 	SABA 87-2
1886.3 	14.90 	SABA 87-2
1885.7 	15.20 	SABA 87-2
1885.3 	15.30 	SABA 87-2
1884.5 	15.20 	SABA 87-2
1883.6 	16.00 	SABA 87-2
1882.6 	15.90 	SABA 87-2
1881.5 	15.70 	SABA 87-2
1880.9 	15.70 	SABA 87-2
1880.0 	14.90 	SABA 87-2
1879.4 	15.50 	SABA 87-2
1878.8 	15.90 	SABA 87-2
1878.6 	15.60 	SABA 87-2
1878.1 	15.70 	SABA 87-2
1877.6 	15.10 	SABA 87-2
1877.1 	16.00 	SABA 87-2
1876.5 	16.00 	SABA 87-2
1875.8 	16.20 	SABA 87-2
1875.1 	NA	SABA 87-2
1874.5 	15.20 	SABA 87-2
1874.1 	15.80 	SABA 87-2
1873.8 	17.50 	SABA 87-2
1873.6 	16.30 	SABA 87-2
1873.2 	16.10 	SABA 87-2
1872.8 	16.00 	SABA 87-2
1872.4 	16.30 	SABA 87-2
1872.0 	16.40 	SABA 87-2
1871.1 	16.10 	SABA 87-2
1870.0 	16.40 	SABA 87-2
1869.0 	15.10 	SABA 87-2
1868.0 	15.70 	SABA 87-2
1867.1 	16.10 	SABA 87-2
1866.3 	NA	SABA 87-2
1865.7 	15.90 	SABA 87-2
1864.9 	16.30 	SABA 87-2
1864.2 	15.90 	SABA 87-2
1863.4 	15.90 	SABA 87-2
1862.4 	15.80 	SABA 87-2
1861.7 	15.60 	SABA 87-2
1861.0 	15.00 	SABA 87-2
1860.0 	15.90 	SABA 87-2
1858.7 	15.80 	SABA 87-2
1858.0 	15.60 	SABA 87-2
1857.0 	15.90 	SABA 87-2
1856.6 	15.10 	SABA 87-2
1856.0 	15.80 	SABA 87-2
1855.1 	15.70 	SABA 87-2
1854.2 	15.50 	SABA 87-2
1853.2 	15.60 	SABA 87-2
1852.0 	15.30 	SABA 87-2
1851.6 	NA	SABA 87-2
1851.0 	NA	SABA 87-2
1850.0 	15.60 	SABA 87-2
1849.6 	15.60 	SABA 87-2
1848.0 	15.80 	SABA 87-2
1846.2 	15.30 	SABA 87-2
1845.6 	NA	SABA 87-2
1844.6 	NA	SABA 87-2
1844.0 	15.70 	SABA 87-2
1843.0 	15.30 	SABA 87-2
1842.0 	15.30 	SABA 87-2
1841.3 	NA	SABA 87-2
1840.6 	16.00 	SABA 87-2
1839.8 	15.70 	SABA 87-2
1838.9 	15.60 	SABA 87-2
1838.0 	15.50 	SABA 87-2
1837.1 	15.60 	SABA 87-2
1836.0 	15.50 	SABA 87-2
1835.0 	15.60 	SABA 87-2
1833.2 	NA	SABA 87-2
1830.9 	15.30 	SABA 87-2
1828.5 	15.00 	SABA 87-2
1826.7 	14.90 	SABA 87-2
1825.0 	15.50 	SABA 87-2
1822.7 	15.10 	SABA 87-2
1820.8 	15.40 	SABA 87-2
1819.0 	15.60 	SABA 87-2
1817.0 	15.60 	SABA 87-2
1815.9 	16.30 	SABA 87-2
1814.4 	15.60 	SABA 87-2
1812.0 	15.70 	SABA 87-2
1811.0 	15.70 	SABA 87-2
1809.8 	15.40 	SABA 87-2
1808.2 	15.20 	SABA 87-2
1806.5 	15.00 	SABA 87-2
1804.8 	15.30 	SABA 87-2
1803.7 	15.60 	SABA 87-2
1802.1 	15.20 	SABA 87-2
1800.0 	15.60 	SABA 87-2
1799.1 	15.30 	SABA 87-2
1797.8 	15.50 	SABA 87-2
1795.0 	15.40 	SABA 87-2
1793.4 	15.60 	SABA 87-2
1792.0 	15.80 	SABA 87-2
1790.9 	15.40 	SABA 87-2
1789.3 	15.40 	SABA 87-2
1788.1 	15.40 	SABA 87-2
1787.0 	15.50 	SABA 87-2
1786.0 	15.40 	SABA 87-2
1784.0 	15.50 	SABA 87-2
1783.0 	15.70 	SABA 87-2
1781.2 	15.60 	SABA 87-2
1779.9 	16.10 	SABA 87-2
1778.2 	16.10 	SABA 87-2
1777.2 	16.30 	SABA 87-2
1777.0 	NA	SABA 87-2
1776.0 	15.60 	SABA 87-2
1775.0 	15.90 	SABA 87-2
1774.6 	16.00 	SABA 87-2
1774.1 	15.90 	SABA 87-2
1773.0 	16.00 	SABA 87-2
1771.9 	15.70 	SABA 87-2
1771.0 	15.60 	SABA 87-2
1770.2 	15.60 	SABA 87-2
1769.0 	15.60 	SABA 87-2
1768.2 	15.60 	SABA 87-2
1767.5 	15.50 	SABA 87-2
1767.1 	15.90 	SABA 87-2
1766.5 	16.40 	SABA 87-2
1765.9 	16.10 	SABA 87-2
1765.0 	16.20 	SABA 87-2
1764.0 	16.00 	SABA 87-2
1763.6 	15.80 	SABA 87-2
1762.5 	15.90 	SABA 87-2
1761.0 	15.80 	SABA 87-2
1760.5 	16.10 	SABA 87-2
1759.3 	15.90 	SABA 87-2
1758.4 	15.60 	SABA 87-2
1757.0 	15.60 	SABA 87-2
1755.9 	15.80 	SABA 87-2
1753.9 	15.50 	SABA 87-2
1752.0 	15.70 	SABA 87-2
1751.1 	15.60 	SABA 87-2
1750.5 	NA	SABA 87-2
1749.7 	15.50 	SABA 87-2
1748.9 	15.90 	SABA 87-2
1748.3 	16.20 	SABA 87-2
1747.4 	15.40 	SABA 87-2
1746.5 	15.30 	SABA 87-2
1745.8 	15.60 	SABA 87-2
1745.0 	15.70 	SABA 87-2
1744.5 	16.30 	SABA 87-2
1744.0 	15.90 	SABA 87-2
1743.1 	15.80 	SABA 87-2
1742.0 	16.10 	SABA 87-2
1740.7 	16.00 	SABA 87-2
1740.2 	16.20 	SABA 87-2
1739.0 	15.90 	SABA 87-2
1738.0 	15.90 	SABA 87-2
1736.9 	15.30 	SABA 88-1
1736.0 	15.40 	SABA 88-1
1735.0 	15.30 	SABA 88-1
1734.0 	15.30 	SABA 88-1
1732.0 	15.50 	SABA 88-1
1730.6 	15.20 	SABA 88-1
1729.0 	15.40 	SABA 88-1
1728.3 	15.40 	SABA 88-1
1727.8 	15.50 	SABA 88-1
1727.4 	15.60 	SABA 88-1
1726.9 	15.40 	SABA 88-1
1726.5 	15.60 	SABA 88-1
1725.8 	15.30 	SABA 88-1
1725.1 	15.30 	SABA 88-1
1724.6 	15.20 	SABA 88-1
1723.9 	15.40 	SABA 88-1
1723.1 	15.80 	SABA 88-1
1722.5 	15.40 	SABA 88-1
1722.0 	15.50 	SABA 88-1
1721.5 	15.40 	SABA 88-1
1720.9 	15.60 	SABA 88-1
1720.3 	15.70 	SABA 88-1
1719.8 	15.80 	SABA 88-1
1719.2 	15.50 	SABA 88-1
1718.8 	15.90 	SABA 88-1
1718.1 	15.70 	SABA 88-1
1717.5 	15.80 	SABA 88-1
1716.9 	15.70 	SABA 88-1
1716.0 	15.20 	SABA 88-1
1715.6 	15.30 	SABA 88-1
1715.2 	15.70 	SABA 88-1
1714.7 	15.40 	SABA 88-1
1713.9 	15.60 	SABA 88-1
1712.9 	15.70 	SABA 88-1
1712.1 	15.40 	SABA 88-1
1711.6 	15.50 	SABA 88-1
1711.1 	15.40 	SABA 88-1
1710.7 	15.10 	SABA 88-1
1710.0 	15.10 	SABA 88-1
1709.0 	15.00 	SABA 88-1
1707.9 	15.10 	SABA 88-1
1707.0 	15.30 	SABA 88-1
1706.0 	15.60 	SABA 88-1
1704.5 	15.70 	SABA 88-1
1703.0 	15.60 	SABA 88-1
1702.0 	15.80 	SABA 88-1
1701.4 	15.50 	SABA 88-1
1700.9 	15.40 	SABA 88-1
1700.6 	15.70 	SABA 88-1
1700.2 	15.60 	SABA 88-1
1697.9 	15.70 	SABA 88-1
1696.4 	15.60 	SABA 88-1
1694.8 	15.50 	SABA 88-1
1693.3 	15.60 	SABA 88-1
1691.5 	15.40 	SABA 88-1
1689.8 	15.40 	SABA 88-1
1687.7 	15.30 	SABA 88-1
1686.8 	15.90 	SABA 88-1
1686.0 	15.30 	SABA 88-1
1684.8 	15.10 	SABA 88-1
1683.9 	15.20 	SABA 88-1
1682.5 	14.10 	SABA 88-1
1681.6 	15.50 	SABA 88-1
1680.6 	15.90 	SABA 88-1
1679.0 	15.90 	SABA 88-1
1678.5 	15.50 	SABA 88-1
1677.7 	15.70 	SABA 88-1
1677.0 	15.40 	SABA 88-1
1675.8 	15.20 	SABA 88-1
1674.9 	15.20 	SABA 88-1
1673.8 	15.10 	SABA 88-1
1672.1 	15.40 	SABA 88-1
1670.4 	15.20 	SABA 88-1
1669.5 	15.40 	SABA 88-1
1668.5 	15.50 	SABA 88-1
1667.1 	15.40 	SABA 88-1
1665.9 	15.40 	SABA 88-1
1664.3 	15.40 	SABA 88-1
1663.3 	15.60 	SABA 88-1
1661.7 	15.80 	SABA 88-1
1660.0 	15.60 	SABA 88-1
1658.2 	15.60 	SABA 88-1
1656.8 	15.30 	SABA 88-1
1655.8 	15.40 	SABA 88-1
1654.4 	15.60 	SABA 88-1
1651.5 	15.40 	SABA 88-1
1649.6 	15.40 	SABA 88-1
1648.0 	16.40 	SABA 88-1
1647.1 	16.60 	SABA 88-1
1646.1 	16.50 	SABA 88-1
1645.4 	16.30 	SABA 88-1
1644.5 	15.50 	SABA 88-1
1644.0 	16.00 	SABA 88-1
1642.8 	15.90 	SABA 88-1
1642.1 	16.10 	SABA 88-1
1641.1 	15.90 	SABA 88-1
1640.4 	15.40 	SABA 88-1
1639.9 	NA	SABA 88-1
1639.2 	NA	SABA 88-1
1638.5 	NA	SABA 88-1
1637.6 	NA	SABA 88-1
1637.3 	NA	SABA 88-1
1637.3 	NA	SABA 88-1
1636.6 	NA	SABA 88-1
1635.7 	NA	SABA 88-1
1635.0 	NA	SABA 88-1
1634.3 	NA	SABA 88-1
1633.4 	NA	SABA 88-1
1632.2 	15.40 	SABA 88-1
1631.4 	16.00 	SABA 88-1
1630.5 	16.40 	SABA 88-1
1629.6 	16.40 	SABA 88-1
1628.1 	16.60 	SABA 88-1
1626.5 	15.60 	SABA 88-1
1624.4 	16.40 	SABA 88-1
1622.9 	16.40 	SABA 88-1
1621.8 	16.80 	SABA 88-1
1621.0 	16.40 	SABA 88-1
1620.3 	15.10 	SABA 88-1
1618.4 	16.30 	SABA 88-1
1616.3 	16.40 	SABA 88-1
1615.6 	16.70 	SABA 88-1
1614.9 	16.50 	SABA 88-1
1614.0 	15.10 	SABA 88-1
1613.0 	16.00 	SABA 88-1
1611.6 	16.20 	SABA 88-1
1610.6 	16.60 	SABA 88-1
1609.0 	16.30 	SABA 88-1
1607.4 	15.20 	SABA 88-1
1605.2 	15.60 	SABA 88-1
1604.1 	16.20 	SABA 88-1
1602.9 	16.10 	SABA 88-1
1600.8 	15.90 	SABA 88-1
1599.5 	15.10 	SABA 88-1
1598.9 	16.10 	SABA 88-1
1598.2 	16.40 	SABA 88-1
1597.7 	16.30 	SABA 88-1
1596.5 	16.00 	SABA 88-1
1594.4 	15.20 	SABA 88-1
1593.2 	16.10 	SABA 88-1
1592.2 	16.10 	SABA 88-1
1590.6 	15.30 	SABA 88-1
1588.9 	15.50 	SABA 88-1
1585.9 	14.80 	SABA 88-1
1584.4 	15.60 	SABA 88-1
1581.9 	15.70 	SABA 88-1
1580.6 	16.00 	SABA 88-1
1578.5 	15.50 	SABA 88-1
1576.6 	14.90 	SABA 88-1
1574.1 	15.40 	SABA 88-1
1571.9 	15.40 	SABA 88-1
1569.6 	15.40 	SABA 88-1
1568.1 	15.10 	SABA 88-1
1566.5 	14.80 	SABA 88-1
1564.4 	15.70 	SABA 88-1
1562.5 	15.80 	SABA 88-1
1560.6 	15.90 	SABA 88-1
1558.5 	15.90 	SABA 88-1
1557.3 	15.10 	SABA 88-1
1555.6 	15.30 	SABA 88-1
1553.8 	15.60 	SABA 88-1
1552.5 	15.10 	SABA 88-1
1550.7 	15.90 	SABA 88-1
1549.0 	15.40 	SABA 88-1
1547.3 	NA	SABA 88-1
1545.4 	15.80 	SABA 88-1
1543.6 	15.60 	SABA 88-1
1542.1 	15.30 	SABA 88-1
1540.7 	14.90 	SABA 88-1
1540.0 	15.90 	SABA 88-1
1538.9 	15.50 	SABA 88-1
1537.7 	15.20 	SABA 88-1
1536.7 	14.10 	SABA 88-1
1535.1 	14.30 	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1532.0 	NA	SABA 88-1
1530.5 	15.4	SABA 88-1
1529.3 	15.90 	SABA 88-1
1526.5 	15.30 	SABA 88-1
1524.3 	15.80 	SABA 88-1
1521.9 	15.50 	SABA 88-1
1519.9 	15.50 	SABA 88-1
1516.8 	15.60 	SABA 88-1
1513.2 	15.00 	SABA 88-1
1509.8 	15.50 	SABA 88-1
1507.1 	15.00 	SABA 88-1
1504.7 	15.40 	SABA 88-1
1502.1 	15.10 	SABA 88-1
1499.9 	14.70 	SABA 88-1
1497.5 	15.10 	SABA 88-1
1494.3 	15.80 	SABA 88-1
1491.9 	16.00 	SABA 88-1
1489.3 	15.60 	SABA 88-1
1487.3 	15.50 	SABA 88-1
1483.3 	16.30 	SABA 88-1
1480.8 	15.50 	SABA 88-1
1479.1 	15.60 	SABA 88-1
1477.3 	15.80 	SABA 88-1
1475.6 	15.30 	SABA 88-1
1473.2 	15.80 	SABA 88-1
1471.9 	15.70 	SABA 88-1
1468.8 	15.70 	SABA 88-1
1466.2 	15.80 	SABA 88-1
1464.9 	15.26 	SABA 88-1
1462.0 	15.85 	SABA 88-1
1458.7 	15.74 	SABA 88-1
1456.9 	15.59 	SABA 88-1
1455.3 	15.56 	SABA 88-1
1453.1 	14.79 	SABA 88-1
1451.4 	15.32 	SABA 88-1
1448.3 	15.71 	SABA 88-1
1446.6 	15.68 	SABA 88-1
1444.9 	15.74 	SABA 88-1
1444.9 	NA	SABA 88-1
1443.0 	15.91 	SABA 88-1
1441.5 	15.59 	SABA 88-1
1439.8 	15.76 	SABA 88-1
1438.1 	15.85 	SABA 88-1
1436.0 	15.71 	SABA 88-1
1432.9 	15.74 	SABA 88-1
1431.2 	15.53 	SABA 88-1
1429.5 	15.41 	SABA 88-1
1428.3 	15.68 	SABA 88-1
1427.0 	15.47 	SABA 88-1
1425.8 	15.76 	SABA 88-1
1424.4 	15.59 	SABA 88-1
1423.6 	15.50 	SABA 88-1
1422.0 	15.15 	SABA 88-1
1421.0 	15.53 	SABA 88-1
1419.6 	15.74 	SABA 88-1
1418.3 	16.03 	SABA 88-1
1417.2 	15.56 	SABA 88-1
1415.9 	14.88 	SABA 88-1
1414.2 	15.03 	SABA 88-1
1411.6 	15.71 	SABA 88-1
1410.2 	15.53 	SABA 88-1
1408.9 	15.74 	SABA 88-1
1407.3 	15.94 	SABA 88-1
1405.4 	15.68 	SABA 88-1
1403.9 	16.29 	SABA 88-1
1402.2 	15.94 	SABA 88-1
1401.0 	15.79 	SABA 88-1
1399.3 	15.76 	SABA 88-1
1397.1 	15.74 	SABA 88-1
1395.4 	15.21 	SABA 88-1
1393.3 	15.15 	SABA 88-1
1391.8 	15.21 	SABA 88-1
1389.4 	15.18 	SABA 88-1
1386.8 	15.68 	SABA 88-1
1385.1 	15.97 	SABA 88-1
1383.1 	16.32 	SABA 88-1
1381.5 	16.18 	SABA 88-1
1379.1 	16.82 	SABA 88-1
1378.3 	17.18 	SABA 88-1
1376.6 	15.44 	SABA 88-1
1375.5 	15.50 	SABA 88-1
1374.1 	15.56 	SABA 88-1
1372.1 	15.62 	SABA 88-1
1369.8 	15.76 	SABA 88-1
1367.5 	15.44 	SABA 88-1
1365.3 	15.74 	SABA 88-1
1364.1 	15.59 	SABA 88-1
1363.1 	15.79 	SABA 88-1
1361.9 	15.71 	SABA 88-1
1360.7 	15.82 	SABA 88-1
1359.2 	15.59 	SABA 88-1
1357.7 	16.00 	SABA 88-1
1356.2 	15.97 	SABA 88-1
1355.3 	15.82 	SABA 88-1
1353.9 	15.82 	SABA 88-1
1352.8 	15.91 	SABA 88-1
1351.6 	15.85 	SABA 88-1
1350.4 	15.62 	SABA 88-1
1349.4 	15.71 	SABA 88-1
1348.3 	15.59 	SABA 88-1
1347.6 	15.71 	SABA 88-1
1346.0 	15.79 	SABA 88-1
1344.9 	15.85 	SABA 88-1
1342.8 	15.62 	SABA 88-1
1340.5 	15.59 	SABA 88-1
1339.2 	15.38 	SABA 88-1
1337.9 	15.97 	SABA 88-1
1337.0 	15.50 	SABA 88-1
1337.0 	NA	SABA 88-1
1335.6 	15.47 	SABA 88-1
1333.6 	15.68 	SABA 88-1
1331.5 	15.41 	SABA 88-1
1329.8 	15.21 	SABA 88-1
1328.1 	15.24 	SABA 88-1
1326.1 	15.44 	SABA 88-1
1324.6 	16.06 	SABA 88-1
1323.3 	15.94 	SABA 88-1
1322.2 	15.68 	SABA 88-1
1320.1 	15.41 	SABA 88-1
1318.7 	15.47 	SABA 88-1
1317.4 	15.26 	SABA 88-1
1315.2 	14.88 	SABA 88-1
1313.4 	15.03 	SABA 88-1
1311.0 	15.12 	SABA 88-1
1309.8 	15.85 	SABA 88-1
1307.9 	15.62 	SABA 88-1
1307.1 	15.65 	SABA 88-1
1306.0 	15.82 	SABA 88-1
1304.1 	15.38 	SABA 88-1
1302.9 	15.50 	SABA 88-1
1300.9 	15.53 	SABA 88-1
1299.5 	15.09 	SABA 88-1
1298.6 	14.79 	SABA 88-1
1297.5 	14.97 	SABA 88-1