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Africa 001.d18O +Temperature estimates determined using linear regression between speleothem d18O and annual mean temperature. An "anomalous" period, from AD 1956-1976 was removed from this calibration. In the context of the Holocene, the application of this calibration results in temperature trends contrary to other published records for the last 10,000 years.  +
Ant 022.dD +Data for past 1000 years from https://www.ncdc.noaa.gov/paleo/study/14201; data for first millennium CE from https://www.ncdc.noaa.gov/paleo/study/13954 (centennial resolution) plus this study (annual resolution). JRI ice core also has a melt-layer record covering 1000 - 2007 CE http://www.ncdc.noaa.gov/paleo/study/14201  +
Ant 029.temperature +Temp inferred from accumulation rate; defer to isotopes  +
Ant 031.d18O +MicS revised dating, NOAA National Climatic Data Center https://www.ncdc.noaa.gov/paleo/study/20246 (2016)  +
Ant 031dD.dD +MicS revised dating, NOAA National Climatic Data Center https://www.ncdc.noaa.gov/paleo/study/20246 (2016)  +
Arc 008.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Arc 011.d18O +QC wait for VMD  +
Arc 012.temperature +MXD record replaces the TRW; duplicate record omited from EuroMed  +
Arc 012mxd.temperature1 +MXD record replaces the TRW; duplicate record omited from EuroMed  +
Arc 016.trsgi +No low frequency;updated detrending in DArrigo et al. (2006) but data not available. Likely divergence issues but the only existing record from northeastern Siberia so it must be used to increase coverage.(FCL)  +
Arc 021.thickness +Based on studies of glacier mass balance and glaciology in Iceland (e.g. Bjornsson; Flowers), Icelandic glacier fluctuations are dominantly controlled by changes in melt season temperature. Glacier fluctuations influence the production and transport of eroded material and the eventual deposition of this sediment in a downstream basin (i.e. a proglacial lake). ... On short timescales (seasonal, annual, inter-annual), changes in sediment accumulation can be driven by many factors and we can all agree that identifying individual controls is messy. But on longer timescales (for example, centennial timescales, ... I would argue strongly that changes in sediment accumulation are driven by changes in glacier size. This is laid out in Larsen et al., 2011 QSR. We subsequently expanded on this initial study to: 1) include the whole Holocene (Larsen et al., 2012 QSR attached, which demonstrates a clear "8.2ka-event" signal and subsequent Neoglacial onset), and 2) by measuring varve thickness in multiple cores along a lake transect and tying the core data to seismic stratigraphy (Larsen et al. 2013 EPSL attached). This latter work demonstrates that the trends in sediment accumulation are consistent and observed throughout the lake basin. Given the available data, I feel comfortable summarizing as follows: Icelandic glacier fluctuations are dominantly controlled by summer temperature. On longer timescales, fluctuations of the Langjokull ice cap can be reconstructed from changes in mean varve thickness at glacial lake Hvitarvatn. Previous comment: QC failed: article states "sediment flux to Hvítárvatn is dominantly controlled by the integrated rate of sediment production by erosion beneath Langjökull, modulated on annual to decadal timescales by the efficiency of the subglacial fluvial sediment delivery system.", variability function of proximity, absolute values function of sediment availability. This is _not_ temperature!; QQ by PF not passed  +
Arc 023.trsgi +QC under question. Very weak correlation to temperature and not well described in the literature (FCL)  +
Arc 024.thickness +Valid only for > 3yr time scales  +
Arc 025.X radiograph dark layer +Time series truncated at 1800 CE. Actual measurement is not the thickness of the organic-rich layer as stated in orignial data citation. Instead, a measure of organic content within a year is estimated by the cumulative sum of the dark component of pixels of radiographs for each varve\  +
Arc 026.d18O +Low frequency  +
Arc 032.d18O +Low frequency  +
Arc 033.d18O +Low frequency  +
Arc 034.d18O +Low frequency  +
Arc 036.temperature +multi-decadal MAT, 50-year or so averages of exactly dated historical documentary information. A hiatus in the 15th and part of the 16th centuries (FCL)  +
Arc 040.temperature +Mind dating uncertainty  +
Arc 043.d18O +Fisher et al report episodic scouring of winter snow, some random warm bias in the isotopic signal  +
Arc 044.d18O +Fisher et al report episodic scouring of winter snow, some random warm bias in the isotopic signal  +
Arc 045.temperature +A newer, higher-resolution record has been published by Jiang et al. (2015, Geology: doi:10.1130/G36377.1; data at: http://www.ncdc.noaa.gov/paleo/study/17635)  +
Arc 053.temperature +QC under question, negative correlation to local temperature (FCL), should be negative accoriding to NickMcKay, keep it.  +
Arc 057.density +Δdensity = MXD - minimum density, more focused summer temp. signal than MXD (Björklund et al., 2014, CP, doi:10.5194/cp-10-877-2014)  +
Arc 058.density +Δdensity = MXD - minimum density, more focused summer temp. signal than MXD (Björklund et al., 2014, CP, doi:10.5194/cp-10-877-2014)  +
Arc 059.density +Δdensity = MXD - minimum density, more focused summer temp. signal than MXD (Björklund et al., 2014, CP, doi:10.5194/cp-10-877-2014)  +
Arc 060.density +Δdensity = MXD - minimum density, more focused summer temp. signal than MXD (Björklund et al., 2014, CP, doi:10.5194/cp-10-877-2014)  +
Arc 065.d18O +Use Arc_66 (same location, other variable)  +
Arc 073.temperature +Mind dating uncertainty  +
Arc 075.thickness +Use calibrated temperatures instead of varve thickness  +
Arc 078.temperature +strong correlation. However, opposite long-term (orbital) trend to most other Arctic records (FCL)  +
Arc 093.trsgi +Strong sign-to-noise ratio in the mean divergence-free regional chronology (representing a network of 29 sites in the Mackenzie Delta region) with Expressed Population Signal (EPS) > 0.85 since AD 1400, and EPS > 0.7 back to AD 1245. The chronology shares a moderate to strong positive correlation with local summer temperatures (r = 0.6, p < 0.001) over the calibration period, and moderate to strong correlations with several other reconstructions from surrounding regions spanning the last millenium.  +
Arc 096.d18O +Rejected - not 300 years long  +
Arc 100.temperature +replaces Esper 2002 and Briffa2008  +
Arc 150.MXD +This MXD chronology supersedes Arc_019  +
Asia 049.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 050.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 051.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 052.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 053.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 054.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 055.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 056.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 057.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 058.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 059.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 060.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 061.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 067.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 068.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 069.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 070.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 071.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 074.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 075.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 076.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 077.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 078.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 079.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 080.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 081.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 082.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 083.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 084.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 085.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 087.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 089.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 090.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 091.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 093.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 096.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 098.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 099.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 101.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 102.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 125.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 126.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 127.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 129.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 130.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 134.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 135.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 144.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 150.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 151.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 152.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 153.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 154.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 155.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 156.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 157.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 158.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 163.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 164.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 165.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 166.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 167.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 168.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 169.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 170.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 171.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 172.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 173.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 174.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 175.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 176.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 177.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 178.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 179.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 180.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 181.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 182.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 184.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 185.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 186.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 187.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 188.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 189.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 190.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 202.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 206.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 207.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 208.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 209.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 214.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 215.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 216.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 217.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 218.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 222.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 223.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 224.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 225.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 230.temperature +Half-centennial resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 233.trsgi +Not a temperature proxy  +
Asia 235.temperature +Temperature history of Kunashir Island based on the joint borehole temperature and tree-ring data. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 236.d18O +Oxygen isotopes show positive correlation with NH temperature anomalies. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 237.dust +Hydro climate  +
Asia 247.d18O +d18O in ice core in northern Tibetan Plateau is a proxy of temperature. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 305.d18O +d18O in ice core in northern Tibetan Plateau is a proxy of temperature. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 317.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 318.temperature +decadal resolution  +
Asia 319.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 320.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 321.temperature +decadal resolution  +
Asia 324.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 325.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 326.temperature +decadal resolution  +
Asia 327.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 328.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 329.temperature +decadal resolution  +
Asia 335.temperature +Species response to winter SST proved using redundancy analysis  +
Aus 010.trsgi +Warm season T signal. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 015.trsgi +Composite series, spring T signal. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 020.trsgi +Composite series, primarily winter T signal. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 041.temperature +Calibrated temperature reconstruction from 2006 JQS paper. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 057.temperature +Calibrated temperature reconstruction from 2006 JQS paper. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 062.trsgi +composite series, warm season T signal, elevation range 210-1060 m, approximate average/centroid values entered in elevation, lat and lon fields for completeness  +
Aus 067.trsgi +composite series, warm season T signal, approximate average/centroid values entered in elevation, lat and lon fields for completeness  +
Aus 071.trsgi +warm season T signal  +
C
Can1101.trsgi +Data directly taken from 2013 NatGeo paper, already shifted by 1 year to match seasonality, RCS detrending  +
E
Eur 001.d18O +The uppermost point marks the present-day conditions in Spannagel at +1.8C and y18O= 7.8x. The average temperature in the Alps during the coldest period between 1688 and 1698 coincided with the Maunder Minimum. As derived from Luterbacher's data the average temperature in this period was 1.0 (F0.5) 8C about 1.8 8C lower than in the period between 1995 and 1998.  +
Eur 002.temperature +We used multiple linear regression (MLR) to establish a calibration model that explains 84% of the variance of summer (JJAS) temperature during the calibration period 1864_1950. We then applied the calibration model downcore to develop a quantitative summer temperature reconstruction extending back to AD 1177.  +
Eur 003.temperature +The average inferred July temperatures between ca 1900 and 2001 AD were significantly warmer (p < 0.05) than the climate reference period (1961-1990) by 1C which is in agreement with the instrumental data. The inferred July temperatures were in the same range as the inferred temperatures during the last part of the MCA suggesting that during the 20th century at Lake Silvaplana the chironomid-inferred temperatures do not exceed the natural climate variability of the past millennium.  +
Eur 005.temperature +Calibrating and verifying the MXD chronologies against the instrumental temperature data showed a promising opportunity to reconstruct warm-season (May through September) temperature variability  +
Eur 006.temperature +By refining dendroclimatological methods the time-series were composited to a mean series and calibrated (1756_1841; r2 = 66%) against Stockholm January_April temperatures.  +
Eur 007.temperature +When compared to local and regional instrumental records since ca 1760 AD significant (p < 0.01) relationships (rPearson > 0.5) are obtained suggesting that chironomids accurately register the changes in temperature for the past ca 250 years  +
Eur 008.d18O +The positive correlation between 013C series of the stalagmites and the surface temperature series shown in the previous section is robust in the three samples but requires some further discussion.  +
Eur 009.d18O +Here we reconstruct thermocline temperature and salinity in this region from AD 818 to 1780 using paired _18O and Mg/Ca ratio measurements of foraminifer shells from a subdecadally resolved marine sediment core.  +
Eur 010.temperature +SST determinations based on the alkenone index UK37 indicate annual upwelling in tensity as the determinant factor for SST variability confirming the Tagus results (Abrantes et al. 2009)  +
Eur 014.MXD +The final reconstruction (N-scan) was calibrated against regional JJA temperature (r 1876_2006 = 0.77) and spans the 138 bc_ ad 2006 period.  +
Eur 016.trsgi +Using AD 1901_1950 as the calibration period the Pearson's correlation coefficient between grid data and reconstruction is 0.34 and for verification is 0.47  +
Eur 017.trsgi +This composite record includes living trees historical timber and subfossil wood and correlates at 0.72 to 0.92 with interannual to multidecadal variations in instrumental June-to-August (JJA) temperature (1864_2003)  +
Eur 018.MXD +Instrumental measurements from high- (low-) elevation grid boxes back to 1818 (1760) reveal strongest growth response to current-year June_September mean temperatures. The reconstruction correlates at 0.7 with high-elevation temperatures back to 1818 with a greater signal in the higher-frequency domain (r 0.8).  +
Eur 019.trsgi +While the highest correlation of 0.53 is gained from the HISTALP southwest subset significantly lower correlation of 0.27 originates from the low-resolution HadCRUT3v data (Brohan et al. 2006) both against June_August temperature means.  +
Eur 020.trsgi +Regional chronologies based on nested PCs display high correlation coefficients in the two calibration periods: both regression-calibrated (r1900_1952 = 0.81 and r1953_2005 = 0.75 on average) and scaling-calibrated (r1900_1952 = 0.73 and r1953_2005 = 0.80 on average). Similarly REs are also high (well above 0) for the two verifications.  +
Eur 022.temperature +For overlapping period (1760-1854) the documentary data series correlate with instrumental temperatures most strongly in winter (86% explained variance in January) and least in autumn (56% in September). For annual average temperatures 81% of the variance is explained. Elevation estimated from GoogleEarth; rounded to 100 m  +
Eur 023.sampleID +Excluded related to sample information and error estimates  +
Eur 025.uncertainty temperature +Excluded related to sample information and error estimates  +
Eur 026.temperature +In order to extend the Tallinn temperature series backward in time three different climate proxies were used. These were: the first day of ice break-up in Tallinn port a proxy for the mean winter air temperature (December to March); the first day of ice break-up on the rivers in northern Estonia a proxy for the beginning of spring; and the first day of the rye harvest a proxy for the mean air temperature in spring and summer (April to July). On the basis of these proxies the mean winter temperature could be extended back to the year AD 1500 and the spring and summer temperature back to 1731.  +
Eur 027.JulianDay +The temperature reconstruction is preferred from this site  +
L
LPD016ef221.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Dataset contains NaN values and datapoints whose chronology is not QC'd  +
LPD027eca7f.Uk37 +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD09e5a770.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDa03ec713  +
LPD0d8fd260.calcification7 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD0e0867fe.temperature +HVM, BM, 20/4/2016 Mediterranean1572bNieto-Moreno2012__TTR17-1_436B  +
LPD1079b4bb.calcification4 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD10e9f8f7.temperature +HVM, BM, 20/4/2016 Mediterranean1157abMoreno2012_MINMC-2_MINMC-1_alk(Muller) The higher-resolution alkenone record was selected. The authors also note that the G. bulloides Mg/Ca records spring upwelling SSTs whereas alkenones represent annual average SSTs. Alkenone data were measured in two cores (MINMC06-1 and MINMC06-2) from the same site. These two records were combined with the data sorted based on age.  +
LPD13a78f9b.temperature +HVM, BM, 20/4/2016 Atlantic0488Kuhnert2011__ GeoB9501-5_Mg/Ca(Anand) Combination of data from GeoB 9501–4 and GeoB 9501–5. Data combined based on age sort order.  +
LPD16c5b9d8.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Dataset contains two records that have not been combined and whose chronology has not been QC'd  +
LPD17d4c9be.notes +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD1a0245b7.temperature +HVM, BM, 20/4/2016 Pacific0185Stott2007_MD98-2181 WDC-paleoclimatology Data Contribution Series # 2007-092 Readme for Stott et al., (2007) notes calibration with Anand et al., (2003).  +
LPD1b77c35b.notes +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD21b789e2.calcification1 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD24dd89b2.composite +Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8  +
LPD2757d69f.calcification4 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD2a3997a7.temperature +HVM, BM, 20/4/2016 Southern0483aShevenell2011_ODP 1098B We used the publically archived data from PANGAEA, dated 2011.  +
LPD2d0bd641.Mg Ca +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD30c5b95c.temperature +HVM, BM, 20/4/2016 Pacific1577Newton2011_MD98-2177 Data archived as Mg/Ca values only. Data converted to SST using the calibration of Dekens et al., (2002), as per the original publication.  +
LPD3100fe0a.composite +Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8  +
LPD335d863f.RABD660 670 +annual T signal is negative (note erratum to original paper). Relative absorption band depth from 660 to 670 nm is a proxy for concentration of chlorophyll a and its derivatives. Note data gap.  +
LPD33714919.calcification2 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD34478ed4.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Dataset not combined with secondary core  +
LPD35442a44.Uk37 +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD378db911.composite +Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8  +
LPD3c013e70.core +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD41213ce8.calcification2 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD4204e2f2.Mg Ca +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD44c75538.Mg Ca +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD44e382ee.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Dataset contains NaN values and datapoints whose chronology is not QC'd  +
LPD4dd77d54.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Dataset contains NaN values and datapoints whose chronology is not QC'd  +
LPD5024de7f.calcification6 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD572f7cc3.temperature +HVM, BM, 20/4/2016 Atlantic0372Richey2007__Pigmy Basin_Mg/Ca  +
LPD57d40973.temperature +HVM, BM, 20/4/2016 Atlantic0043bRichey2009__Fisk_PE07-5I_Mg/Ca  +
LPD5c89a1b5.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Contains datapoints that are not chronologically tied according to the globbal temperature dataset criteria; furthermore contains NaN values as well  +
LPD6315f935.temperature +HVM, BM, 20/4/2016 Southern1159aSepulveda2009_CF7-PC33  +
LPD692315c3.ageMax +yearOld_AD  +
LPD6997b626.Uk37 +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD6c1fc0ed.calcification2 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD6dbf8788.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Separate cores not combined in this dataset; Not QC  +
LPD70878a8b.calcification1 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD708fb697.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDe51d17e8  +
LPD716b88d0.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Contains NaN values  +
LPD72b1e1cd.calcification1 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD7311e829.calcification4 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD7457ad38.calcification4 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD74bc6584.calcification5 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD775e8bad.year old +The timescale for the Common Era of WDC06A was recently revised. The former timescale (“WDC06A-7”, Sigl et al., 2013) was based on manually interpreting annual-layers with multi-parameter aerosol records and was used in PAGES 2k Consortium (2013). This timescale is now replaced by a timescale (“WD2014”) based on the same aerosol datasets, but interpreted with an objective layer-counting algorithm and constrained with a distinctive, global-scale, marker horizon in 775 AD detected by annual 10Be ice-core measurements (see additional details in Sigl et al., 2015). During the first millennium WD2014 differs from WDC06A-7 by on average 7 years (maximum of 9 years), with the revised timescale giving always younger ages. The time period 1258 AD to present is identical for both timescales. WD2014 is considered more accurate than WDC06A-7 (Sigl et al., 2015), and is the recommended timescale, but both timescales are reported in the PAGES2k database Ant_031 and Ant_031WD2014.  +
LPD796b99d7.calcification2 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD7be6185d.calcification1 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD7c7e19c5.temperature +HVM, BM, 20/4/2016 Atlantic0326aLund2006_MgCa_MC125_GreatBahamaBank  +
LPD7cf4e05b.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPD2a3997a7  +
LPD7d948e2c.calcification3 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD7e8e8eaa.temperature +HVM, BM, 20/4/2016 Pacific0291Newton2011_MD98-2160 Data archived as Mg/Ca values only. Data converted to SST using the calibration of Dekens et al., 2002, as per the original publication  +
LPD7fd5bd52.Uk37 +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD806644b2.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Contains datapoints with time resolution larger than 200 years  +
LPD81e7ab49.calcification1 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD8248269c.Mg Ca +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD84ab67b9.temperature +HVM, BM, 20/4/2016 Atlantic0487McGregor2007__GeoB6008-1, GeoB6008-2_ alkenone(Prahl et al., 1988)  +
LPD87328d97.TEX86 +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD8bd4e07e.composite +Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8  +
LPD8c7da1f7.Mg Ca +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD97433e99.Mg Ca +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD9b023bc9.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDf7bace53  +
LPD9c86dbd0.Uk37 +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD9cc3baf6.temperature +HVM, BM, 20/4/2016 Atlantic0316Weldeab2007__MD03-2707_Mg/Ca  +
LPDa03ec713.temperature +HVM, BM, 20/4/2016 Atlantic0255aSaenger2011__CH07-98-MC22_Mg/Ca(Anand) Atlantic0255bSaenger2011__KNR140_2_59GGC_Mg/Ca(Anand)  +
LPDa2107e77.temperature +HVM, BM, 20/4/2016 Atlantic0255bSaenger2011__KNR140_2_59GGC_Mg/Ca(Anand)  +
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