Ã¯Â»Â¿# Bermuda Coral Isotope and Skeletal Density Data
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#                World Data Center for Paleoclimatology, Boulder 
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#                     NOAA Paleoclimatology Program 
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# 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. 
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# Online_Resource: 
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# Online_Resource: https://www.ncdc.noaa.gov/paleo/study/24611
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# Original_Source_URL: 
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# Description/Documentation lines begin with #
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# Archive: Corals and Sclerosponges
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# Contribution_Date
#	Date: 2015-11-11
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# Title
#	Study_Name: Bermuda Coral Isotope and Skeletal Density Data
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# Investigators
#       Investigators: Draschba, S.; Patzold, J.; Wefer, G.
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# Description_and_Notes
#	Description: 
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# Publication 
#       Authors: Draschba, S.; Patzold, J.; Wefer, G.
#       Published_Date_or_Year: 2000
#       Published_Title: North Atlantic climate variability since AD 1350 recorded in ÃÂ´ 18O and skeletal density of Bermuda corals
#       Journal_Name: International Journal of Earth Sciences
#       Volume: 88
#       Edition: 
#       Issue: 4
#       Pages: 733-741
#       DOI: 10.1007/s005310050301
#       Online_Resource: http://link.springer.com/article/10.1007%2Fs005310050301
#       Full_Citation: 
#       Abstract: The reconstruction of the climatic history during the past several hundred years requires a sufficient geographical coverage of combined climate proxy series. Especially in order to identify causal connections between the atmosphere and the ocean, inclusion of marine records into composite climate time series is of fundamental importance. We present two skeletal ÃÂ´ 18O chronologies of coral skeletons of Diploria labyrinthiformis from Bermuda fore-reef sites covering periods in the nineteenth and twentieth centuries and compare them with instrumental temperature data. Both time series are demonstrated to display sea-surface temperature (SST) variability on inter-annual to decadal time scales. On the basis of a specific modern ÃÂ´ 18O vs instrumental SST calibration we reconstruct a time series of SST anomalies between AD 1350 and 1630 covering periods during the Little Ice Age. The application of the coral ÃÂ´ 18O vs temperature relationship leads to estimates of past SST variability which are comparable to the magnitude of modern variations. Parallel to ÃÂ´ 18O chronologies we present time series of skeletal bulk density. Coral ÃÂ´ 18O and skeletal density reveal a strong similarity during Little Ice Age, confirming the reliability of both proxy climate indicators. The past coral records, presented in this study, share features with a previously published climate proxy record from Bermuda and a composite time series of reconstructed Northern Hemisphere summer temperatures. The coral proxy data presented here represent a valuable contribution to elucidate northern Atlantic subtropical climate variation during the past several centuries.
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#	Authors: Anderson, D.M., Tardif, R., Horlick, K., Erb, M.P., Hakim, G.J., Noone, D., Perkins, W.A., and E. Steig
#	Published_Date_or_Year: 2018
#	Published_Title: Additions to the last millennium reanalysis multi-proxy database
#	Journal_Name: Data Science Journal
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#	Full_Citation: Anderson, D.M., Tardif, R., Horlick, K., Erb, M.P., Hakim, G., J., Noone, D., Perkins, W.A., and E. Steig, submitted. Additions to the last millennium reanalysis multi-proxy database. Data Science Journal.
#	Abstract: Progress in paleoclimatology increasingly occurs via data syntheses. We describe additions to a collection prepared for use in paleoclimate state estimation, specifically the Last Millennium Reanalysis (LMR).  The 2290 additional series include 2152 tree ring chronologies and 138 other series.  They supplement the collection used previously and together form a database titled LMRdb 1.0.0. The additional data draws from lake core, ice core, coral, speleothem, and tree ring archives, using published data primarily from the NOAA Paleoclimatology archive and a set of tree ring width chronologies standardized from raw International Tree Ring Data Bank ring width series. In contrast to many previous paleo compilations, the data were not selected (screened) on the basis of their environmental correlation, multi-century length, or other attributes. The inclusion of proxies sensitive to moisture and other environmental variables expands their use in data assimilation.  A preliminary calibration using linear regression with mean annual temperature reveals characteristics of the proxy series and their relationship to temperature, as well as the noise and error characteristics of the records. The additional records are structured as individual files in the NOAA Paleoclimatology format and archived at NOAA Paleoclimatology (Anderson et al. 2018) and will continue to be improved and expanded as part of the LMR Project.  The additions represent a four-fold increase in the number of records available for assimilation, provide expanded geographic coverage, and add additional proxy variables.  Applications include data assimilation, proxy system model development, and paleoclimate reconstruction using climate field reconstruction and other methods.
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# Funding_Agency 
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#       Grant: 
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#	Funding_Agency_Name: National Science Foundation
#	Grant:AGS-1304263
#	Funding_Agency_Name: National Oceanic and Atmospheric Administration
#	Grant:NA14OAR4310176
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# Site_Information 
#       Site_Name: Northeast Breakers, Bermuda 
#       Location: Ocean>Atlantic Ocean>North Atlantic Ocean>Bermuda
#	Country: Bermuda  
#	Northernmost_Latitude: 32.33 
# 	Southernmost_Latitude: 32.33 
# 	Easternmost_Longitude: -64.75 
# 	Westernmost_Longitude: -64.75 
# 	Elevation: -25 m  
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# Data_Collection   
#	Collection_Name: 00berm01b 
#	Earliest_Year: 1856
#	Most_Recent_Year: 1920
#	Time_Unit: y_ad
#	Core_Length: 
#	Notes: {"database":"LMR"} 
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# Species
#	Species_Name: Diploria labyrinthiformis 
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# Chronology: 
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# Variables 
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# 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) 
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##age	age, , ,y_ad, , Corals and Sclerosponges, , ,N
##d18O	delta 18 Oxygen, Diploria labyrinthiformis, , permil VPDB, , Corals and Sclerosponges, , Mass spectrometer Finnigan MAT 251,N
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# Data:
# Data lines follow (have no #)
# Data line format - tab-delimited text, variable short name as header
# Missing Values: NAN
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age	d18O
1920	-3.22
1917	-3.28
1915	-2.93
1911	-2.76
1908	-3.04
1905	-2.96
1902	-2.85
1900	-3.02
1897	-3.17
1894	-3.24
1891	-2.82
1888	-3.24
1885	-3.13
1881	-3.06
1878	-2.83
1875	-3.18
1872	-3.35
1870	-3.45
1868	-3.24
1865	-2.92
1862	-3.24
1859	-2.95
1856	-2.69