<?xml version="1.0" encoding="ISO-8859-1"?>

<metadata>
<idinfo>
<citation>
<citeinfo>
<origin>
Thomas Felis
</origin>
<origin>
JÃ¼rgen PÃ¤tzold
</origin>
<origin>
Gerold Wefer
</origin>
<pubdate>
2000/12
</pubdate>
<title>
Ras Umm Sidd Oxygen Isotope (delta 18O) Data for 1750 to 1995
</title>
<serinfo>
<sername>
World Data Center for Paleoclimatology Data Contribution Series
</sername>
<issue>
2000-067
</issue>
</serinfo>
<pubinfo>
<pubplace>
Boulder
</pubplace>
<publish>
World Data Center for Paleoclimatology, Boulder
</publish>
</pubinfo>
</citeinfo>
</citation>
<descript>
<abstract>
Ras Umm Sidd bimonthly coral oxygen isotope data (coral core RUS-95). Notes on the data: File (Ras Umm Sidd d18O.txt.) includes columns for Year AD (bimonthly resolution: Jan-Feb, Mar-Apr, May-Jun, etc.) and coral d18O in per mil relative to the Vienna peedee belemnite (VPDB) reference standard. The coral core was collected in the end of November 1995 in the northern Red Sea at Ras Umm Sidd (27Â°50.9&apos;N, 34Â°18.6&apos;E) in the Ras Mohammed National Park near the southern tip of the Sinai Peninsula (Egypt), from a 2.6-m-high coral colony (Porites sp.) growing at a water depth of ~5.5 m. The average annual growth rate of the coral is 1 cm/year. The average sampling resolution for oxygen isotope analysis is more than 6 samples per year. Oxygen isotope analysis was performed on a Finnigan MAT 251 mass spectrometer coupled to an automated carbonate device at the stable isotope laboratory of the Department of Geosciences at Bremen University, Germany. Long-term reproducibility for d18O, deduced from replicate measurementsof an internal carbonate standard, is better than Â±0.07 per mil. The coral chronology is constructed by setting the maximum d18O value in a given year equal to mid-February (consistent with the climatological minimum in sea surface temperature) and assuming a constant coral growth rate between February of every year. Therefore we interpolated linearly between these fixed points for further age assignments. The resulting values were interpolated linearly to six equally spaced values per year, providing a bimonthly resolution. The strong seasonal cycle in d18O was used to count annual layers in the coral, supported by the consistent density banding pattern of low-density band creation during winter and high-density band creation during summer. The coral record extends from fall 1750 to fall 1995. We assigned an age model error of at least 2-3 months to the coral chronology. In addition, we assigned an age model error of Â±1 year to the interval 1924-1783 and an additional Â±1 year to 1782-1750. Therefore the chronology is assigned a cumulative age model error of less than Â±3 years at the bottom of the core.  More information on the Ras Umm Sidd coral oxygen isotope record can be found in the original reference.
</abstract>
<purpose>
Paleoclimatic Research
</purpose>
<noaainfo>
<entry>
G2091
</entry>
<center>
National Geophysical Data Center
</center>
<nsurls>
<moreinfo>
http://www.ngdc.noaa.gov/paleo/corals.html
</moreinfo>
</nsurls>
<onlsiz>
1
</onlsiz>
</noaainfo>
</descript>
<timeperd>
<timeinfo>
<rngdates>
<begdate>
1750
</begdate>
<enddate>
1995
</enddate>
</rngdates>
</timeinfo>
<current>
Publication Date
</current>
</timeperd>
<status>
<progress>
Complete
</progress>
<update>
None Planned
</update>
</status>
<spdom>
<bounding>
<westbc>
34.31
</westbc>
<eastbc>
34.31
</eastbc>
<northbc>
27.85
</northbc>
<southbc>
27.85
</southbc>
</bounding>
</spdom>
<keywords>
<theme>
<themekt>
CoRIS Theme Keywords Version 1.0
</themekt>
<themekey>
EARTH SCIENCE &gt; Paleoclimate  &gt; Coral Records &gt; delta 18O
</themekey>
<themekey>
EARTH SCIENCE &gt; Paleoclimate  &gt; Coral Records &gt; density
</themekey>
<themekey>
EARTH SCIENCE &gt; Paleoclimate  &gt; Coral Records &gt; linear extension rate
</themekey>
<themekey>
Numeric Data Sets &gt; Paleoclimatology
</themekey>
</theme>
<place>
<placekt>
CoRIS Place Keywords Version 1.0
</placekt>
<placekey>
COUNTRY/TERRITORY &gt; Egypt &gt; Ras Um Sid (27N034E0003)
</placekey>
<placekey>
OCEAN BASIN &gt; Indian Ocean &gt; Red Sea &gt; Sharm el Sheikh &gt; Ras Um Sid (27N034E0003)
</placekey>
</place>
<temporal>
<tempkt>
CoRIS Temporal Keywords Version 1.0
</tempkt>
<tempkey>
Holocene, Modern
</tempkey>
</temporal>
</keywords>
<accconst>
None
</accconst>
<useconst>
PLEASE CITE ORIGINAL REFERENCE WHEN USING THIS DATA
</useconst>
<datacred>
Felis, T., J. Pätzold, Y. Loya, M. Fine, A. H. Nawar, and G. Wefer, 2000, A coral oxygen isotope record from the northern Red Sea documenting NAO, ENSO, and North Pacific teleconnections on Middle East climate variability since the year 1750. Paleoceanography, 15, 679-694.
</datacred>
</idinfo>
<eainfo>
<detailed>
<enttyp>
<enttypl>
coral variable
</enttypl>
<enttypd>
coral variable
</enttypd>
<enttypds>
coral variable
</enttypds>
</enttyp>
<attr>
<attrlabl>
del18O
</attrlabl>
<attrdef>
delta 18O (per mil) relative to PDB
</attrdef>
<attrdefs>
Craig, H., 1957.  Isotopic standards for mass spectrometric analysis of carbon dioxide.  Geochimica Cosmochimica Acta, 12:113-140
</attrdefs>
<attrdomv>
<rdom>
<rdommin>
unknown
</rdommin>
<rdommax>
unknown
</rdommax>
<attrunit>
per mil
</attrunit>
<attrmres>
0.01
</attrmres>
</rdom>
</attrdomv>
</attr>
</detailed>
</eainfo>
<distinfo>
<distrib>
<cntinfo>
<cntorgp>
<cntorg>
NOAA Paleoclimatology Program
</cntorg>
<cntper>
Bruce Bauer
</cntper>
</cntorgp>
<cntpos>
Data Manager
</cntpos>
<cntaddr>
<addrtype>
Mailing Address
</addrtype>
<address>
325 Broadway, E/GC
</address>
<city>
Boulder
</city>
<state>
CO
</state>
<postal>
80305-3328
</postal>
<country>
U.S.A.
</country>
</cntaddr>
<cntvoice>
(303) 497-6160
</cntvoice>
<cnttdd>
(303) 497-6958
</cnttdd>
<cntfax>
(303) 497-6513
</cntfax>
<cntemail>
paleo@ngdc.noaa.gov
</cntemail>
<hours>
9-5 MST Monday-Friday
</hours>
</cntinfo>
</distrib>
<distliab>
Disclaimer- While every effort has been made to ensure that these data are accurate and reliable within the limits of the current state of the art, NOAA cannot assume liability for any damages caused by any errors or omissions in the data, nor as a result of the failure of the data to function on a particular system.  NOAA makes no warranty, expressed or implied, nor does the fact of distribution constitute such a warranty.
</distliab>
<stdorder>
<digform>
<digtinfo>
<formname>
ASCII
</formname>
</digtinfo>
<digtopt>
<onlinopt>
<computer>
<networka>
<networkr>
ftp://ftp.ngdc.noaa.gov/paleo/coral/red_sea/ras_um_sid_2000.txt
</networkr>
<networkr>
ftp://ftp.ngdc.noaa.gov/paleo/coral/red_sea/ras_um_sid_2000.xml
</networkr>
</networka>
</computer>
<accinstr>
Data can be obtained from http://www.ngdc.noaa.gov/paleo and via anonymous ftp to ftp.ngdc.noaa.gov.  Diskette and paper copies may be obtained by mail.
</accinstr>
</onlinopt>
<offoptn>
<offmedia>
Diskette
</offmedia>
<recfmt>
cpio
</recfmt>
</offoptn>
</digtopt>
</digform>
<fees>
On-line data are available free of charge, other forms are available for the cost of reproduction
</fees>
<ordering>
Contact the Data Center to order paper copies of data
</ordering>
<turnarnd>
4 days
</turnarnd>
</stdorder>
</distinfo>
<metainfo>
<metd>
20010816
</metd>
<metc>
<cntinfo>
<cntorgp>
<cntorg>
NOAA Paleoclimatology Program
</cntorg>
<cntper>
Carissa Carter
</cntper>
</cntorgp>
<cntaddr>
<addrtype>
Mailing Address
</addrtype>
<address>
325 Broadway, EGC
</address>
<city>
Boulder
</city>
<state>
Colorado
</state>
<postal>
80305-3328
</postal>
<country>
United States
</country>
</cntaddr>
<cntvoice>
(303) 497-6160
</cntvoice>
<cnttdd>
(303) 497-6958
</cnttdd>
<cntfax>
(303) 497-6513
</cntfax>
<cntemail>
carissa.l.carter@noaa.gov
</cntemail>
</cntinfo>
</metc>
<metstdn>
FGDC Content Standard for Digital Geospatial Metadata
</metstdn>
<metstdv>
FGDC-STD-001-1998
</metstdv>
<metac>
No Constraints
</metac>
<metuc>
No Constraints
</metuc>
</metainfo>
</metadata>