TY - JOUR
T1 - SISALv3
T2 - A global speleothem stable isotope and trace element database
AU - SISAL Working Group members
AU - Kaushal, Nikita
AU - Lechleitner, Franziska A.
AU - Wilhelm, Micah
AU - Azennoud, Khalil
AU - Bühler, Janica C.
AU - Braun, Kerstin
AU - Brahim, Yassine Ait
AU - Baker, Andy
AU - Burstyn, Yuval
AU - Comas-Bru, Laia
AU - Fohlmeister, Jens
AU - Goldsmith, Yonaton
AU - Harrison, Sandy P.
AU - Hatvani, István G.
AU - Rehfeld, Kira
AU - Ritzau, Magdalena
AU - Skiba, Vanessa
AU - Stoll, Heather M.
AU - Szucs, József G.
AU - Tanos, Péter
AU - Treble, Pauline C.
AU - Azevedo, Vitor
AU - Baker, Jonathan L.
AU - Borsato, Andrea
AU - Chawchai, Sakonvan
AU - Columbu, Andrea
AU - Endres, Laura
AU - Hu, Jun
AU - Kern, Zoltán
AU - Kimbrough, Alena
AU - Koç, Koray
AU - Markowska, Monika
AU - Martrat, Belen
AU - Ahmad, Syed Masood
AU - Nehme, Carole
AU - Novello, Valdir Felipe
AU - Pérez-Mejías, Carlos
AU - Ruan, Jiaoyang
AU - Sekhon, Natasha
AU - Sinha, Nitesh
AU - Tadros, Carol V.
AU - Tiger, Benjamin H.
AU - Warken, Sophie
AU - Wolf, Annabel
AU - Zhang, Haiwei
AU - Asrat, Asfawossen
AU - Honiat, Charlotte
AU - Riechelmann, Dana Felicitas Christine
AU - Scholz, Denis
AU - Liu, Dianbing
N1 - Publisher Copyright:
© 2024 Nikita Kaushal et al.
PY - 2024/4/26
Y1 - 2024/4/26
N2 - Palaeoclimate information on multiple climate variables at different spatiotemporal scales is becoming increasingly important to understand environmental and societal responses to climate change. A lack of high-quality reconstructions of past hydroclimate has recently been identified as a critical research gap. Speleothems, with their precise chronologies, widespread distribution, and ability to record changes in local to regional hydroclimate variability, are an ideal source of such information. Here, we present a new version of the Speleothem Isotopes Synthesis and AnaLysis database (SISALv3), which has been expanded to include trace element ratios and Sr isotopes as additional, hydroclimate-sensitive geochemical proxies. The oxygen and carbon isotope data included in previous versions of the database have been substantially expanded. SISALv3 contains speleothem data from 365 sites from across the globe, including 95 Mg/Ca, 85 Sr/Ca, 52 Ba/Ca, 25 U/Ca, 29 P/Ca, and 14 Sr-isotope records. The database also has increased spatiotemporal coverage for stable oxygen (892) and carbon (620) isotope records compared with SISALv2 (which consists of 673 and 430 stable oxygen and carbon records, respectively). Additional meta information has been added to improve the machine-readability and filtering of data. Standardized chronologies are included for all new entities along with the originally published chronologies. Thus, the SISALv3 database constitutes a unique resource of speleothem palaeoclimate information that allows regional to global palaeoclimate analyses based on multiple geochemical proxies, permitting more robust interpretations of past hydroclimate and comparisons with isotope-enabled climate models and other Earth system and hydrological models. The database can be accessed at 10.5287/ora-2nanwp4rk (Kaushal et al., 2024).
AB - Palaeoclimate information on multiple climate variables at different spatiotemporal scales is becoming increasingly important to understand environmental and societal responses to climate change. A lack of high-quality reconstructions of past hydroclimate has recently been identified as a critical research gap. Speleothems, with their precise chronologies, widespread distribution, and ability to record changes in local to regional hydroclimate variability, are an ideal source of such information. Here, we present a new version of the Speleothem Isotopes Synthesis and AnaLysis database (SISALv3), which has been expanded to include trace element ratios and Sr isotopes as additional, hydroclimate-sensitive geochemical proxies. The oxygen and carbon isotope data included in previous versions of the database have been substantially expanded. SISALv3 contains speleothem data from 365 sites from across the globe, including 95 Mg/Ca, 85 Sr/Ca, 52 Ba/Ca, 25 U/Ca, 29 P/Ca, and 14 Sr-isotope records. The database also has increased spatiotemporal coverage for stable oxygen (892) and carbon (620) isotope records compared with SISALv2 (which consists of 673 and 430 stable oxygen and carbon records, respectively). Additional meta information has been added to improve the machine-readability and filtering of data. Standardized chronologies are included for all new entities along with the originally published chronologies. Thus, the SISALv3 database constitutes a unique resource of speleothem palaeoclimate information that allows regional to global palaeoclimate analyses based on multiple geochemical proxies, permitting more robust interpretations of past hydroclimate and comparisons with isotope-enabled climate models and other Earth system and hydrological models. The database can be accessed at 10.5287/ora-2nanwp4rk (Kaushal et al., 2024).
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U2 - 10.5194/essd-16-1933-2024
DO - 10.5194/essd-16-1933-2024
M3 - Article
AN - SCOPUS:85192445958
SN - 1866-3508
VL - 16
SP - 1933
EP - 1963
JO - Earth System Science Data
JF - Earth System Science Data
IS - 4
ER -