All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement; composite core depths [raw depth in core = 254 cm]; see table 1 at http://dx.doi.org/10.1016/j.quaint.2012.09.006

ID number of core used to generate composite record

core (O2kLR_185): interpretation1_scope: '' has been replaced by 'climate'

Zhao, Meixun;Eglinton, Geoffrey;Read, Gareth;Schimmelmann, Arndt

An alkenone (U37K′) quasi-annual sea surface temperature record (A.D. 1440 to 1940) using varved sediments from the Santa Barbara Basin

used in Tierney et al, as a composite with HR_156; the original records are provided here rather than composites

used in Tierney et al, as a composite with HR_157; the original records are provided here rather than composites

Savusavu Bay, Fiji oxygen isotope record 1776-2001

Bagnato, Stefan;Linsley, Braddock K.;Howe, Stephen S.;Wellington, Gerard M.;Salinger, Jim

Coral oxygen isotope records of interdecadal climate variations in the South Pacific Convergence Zone region

Secas Island, Panama isotope record 1707 - 1984

Linsley, Braddock K.;Dunbar, Robert B.;Wellington, Gerard M.;Mucciarone, David A.

A coral-based reconstruction of Intertropical Convergence Zone variability over Central America since 1707

Moustafa, Yaser Ahmed;Pätzold, Jürgen;Loya, Yossi;Wefer, Gerold

Berichte, Fachbereich Geowissenschaften, Universität Bremen

Mid-Holocene stable isotope record of corals from the northern Red Sea

HVM, BM, 20/4/2016 Atlantic0484Leduc2010_GeoB8331-4+GeoB8331-2_alkenone(Muller)_winter (upwelling) season

Leduc, Guillaume; Herbert, Caren T; Blanz, Thomas; Martinez, Philippe; Schneider, Ralph R

Sea surface temperature off West Africa based on alkenones

Uk37 (LPD027eca7f): interpretation1_scope: '' has been replaced by 'climate'
Uk37 (LPDabae85f2): interpretation1_scope: '' has been replaced by 'climate'

Leduc, Guillaume;Herbert, Caren T.;Blanz, Thomas;Martinez, Philippe;Schneider, Ralph

Contrasting evolution of sea surface temperature in the Benguela upwelling system under natural and anthropogenic climate forcings