SST calculated from Mg/Ca (TSid=RsGueF5Ezuc) using the BAYMAG program baymag_predict.  Parameters: omega=1.1672, clean=1, species=ruber, pstd=10, varargin=unspecified;  For salinity and pH, values are specified to change through time, and are calculated using the get_phsal program from Jess Tierney, based on modern values of salinity (34.2657) and pH (7.9461) for the archive location and using the ages

temperature (RvhBzegpmNO): paleoData_proxyGeneral: '' has been replaced by 'Mg/Ca'

Sea surface and subsurface circulation dynamics off equatorial Peru during the last ~17 kyr

Rainfall response to orbital and millennial forcing in northern Peru over the last 18 ka

species specific calibration for G. ruber of Regenberg et al. [2009].

C37:2 and C37:4; changed from C36 after asking authors

SST calculated from Uk37 (TSid=RbIuRfn9Vxz) using the BAYSPLINE program UK_predict.  Parameters: pstd=10, bayes=unspecified

temperature (Ry7Sq4X11wb): paleoData_proxyGeneral: '' has been replaced by 'Mg/Ca'

N _rnberg, Dirk; B̦schen, Tebke; Doering, Kristin; Mollier-Vogel, Elfi; Raddatz, Jacek; Schneider, Ralph

Sea surface and subsurface circulation dynamics off equatorial Peru during the last 17 kyr

meets resolution for 5ka to present; accepted to fill large spatial data gap

Variable name changed from errorPlus to 1SD during update from DKs csv files.

Variable name changed from notes to core during update from DKs csv files.

Woltering, Martijn; Atahan, Pia; Grice, Kliti; Heijnis, Henk; Taffs, Kathryn; Dodson, John

<jats:title>Abstract</jats:title><jats:p>Branched glycerol dialkyl glycerol tetraether (GDGT) distributions observed in a sediment core from Lake McKenzie were utilized to quantitatively reconstruct the pattern of mean annual air temperature (MAAT) from coastal subtropical eastern Australia between 37 and 18.3 cal ka BP and 14.0 cal ka BP to present. Both the reconstructed trend and amplitude of MAAT changes from the top of the sediment core were nearly identical to a local instrumental MAAT record from Fraser Island, providing confidence that in this sediment core branched GDGTs could be used to produce a quantitative record of past MAAT. The reconstructed trend of MAAT during 37 to 18.3 cal ka BP and timing of the Last Glacial Maximum (LGM) in the Lake McKenzie record were in agreement with previously published nearby marine climate records. The amplitude of lower-than-present MAAT during the LGM potentially provides information on the latitude of separation of the Tasman Front from the East Australian current in the subtropical western Pacific. The Lake McKenzie record shows an earlier onset of near modern day warm temperatures in the early Holocene compared to marine records and the presence of a warmer than present day period during the mid-Holocene.</jats:p>