Norway-Swiss calibration dataset (Heiri et al. 2011)

eSEP (estimated standard error of prediction)

mixed-effect regression within the framework of generalized additive modelling

Arctostaphylus uva-ursi leaves, terr. seed

reliable (R2hcWIkKwzm): paleoData_proxyGeneral: '' has been replaced by 'chironomid'
uncertainty (RxBmcyei4Yh): paleoData_proxyGeneral: '' has been replaced by 'chironomid'
uncertainty (RzqdPKxhlqI): paleoData_proxyGeneral: '' has been replaced by 'chironomid'

Samartin, S.; Heiri, O.; Joos, F.; Renssen, H.; Franke, J.; Broennimann, S.; Tinner, W.

Warm Mediterranean mid-Holocene summers inferred from fossil midge assemblages

Agilent 720 Inductively Coupled Plasma Optical Emission Spectrometer

youngest = 4.2 ka, but passes resolution & chronology; PMS: the SST could also be wind driven upwelling

SST calculated from Mg/Ca (TSid=RL64xxOUoVT) using the BAYMAG program baymag_predict.  Parameters: omega=1.1352, clean=0, 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 (33.5498) and pH (8.0672) for the archive location and using the ages

Using the age-depth model of GeoB 10042-1
GeoB 10042-1: (6-8 cm core depth) that has been linked to the Krakatau eruption in 1883 [Southon et al.

Using the age-depth model of GeoB 10042-1
we found a hiatus indicated by a dramatic increase in the sedimentation rate from 3.6 to 31 cm/kyr around 10 kyr B.P. associated with abrupt changes in d18O and Ti/Ca log ratio (Figure 3).
we found a hiatus indicated by a dramatic increase in the sedimentation rate from 3.6 to 31 cm/kyr around 10 kyr B.P. associated with abrupt changes in d18O and Ti/Ca log ratio (Figure 3).
we found a hiatus indicated by a dramatic increase in the sedimentation rate from 3.6 to 31 cm/kyr around 10 kyr B.P. associated with abrupt changes in d18O and Ti/Ca log ratio (Figure 3).
we found a hiatus indicated by a dramatic increase in the sedimentation rate from 3.6 to 31 cm/kyr around 10 kyr B.P. associated with abrupt changes in d18O and Ti/Ca log ratio (Figure 3).
we found a hiatus indicated by a dramatic increase in the sedimentation rate from 3.6 to 31 cm/kyr around 10 kyr B.P. associated with abrupt changes in d18O and Ti/Ca log ratio (Figure 3).
we found a hiatus indicated by a dramatic increase in the sedimentation rate from 3.6 to 31 cm/kyr around 10 kyr B.P. associated with abrupt changes in d18O and Ti/Ca log ratio (Figure 3).
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
Using the age-depth model of GeoB 10042-1
2013]