1.

Water upwelling radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

2.

Water upwelling radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

3.

Water upwelling radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

4.

Water upwelling radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

5.

Water upwelling radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

6.

Water upwelling radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

7.

Water upwelling radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

1.

Water upwelling radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

2.

Water upwelling radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

3.

Water upwelling radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

4.

Water upwelling radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

5.

Water upwelling radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

6.

Water upwelling radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

7.

Water upwelling radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

1.

Downwelling sky radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

2.

Downwelling sky radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

3.

Downwelling sky radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

4.

Downwelling sky radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

5.

Downwelling sky radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

6.

Downwelling sky radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

7.

Downwelling sky radiance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

1.

Downwelling sky radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

2.

Downwelling sky radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

3.

Downwelling sky radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

4.

Downwelling sky radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

5.

Downwelling sky radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

6.

Downwelling sky radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

7.

Downwelling sky radiance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

1.

Water reflectance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

2.

Water reflectance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

3.

Water reflectance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

4.

Water reflectance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

5.

Water reflectance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

6.

Water reflectance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

7.

Water reflectance from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

1.

Water reflectance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

2.

Water reflectance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

3.

Water reflectance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

4.

Water reflectance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

5.

Water reflectance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

6.

Water reflectance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

7.

Water reflectance standard deviation from six different study areas (in Argentina, China, France and Belgium) measured with TRiOS

1.

SST Proxies of ODP Site 202-1234

2.

SST Proxies of ODP Site 202-1234

3.

SST Proxies of ODP Site 202-1234

1.

SST Proxies of ODP Site 202-1235

2.

SST Proxies of ODP Site 202-1235

3.

SST Proxies of ODP Site 202-1235

1.

(Table S2) Concentration of the individual and summed BHPs of the suspended particulate matter

2.

(Table S2) Concentration of the individual and summed BHPs of the suspended particulate matter

3.

(Table S2) Concentration of the individual and summed BHPs of the suspended particulate matter

1.

(Appendix 6) Concentrations of CL and IPL-derived isoGDGTs normalized to OC and BIT values for marine surface sediments

2.

(Appendix 6) Concentrations of CL and IPL-derived isoGDGTs normalized to OC and BIT values for marine surface sediments

3.

(Appendix 6) Concentrations of CL and IPL-derived isoGDGTs normalized to OC and BIT values for marine surface sediments