Paula Diz
Biographic Data
| ID | 6376046 |
|---|---|
| NAME | Paula Diz |
| GIVEN NAMES | Paula |
| FAMILY NAME | Diz |
| SIGNATURE | DIZ P |
| AFFILIATIONS | Universidade de Vigo |
| ORCID | 0000-0002-7136-0690 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 16 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2002 |
| LATEST PUBLICATION YEAR | 2006 |
| H-INDEX | 2 |
Climate change and coastal hydrographic response along the Atlantic Iberian margin (Tagus Prodelta and Muros Ría) during the last two millennia
The Tagus Prodelta (W Portugal) and the Muros Ría (NW Spain) are areas of high deposition rates registering high-resolution palaeoclimatic records for western Iberia. We compare the climatic conditions of the two areas over the last two millennia based on proxies of temperature (sea surface temperatures and oxygen isotopes), continental input (grain size, iron and magnetic susceptibility) and productivity (inorganic and organic carbon, carbon iso…
The last 3000 years in the Ría de Vigo (NW Iberian Margin)
The hydrographic evolution of the Ria de Vigo (NW Spain) during the last 3000 years has been reconstructed using benthic foraminiferal assemblages, stable oxygen isotopes, molecular biomarkers and seasurface temperatures (SST) reconstructed from the U K 37 index. Benthic oxygen isotopes and SST records provide evidence of episodic salinity contrasts between surface and bottom waters. The comparison of SSTs with other climate records for the North…
Climate change and coastal hydrographic response along the Atlantic Iberian margin (Tagus Prodelta and Muros Ría) during the last two millennia
The Tagus Prodelta (W Portugal) and the Muros Ría (NW Spain) are areas of high deposition rates registering high-resolution palaeoclimatic records for western Iberia. We compare the climatic conditions of the two areas over the last two millennia based on proxies of temperature (sea surface temperatures and oxygen isotopes), continental input (grain size, iron and magnetic susceptibility) and productivity (inorganic and organic carbon, carbon iso…
The last 3000 years in the Ría de Vigo (NW Iberian Margin)
The hydrographic evolution of the Ria de Vigo (NW Spain) during the last 3000 years has been reconstructed using benthic foraminiferal assemblages, stable oxygen isotopes, molecular biomarkers and seasurface temperatures (SST) reconstructed from the U K 37 index. Benthic oxygen isotopes and SST records provide evidence of episodic salinity contrasts between surface and bottom waters. The comparison of SSTs with other climate records for the North…
The last 3000 years in the Ría de Vigo (NW Iberian Margin)
The hydrographic evolution of the Ria de Vigo (NW Spain) during the last 3000 years has been reconstructed using benthic foraminiferal assemblages, stable oxygen isotopes, molecular biomarkers and seasurface temperatures (SST) reconstructed from the U K 37 index. Benthic oxygen isotopes and SST records provide evidence of episodic salinity contrasts between surface and bottom waters. The comparison of SSTs with other climate records for the North…
Climate change and coastal hydrographic response along the Atlantic Iberian margin (Tagus Prodelta and Muros Ría) during the last two millennia
The Tagus Prodelta (W Portugal) and the Muros Ría (NW Spain) are areas of high deposition rates registering high-resolution palaeoclimatic records for western Iberia. We compare the climatic conditions of the two areas over the last two millennia based on proxies of temperature (sea surface temperatures and oxygen isotopes), continental input (grain size, iron and magnetic susceptibility) and productivity (inorganic and organic carbon, carbon iso…
Benthic zone (2 works) · Foraminifera (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Hydrography (2 works) · Oceanography (2 works) · Upwelling (2 works) · Atlantic multidecadal oscillation (1 work) · Biogeochemical cycle (1 work) · Climate change (1 work)