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Thomas Blanz

Datos Biográficos

ID6374458
NOMBREThomas Blanz
NOMBRESThomas
APELLIDOBlanz
FIRMABLANZ T
AFILIACIONESInstitute of Geosciences, Kiel University, Germany
ORCID0000-0001-6955-2020
VERIFICADOSí
TOTAL DE OBRAS5
TOTAL DE CITAS26
TOTAL COMO AUTOR5
TOTAL COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN2003
AÑO MÁS RECIENTE DE PUBLICACIÓN2021
ÍNDICE H2
  • Hydrographic shifts south of Australia over the last deglaciation and possible interhemispheric linkages

    Open Access•Matthias Moros, Patrick De Deckker et al.•ARTICLE•Quaternary Research•2021

    Northern and southern hemispheric influences—particularly changes in Southern Hemisphere westerly winds (SSW) and Southern Ocean ventilation—triggered the stepwise atmospheric CO 2 increase that accompanied the last deglaciation. One approach for gaining potential insights into past changes in SWW/CO 2 upwelling is to reconstruct the positions of the northern oceanic fronts associated with the Antarctic Circumpolar Current. Using two deep-sea cor…

  • Holocene water mass changes in the Labrador Current

    Open Access•Annalena Lochte, Annalena Antonia Lochte et al.•ARTICLE•The Holocene•2019•Citada por: 1•Referencias: 17

    The Labrador Current is part of the anticlockwise subpolar gyre and plays a major role in the formation of North Atlantic Deep Water. It is influenced by the West Greenland and Baffin currents supplying warmer Atlantic and cold polar waters, respectively. During the early Holocene, at the final stage of the last deglaciation, meltwater and iceberg discharge caused highly variable conditions in the Labrador Current. In order to assess its sensitiv…

  • Regional climate change and the onset of farming in northern Germany and southern Scandinavia

    Open Access•Veronica Rohde Krossa, Matthias Moros et al.•ARTICLE•The Holocene•2017•Citada por: 3•Referencias: 23

    In Europe, the transition from hunter–gatherer–fisher-based communities into societies mainly relying on farming was spread from the southeast towards the north and west during the Holocene. In central Germany, farming was adopted at ~7500 cal. yr BP, whereas the shift is evident at ~6000–5500 cal. yr BP in northern Germany and southern Scandinavia. Consequently, farming techniques were available for more than a millennium. Some studies argue tha…

  • Centennial-scale variations in diatom productivity off Peru over the last 3000 years

    Open Access•Sophie Fleury, Xavier Crosta et al.•ARTICLE•The Holocene•2015•Citada por: 1•Referencias: 5

    The Peruvian coastal upwelling is one of the most productive systems in the global ocean, with important impacts on the carbon cycle. Primary productivity there displays strong variations at the interannual to decadal timescales. However, down-core investigations rarely reach sufficient temporal resolution to assess the response of productivity to climatic variations at these timescales beyond the instrumental and historical periods. We here anal…

  • Salinity changes in the central Baltic Sea (NW Europe) over the last 10000 years

    Open Access•Kay-Christian Emeis, Kay‐Christian Emeis et al.•ARTICLE•The Holocene•2003•Citada por: 21•Referencias: 4

    We attempt a reconstruction of salinity levels of the central Baltic Sea based on diatom assemblages, the isotopic composition of organic matter and sedimentological expression of anoxia over the last 10 000 years. We use the data to investigate the dependence of salinity levels on climate evolution and isostasy. Changes in salinity of surface and deep waters were most pronounced from 8400 to approximately 5000 cal. BP. Density stratification bet…

  • Salinity changes in the central Baltic Sea (NW Europe) over the last 10000 years

    Open Access•Kay-Christian Emeis, Kay‐Christian Emeis et al.•ARTICLE•The Holocene•2003•Citada por: 21•Referencias: 4

    We attempt a reconstruction of salinity levels of the central Baltic Sea based on diatom assemblages, the isotopic composition of organic matter and sedimentological expression of anoxia over the last 10 000 years. We use the data to investigate the dependence of salinity levels on climate evolution and isostasy. Changes in salinity of surface and deep waters were most pronounced from 8400 to approximately 5000 cal. BP. Density stratification bet…

  • Regional climate change and the onset of farming in northern Germany and southern Scandinavia

    Open Access•Veronica Rohde Krossa, Matthias Moros et al.•ARTICLE•The Holocene•2017•Citada por: 3•Referencias: 23

    In Europe, the transition from hunter–gatherer–fisher-based communities into societies mainly relying on farming was spread from the southeast towards the north and west during the Holocene. In central Germany, farming was adopted at ~7500 cal. yr BP, whereas the shift is evident at ~6000–5500 cal. yr BP in northern Germany and southern Scandinavia. Consequently, farming techniques were available for more than a millennium. Some studies argue tha…

  • Holocene water mass changes in the Labrador Current

    Open Access•Annalena Lochte, Annalena Antonia Lochte et al.•ARTICLE•The Holocene•2019•Citada por: 1•Referencias: 17

    The Labrador Current is part of the anticlockwise subpolar gyre and plays a major role in the formation of North Atlantic Deep Water. It is influenced by the West Greenland and Baffin currents supplying warmer Atlantic and cold polar waters, respectively. During the early Holocene, at the final stage of the last deglaciation, meltwater and iceberg discharge caused highly variable conditions in the Labrador Current. In order to assess its sensitiv…

  • Centennial-scale variations in diatom productivity off Peru over the last 3000 years

    Open Access•Sophie Fleury, Xavier Crosta et al.•ARTICLE•The Holocene•2015•Citada por: 1•Referencias: 5

    The Peruvian coastal upwelling is one of the most productive systems in the global ocean, with important impacts on the carbon cycle. Primary productivity there displays strong variations at the interannual to decadal timescales. However, down-core investigations rarely reach sufficient temporal resolution to assess the response of productivity to climatic variations at these timescales beyond the instrumental and historical periods. We here anal…

  • Salinity changes in the central Baltic Sea (NW Europe) over the last 10000 years

    Open Access•Kay-Christian Emeis, Kay‐Christian Emeis et al.•ARTICLE•The Holocene•2003•Citada por: 21•Referencias: 4

    We attempt a reconstruction of salinity levels of the central Baltic Sea based on diatom assemblages, the isotopic composition of organic matter and sedimentological expression of anoxia over the last 10 000 years. We use the data to investigate the dependence of salinity levels on climate evolution and isostasy. Changes in salinity of surface and deep waters were most pronounced from 8400 to approximately 5000 cal. BP. Density stratification bet…

  • Centennial-scale variations in diatom productivity off Peru over the last 3000 years

    Open Access•Sophie Fleury, Xavier Crosta et al.•ARTICLE•The Holocene•2015•Citada por: 1•Referencias: 5

    The Peruvian coastal upwelling is one of the most productive systems in the global ocean, with important impacts on the carbon cycle. Primary productivity there displays strong variations at the interannual to decadal timescales. However, down-core investigations rarely reach sufficient temporal resolution to assess the response of productivity to climatic variations at these timescales beyond the instrumental and historical periods. We here anal…

  • Regional climate change and the onset of farming in northern Germany and southern Scandinavia

    Open Access•Veronica Rohde Krossa, Matthias Moros et al.•ARTICLE•The Holocene•2017•Citada por: 3•Referencias: 23

    In Europe, the transition from hunter–gatherer–fisher-based communities into societies mainly relying on farming was spread from the southeast towards the north and west during the Holocene. In central Germany, farming was adopted at ~7500 cal. yr BP, whereas the shift is evident at ~6000–5500 cal. yr BP in northern Germany and southern Scandinavia. Consequently, farming techniques were available for more than a millennium. Some studies argue tha…

  • Holocene water mass changes in the Labrador Current

    Open Access•Annalena Lochte, Annalena Antonia Lochte et al.•ARTICLE•The Holocene•2019•Citada por: 1•Referencias: 17

    The Labrador Current is part of the anticlockwise subpolar gyre and plays a major role in the formation of North Atlantic Deep Water. It is influenced by the West Greenland and Baffin currents supplying warmer Atlantic and cold polar waters, respectively. During the early Holocene, at the final stage of the last deglaciation, meltwater and iceberg discharge caused highly variable conditions in the Labrador Current. In order to assess its sensitiv…

  • Hydrographic shifts south of Australia over the last deglaciation and possible interhemispheric linkages

    Open Access•Matthias Moros, Patrick De Deckker et al.•ARTICLE•Quaternary Research•2021

    Northern and southern hemispheric influences—particularly changes in Southern Hemisphere westerly winds (SSW) and Southern Ocean ventilation—triggered the stepwise atmospheric CO 2 increase that accompanied the last deglaciation. One approach for gaining potential insights into past changes in SWW/CO 2 upwelling is to reconstruct the positions of the northern oceanic fronts associated with the Antarctic Circumpolar Current. Using two deep-sea cor…

Geology and Paleoclimatology Research (5 obras) · Geology (4 obras) · Holocene (4 obras) · Oceanography (4 obras) · Climatology (3 obras) · Geography (3 obras) · Climate change (2 obras) · Deglaciation (2 obras) · Glacial period (2 obras) · Isotope Analysis in Ecology (2 obras)

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