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Research and Review Papers |
| 3. | Global characterization of the Holocene Thermal Maximum
Original Research Article
Pages 7-19
H. Renssen, H. Seppä, X. Crosta, H. Goosse, D.M. Roche
Highlights► We provide a global characterization of the Holocene Thermal Maximum. ► We analyze the spatial variations in timing, intensity and seasonal _expression_. ► The model results are in general agreement with global proxy evidence.
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| 4. | LGM ice sheet extent in the Weddell Sea: evidence for diachronous behavior of Antarctic Ice Sheets
Original Research Article
Pages 20-31
Travis Stolldorf, Hans-Werner Schenke, John B. Anderson
Highlights► Grounding line retreat in the Weddell Sea is constrained by radiocarbon dates. ► The East Antarctic Ice Sheet has not appreciably advanced in the last 30,000 years. ► Identification of a previously unknown glacial trough (named Hughes Trough). ► Mega-scale glacial lineations identified in Ronne and Hughes Troughs.
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| 8. | Dating High Arctic Holocene relative sea level changes using juvenile articulated marine shells in raised beaches
Original Research Article
Pages 61-66
Antony J. Long, Mateusz C. Strzelecki, Jerry M. Lloyd, Charlotte L. Bryant
Highlights► We detail a new way to date raised beaches using reworked marine molluscs. ► Carefully collected paired valves of juvenileAstarte borealisyield excellent sea-level data. ► We develop a new sea-level curve for central Spitsbergen. ► Our findings support a significant ice dome in the north-east Barents Sea. ► The method has potential applications elsewhere in High Arctic settings.
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| 11. | Regional imprints of millennial variability during the MIS 3 period around Antarctica
Original Research Article
Pages 99-112
D. Buiron, B. Stenni, J. Chappellaz, A. Landais, M. Baumgartner, M. Bonazza, E. Capron, M. Frezzotti, M. Kageyama, B. Lemieux-Dudon, V. Masson-Delmotte, F. Parrenin, A. Schilt, E. Selmo, M. Severi, D. Swingedouw, R. Udisti
Highlights► Review of glacial millennial-scale climate variability in Antarctic ice cores. ► Comparison between Antarctic ice core data and global coupled model simulations. ► Included new Talos Dome ice core climatic data. ► Regional differences of Southern Ocean and Antarctica climate are observed when North Atlantic Ocean circulation is weakened.
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Núcleo de Arqueologia e Paleoecologia FCHS Universidade do Algarve Campus de Gambelas 8005-139 Faro, PORTUGAL
Mail: nap.ualg@gmail.com
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Núcleo de Arqueologia e Paleoecologia FCHS Universidade do Algarve Campus de Gambelas 8005-139 Faro, PORTUGAL
Mail: nap.ualg@gmail.com
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