Mid- to late-Holocene climate variability and anthropogenic impacts: multi-proxy evidence from Lake Bliden, Denmark

2009 ◽  
Vol 43 (2) ◽  
pp. 323-343 ◽  
Author(s):  
Jesper Olsen ◽  
Nanna Noe-Nygaard ◽  
Brent B. Wolfe
Keyword(s):  
Climate Variability ◽  
Late Holocene ◽  
Anthropogenic Impacts ◽  
Holocene Climate

The response of a jack pine forest to late-Holocene climate variability in northwestern Wisconsin

The Holocene ◽  
2009 ◽  
Vol 19 (7) ◽  
pp. 1049-1061 ◽  
Author(s):  
Michael A. Tweiten ◽  
Sara C. Hotchkiss ◽  
Robert K. Booth ◽  
Randy R. Calcote ◽  
Elizabeth A. Lynch
Keyword(s):  
Climate Variability ◽  
Late Holocene ◽  
Jack Pine ◽  
Pine Forest ◽  
Holocene Climate

Evidence of late Holocene climate variability in the western Nanling Mountains, South China

2014 ◽  
Vol 52 (1-2) ◽  
pp. 1-10 ◽  
Author(s):  
Wei Zhong ◽  
Jibin Xue ◽  
Jun Ouyang ◽  
Jiayuan Cao ◽  
Zhanghong Peng
Keyword(s):  
Climate Variability ◽  
South China ◽  
Late Holocene ◽  
Holocene Climate ◽  
Nanling Mountains

scholarly journals Late Holocene climate variability in the southwestern Mediterranean region: an integrated marine and terrestrial geochemical approach

2010 ◽  
Vol 6 (6) ◽  
pp. 807-816 ◽  
Author(s):  
C. Martín-Puertas ◽  
F. Jiménez-Espejo ◽  
F. Martínez-Ruiz ◽  
V. Nieto-Moreno ◽  
M. Rodrigo ◽  
...  
Keyword(s):  
Climate Variability ◽  
North Atlantic ◽  
Mediterranean Region ◽  
Late Holocene ◽  
Western Mediterranean ◽  
Medieval Climate Anomaly ◽  
Holocene Climate ◽  
Climate Anomaly ◽  
The North ◽  
The North Atlantic

Abstract. A combination of marine (Alboran Sea cores, ODP 976 and TTR 300 G) and terrestrial (Zoñar Lake, Andalucia, Spain) geochemical proxies provides a high-resolution reconstruction of climate variability and human influence in the southwestern Mediterranean region for the last 4000 years at inter-centennial resolution. Proxies respond to changes in precipitation rather than temperature alone. Our combined terrestrial and marine archive documents a succession of dry and wet periods coherent with the North Atlantic climate signal. A dry period occurred prior to 2.7 cal ka BP – synchronously to the global aridity crisis of the third-millennium BC – and during the Medieval Climate Anomaly (1.4–0.7 cal ka BP). Wetter conditions prevailed from 2.7 to 1.4 cal ka BP. Hydrological signatures during the Little Ice Age are highly variable but consistent with more humidity than the Medieval Climate Anomaly. Additionally, Pb anomalies in sediments at the end of the Bronze Age suggest anthropogenic pollution earlier than the Roman Empire development in the Iberian Peninsula. The Late Holocene climate evolution of the in the study area confirms the see-saw pattern between the eastern and western Mediterranean regions and the higher influence of the North Atlantic dynamics in the western Mediterranean.

Holocene climate variability and anthropogenic impacts from Lago Paixban, a perennial wetland in Peten, Guatemala

2016 ◽  
Vol 138 ◽  
pp. 70-81 ◽  
Author(s):  
David Wahl ◽  
Richard D. Hansen ◽  
Roger Byrne ◽  
Lysanna Anderson ◽  
Thomas Schreiner
Keyword(s):  
Climate Variability ◽  
Anthropogenic Impacts ◽  
Holocene Climate

Coherent rainfall response to middle- and late-Holocene climate variability across the mid-latitude South Pacific

The Holocene ◽  
2013 ◽  
Vol 23 (7) ◽  
pp. 1002-1007 ◽  
Author(s):  
Basil Gomez ◽  
Lionel Carter ◽  
Noel A Trustrum ◽  
Michael J Page ◽  
Alan R Orpin
Keyword(s):  
Climate Variability ◽  
Late Holocene ◽  
South Pacific ◽  
Holocene Climate ◽  
Middle And Late Holocene
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