TY  - JOUR
A1  - Hoogakker, Babette A. A.
A1  - Smith, Robin S.
A1  - Singarayer, Joy
A1  - Marchant, Robert
A1  - Prentice, I. Colin
A1  - Allen, Judy R. M.
A1  - Anderson, R. Scott
A1  - Bhagwat, Shonil A.
A1  - Behling, Hermann
A1  - Borisova, Olga
A1  - Bush, Mark B.
A1  - Correa-Metrio, Alexander
A1  - De Vernal, Anne
A1  - Finch, Jemma M.
A1  - Fréchette, Bianca
A1  - Lozano-García, Socorro
A1  - Gosling, William D.
A1  - Granoszewski, Wojciech
A1  - Grimm, Eric C.
A1  - Grüger, Eberhard
A1  - Hanselman, Jennifer
A1  - Harrison, Sandy P.
A1  - Hill, Trevor R.
A1  - Huntley, Brian
A1  - Jimenez-Moreno, Gonzalo
A1  - Kershaw, Arnold Peter
A1  - Ledru, Marie-Pierre
A1  - Magri, Donatella
A1  - McKenzie, Merna
A1  - Müller, Ulrich
A1  - Nakagawa, Takeshi
A1  - Novenko, Elena
A1  - Penny, Daniel
A1  - Sadori, Laura
A1  - Scott, Louis
A1  - Stevenson, Janelle
A1  - Valdes, Paul J.
A1  - Vandergoes, Marcus
A1  - Velichko, Andrey
A1  - Whitlock, Cathy
A1  - Tzedakis, Chronis
T1  - Terrestrial biosphere changes over the last 120 kyr
T2  - Climate of the past
N2  - A new global synthesis and biomization of long (> 40 kyr) pollen-data records is presented and used with simulations from the HadCM3 and FAMOUS climate models and the BIOME4 vegetation model to analyse the dynamics of the global terrestrial biosphere and carbon storage over the last glacial–interglacial cycle. Simulated biome distributions using BIOME4 driven by HadCM3 and FAMOUS at the global scale over time generally agree well with those inferred from pollen data. Global average areas of grassland and dry shrubland, desert, and tundra biomes show large-scale increases during the Last Glacial Maximum, between ca. 64 and 74 ka BP and cool substages of Marine Isotope Stage 5, at the expense of the tropical forest, warm-temperate forest, and temperate forest biomes. These changes are reflected in BIOME4 simulations of global net primary productivity, showing good agreement between the two models. Such changes are likely to affect terrestrial carbon storage, which in turn influences the stable carbon isotopic composition of seawater as terrestrial carbon is depleted in 13C.
Y1  - 2016
UR  - http://publikationen.ub.uni-frankfurt.de/frontdoor/index/index/docId/42017
UR  - https://nbn-resolving.org/urn:nbn:de:hebis:30:3-420176
UR  - http://www.clim-past.net/12/51/2016
SN  - 1814-9332
SN  - 1814-9324
N1  - © Author(s) 2016. CC Attribution 3.0 License.
VL  - 12
IS  - 1
SP  - 51
EP  - 73
PB  - Copernicus Ges.
CY  - Katlenburg-Lindau
ER  -