@article{fdi:010066658,
  title = {{T}errestrial biosphere changes over the last 120 kyr},
  author = {{H}oogakker, {B}. {A}. {A}. and {S}mith, {R}. {S}. and {S}ingarayer, {J}. {S}. and {M}archant, {R}. and {P}rentice, {I}. {C}. and {A}llen, {J}. {R}. {M}. and {A}nderson, {R}. {S}. and {B}hagwat, {S}. {A}. and {B}ehling, {H}. and {B}orisova, {O}. and {B}ush, {M}. and {C}orrea-{M}etrio, {A}. and de {V}ernal, {A}. and {F}inch, {J}. {M}. and {F}rechette, {B}. and {L}ozano-{G}arcia, {S}. and {G}osling, {W}. {D}. and {G}ranoszewski, {W}. and {G}rimm, {E}. {C}. and {G}ruger, {E}. and {H}anselman, {J}. and {H}arrison, {S}. {P}. and {H}ill, {T}. {R}. and {H}untley, {B}. and {J}imenez-{M}oreno, {G}. and {K}ershaw, {P}. and {L}edru, {M}arie-{P}ierre and {M}agri, {D}. and {M}c{K}enzie, {M}. and {M}uller, {U}. and {N}akagawa, {T}. and {N}ovenko, {E}. and {P}enny, {D}. and {S}adori, {L}. and {S}cott, {L}. and {S}tevenson, {J}. and {V}aldes, {P}. {J}. and {V}andergoes, {M}. and {V}elichko, {A}. and {W}hitlock, {C}. and {T}zedakis, {C}.},
  editor = {},
  language = {{ENG}},
  abstract = {{A} new global synthesis and biomization of long (>40 kyr) pollen-data records is presented and used with simulations from the {H}ad{CM}3 and {FAMOUS} climate models and the {BIOME}4 vegetation model to analyse the dynamics of the global terrestrial biosphere and carbon storage over the last glacial-interglacial cycle. {S}imulated biome distributions using {BIOME}4 driven by {H}ad{CM}3 and {FAMOUS} at the global scale over time generally agree well with those inferred from pollen data. {G}lobal average areas of grassland and dry shrubland, desert, and tundra biomes show large-scale increases during the {L}ast {G}lacial {M}aximum, between ca. 64 and 74 ka {BP} and cool substages of {M}arine {I}sotope {S}tage 5, at the expense of the tropical forest, warm-temperate forest, and temperate forest biomes. {T}hese changes are reflected in {BIOME}4 simulations of global net primary productivity, showing good agreement between the two models. {S}uch 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 {C}-13.},
  keywords = {{MONDE}},
  booktitle = {},
  journal = {{C}limate of the {P}ast},
  volume = {12},
  numero = {1},
  pages = {51--73},
  ISSN = {1814-9324},
  year = {2016},
  DOI = {10.5194/cp-12-51-2016},
  URL = {https://www.documentation.ird.fr/hor/fdi:010066658},
}