IMIS

Publicaties | Instituten | Personen | Datasets | Projecten | Kaarten
[ meld een fout in dit record ]mandje (0): toevoegen | toon Print deze pagina

Ultra-high resolution pollen record from the northern Andes reveals rapid shifts in montane climates within the last two glacial cycles
Groot, M.H.M.; Bogotá, R.G.; Lourens, L.J.; Hooghiemstra, H.; Vriend, M.; Berrio, J.C.; Tuenter, E.; Van der Plicht, J.; van Geel, B.; Ziegler, M.; Weber, S.L.; Betancourt, A.; Contreras, L.; Gaviria, S.; Giraldo, C.; González, N.; Jansen, J.H.F.; Konert, M.; Ortega, D.; Rangel, O.; Sarmiento, G.; Vandenberghe, J.; Van der Hammen, T.; van der Linden, M.; Westerhoff, W. (2011). Ultra-high resolution pollen record from the northern Andes reveals rapid shifts in montane climates within the last two glacial cycles. Clim. Past 7(1): 299-316
In: Climate of the Past. Copernicus: Göttingen. ISSN 1814-9324; e-ISSN 1814-9332, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

Auteurs  Top 
  • Groot, M.H.M.
  • Bogotá, R.G.
  • Lourens, L.J.
  • Hooghiemstra, H.
  • Vriend, M.
  • Berrio, J.C.
  • Tuenter, E., meer
  • Van der Plicht, J.
  • van Geel, B.
  • Ziegler, M.
  • Weber, S.L.
  • Betancourt, A.
  • Contreras, L.
  • Gaviria, S.
  • Giraldo, C.
  • González, N.
  • Jansen, J.H.F., meer
  • Konert, M.
  • Ortega, D.
  • Rangel, O.
  • Sarmiento, G.
  • Vandenberghe, J.
  • Van der Hammen, T., meer
  • van der Linden, M.
  • Westerhoff, W.

Abstract
    Here we developed a composite pollen-based record of altitudinal vegetation changes from Lake Fuquene (5 degrees N) in Colombia at 2540m elevation. We quantitatively calibrated Arboreal Pollen percentages (AP%) into mean annual temperature (MAT) changes with an unprecedented similar to 60-year resolution over the past 284 000 years. An age model for the AP% record was constructed using frequency analysis in the depth domain and tuning of the distinct obliquity-related variations to the latest marine oxygen isotope stacked record. The reconstructed MAT record largely concurs with the similar to 100 and 41-kyr (obliquity) paced glacial cycles and is superimposed by extreme changes of up to 7 to 10 degrees Celsius within a few hundred years at the major glacial terminations and during marine isotope stage 3, suggesting an unprecedented North Atlantic - equatorial link. Using intermediate complexity transient climate modelling experiments, we demonstrate that ice volume and greenhouse gasses are the major forcing agents causing the orbital-related MAT changes, while direct precession-induced insolation changes had no significant impact on the high mountain vegetation during the last two glacial cycles.

Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid Top | Auteurs