CO 2 radiative forcing during the Holocene Thermal Maximum revealed by stomatal frequency of Iberian oak leaves

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: CO 2 radiative forcing during the Holocene Thermal Maximum revealed by stomatal frequency of Iberian oak leaves ; number:5 ; year:2008 ; pages:3945-3964
Biogeosciences discussions ; Heft 5 (2008), 3945-3964

Creator: García-Amorena, I.
Wagner-Cremer, F.
Gómez Manzaneque, F.
van Hoof, T. B.
García Álvarez, S.
Visscher, H.

DOI: 10.5194/bgd-5-3945-2008

URN: urn:nbn:de:101:1-2018010314182

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:24 AM CEST

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García-Amorena, I.
Wagner-Cremer, F.
Gómez Manzaneque, F.
van Hoof, T. B.
García Álvarez, S.
Visscher, H.

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CO 2 radiative forcing during the Holocene Thermal Maximum revealed by stomatal frequency of Iberian oak leaves

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Other Objects (12)

Reconstructing burnt area during the Holocene: an Iberian case study

Does Belgian Holocene speleothem records solar forcing and cold events?

High-frequency climate forcing causes prolonged cold periods in the Holocene

Transpiration and stomatal conductance of mistletoe (Loranthus europaeus) and its host plant, downy oak (Quercus pubescens)

Monsoonal response to mid-holocene orbital forcing in a high resolution GCM

Coupled climate model simulation of Holocene cooling events: oceanic feedback amplifies solar forcing

Metabolomics for understanding stomatal movements

Sensitivity to open boundary forcing in a fine-resolution model of the Iberian shelf-slope region

Integrating stomatal physiology and morphology: evolution of stomatal control and development of future crops

Quantitative reconstruction of precipitation changes in the Iberian Peninsula during the Late Pleistocene and the Holocene

Mid- to Late Holocene climate variability and the 4.2 ka BP event on the Iberian Peninsula

Identifying biological affinities of Holocene northern Iberian populations through the inner structures of the upper first molars

Reconstructing burnt area during the Holocene: an Iberian case study

Does Belgian Holocene speleothem records solar forcing and cold events?

High-frequency climate forcing causes prolonged cold periods in the Holocene

Transpiration and stomatal conductance of mistletoe (Loranthus europaeus) and its host plant, downy oak (Quercus pubescens)

Monsoonal response to mid-holocene orbital forcing in a high resolution GCM

Coupled climate model simulation of Holocene cooling events: oceanic feedback amplifies solar forcing

Metabolomics for understanding stomatal movements

Sensitivity to open boundary forcing in a fine-resolution model of the Iberian shelf-slope region

Integrating stomatal physiology and morphology: evolution of stomatal control and development of future crops

Quantitative reconstruction of precipitation changes in the Iberian Peninsula during the Late Pleistocene and the Holocene

Mid- to Late Holocene climate variability and the 4.2 ka BP event on the Iberian Peninsula

Identifying biological affinities of Holocene northern Iberian populations through the inner structures of the upper first molars

Reconstructing burnt area during the Holocene: an Iberian case study

Does Belgian Holocene speleothem records solar forcing and cold events?

High-frequency climate forcing causes prolonged cold periods in the Holocene

Transpiration and stomatal conductance of mistletoe (Loranthus europaeus) and its host plant, downy oak (Quercus pubescens)

Monsoonal response to mid-holocene orbital forcing in a high resolution GCM

Coupled climate model simulation of Holocene cooling events: oceanic feedback amplifies solar forcing

Metabolomics for understanding stomatal movements

Sensitivity to open boundary forcing in a fine-resolution model of the Iberian shelf-slope region

Integrating stomatal physiology and morphology: evolution of stomatal control and development of future crops

Quantitative reconstruction of precipitation changes in the Iberian Peninsula during the Late Pleistocene and the Holocene

Mid- to Late Holocene climate variability and the 4.2 ka BP event on the Iberian Peninsula

Identifying biological affinities of Holocene northern Iberian populations through the inner structures of the upper first molars

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