Publications des scientifiques de l'IRD

Montade V., Ledru Marie-Pierre, Burte J., Passos Rodrigues Martins E. S., Verola C. F., da Costa I. R., Magalhaes e Silva F. H. (2014). Stability of a Neotropical microrefugium during climatic instability. Journal of Biogeography, 41 (6), p. 1215-1226. ISSN 0305-0270.

Titre du document
Stability of a Neotropical microrefugium during climatic instability
Année de publication
2014
Type de document
Article référencé dans le Web of Science WOS:000335704500017
Auteurs
Montade V., Ledru Marie-Pierre, Burte J., Passos Rodrigues Martins E. S., Verola C. F., da Costa I. R., Magalhaes e Silva F. H.
Source
Journal of Biogeography, 2014, 41 (6), p. 1215-1226 ISSN 0305-0270
Aim The primary objectives of this study were (1) to assess, in the light of palaeoecological reconstruction, the climate stability hypothesis used by evolutionary biologists to explain high diversity in historically stable areas, and (2) to identify the response mechanisms of a tropical rain forest microrefugium to climatic variability. Location North-eastern Brazil, Serra de Maranguape. Methods Vegetation and climatic changes were reconstructed using a pollen record in a sediment core from a forest hollow, and the chronology was based on accelerator mass spectrometry radiocarbon analyses. Results Past vegetation dynamics consisted of three main forest types, shown by major compositional changes in rain forest assemblages between 5000 and 1000cal. yr bp. Dense ombrophilous forest was abruptly replaced by heliophilous early successional tree taxa at 4275cal. yr bp. These early successional tree taxa were established over a period of c.100years, and their dominance lasted for c.750years and was associated with dry conditions until 3525cal. yr bp. Subsequently, the expansion of secondary successional tree taxa over a period of c.550years enabled the recovery of ombrophilous forest. Main conclusions The vegetation changes in the Serra de Maranguape provide evidence for the high sensitivity of this rain forest microrefugium to climatic variability on a multidecadal to millennial time-scale during the mid- to late Holocene. Despite the substantial compositional and climatic changes, this microrefugium apparently was continuously forested and responded to climatic instability by recruiting key species to its highly diverse stock. This evidence helps to address the joint concerns of evolutionary biologists and palaeoecologists regarding how forests can persist during periods of climatic variability by showing that some tropical regions can remain continuously forested despite reorganization during abrupt and short-term climatic changes.
Plan de classement
Sciences du milieu [021] ; Géologie et formations superficielles [064] ; Etudes, transformation, conservation du milieu naturel [082]
Description Géographique
BRESIL ; ZONE TROPICALE
Localisation
Fonds IRD [F B010062057]
Identifiant IRD
fdi:010062057
Contact