Vegetation and climate in the eastern Iberian Peninsula during the pre-evaporitic Messinian (late Miocene). Palynological data from the Upper Turolian of Venta del Moro (Spain)

The present paper reports a complete palynological study of the Upper Turolian sediments outcropping at the Venta del Moro site (eastern Iberian Peninsula). The pollen assemblages observed mainly reflect the local and regional vegetation, which must have formed part of a wetland ecosystem within a g...

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Published inReview of palaeobotany and palynology Vol. 215; pp. 85 - 99
Main Authors Casas-Gallego, Manuel, Lassaletta, Luis, Barrón, Eduardo, Bruch, Angela A., Montoya, Plinio
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.04.2015
Subjects
Eastern Iberian Peninsula
Late Miocene
Open vegetation
Palaeoclimate
Pollen analysis
Late Miocene
Eastern Iberian Peninsula
Open vegetation
Palaeoclimate
Pollen analysis
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Abstract The present paper reports a complete palynological study of the Upper Turolian sediments outcropping at the Venta del Moro site (eastern Iberian Peninsula). The pollen assemblages observed mainly reflect the local and regional vegetation, which must have formed part of a wetland ecosystem within a general setting of open steppe, as indicated by the great abundance and diversity of herbaceous pollen. This reflects the persistence of open vegetation in the Iberian Peninsula after the Middle Miocene when it became extensive. We here report the most recent record of Disanthus for the Iberian Peninsula. This shrub played an important role in an unusual, edaphically-mediated vegetation linked to lacustrine–palustrine or riparian shore conditions. A shift in the water level led to a flooding episode, extending wetland and causing a drastic reduction in Disanthus and Amaranthaceae. The results of quantitative (multivariate and coexistence) and semi-quantitative (integrated plant record) analyses of the pollen dataset support these interpretations of the palaeovegetation and provide insight into the regional palaeoclimate. Stable climatic conditions would appear to have reigned before the onset of the Messinian salinity crisis. The palynoflora of Venta del Moro is compared with counterparts in other areas of the Mediterranean Basin. •A complete palynological study of a late Miocene site in eastern Iberian Peninsula is presented.•The vegetation inferred consists in a wetland environment developed within an arid setting.•We report the most recent record of Disanthus on the Iberian Peninsula.•Changes in pollen abundances indicate a shift in groundwater level affecting the vegetation.•The coexistence approach method supplies quantitative values for four palaeoclimatic parameters.
AbstractList The present paper reports a complete palynological study of the Upper Turolian sediments outcropping at the Venta del Moro site (eastern Iberian Peninsula). The pollen assemblages observed mainly reflect the local and regional vegetation, which must have formed part of a wetland ecosystem within a general setting of open steppe, as indicated by the great abundance and diversity of herbaceous pollen. This reflects the persistence of open vegetation in the Iberian Peninsula after the Middle Miocene when it became extensive. We here report the most recent record of Disanthus for the Iberian Peninsula. This shrub played an important role in an unusual, edaphically-mediated vegetation linked to lacustrine–palustrine or riparian shore conditions. A shift in the water level led to a flooding episode, extending wetland and causing a drastic reduction in Disanthus and Amaranthaceae. The results of quantitative (multivariate and coexistence) and semi-quantitative (integrated plant record) analyses of the pollen dataset support these interpretations of the palaeovegetation and provide insight into the regional palaeoclimate. Stable climatic conditions would appear to have reigned before the onset of the Messinian salinity crisis. The palynoflora of Venta del Moro is compared with counterparts in other areas of the Mediterranean Basin. •A complete palynological study of a late Miocene site in eastern Iberian Peninsula is presented.•The vegetation inferred consists in a wetland environment developed within an arid setting.•We report the most recent record of Disanthus on the Iberian Peninsula.•Changes in pollen abundances indicate a shift in groundwater level affecting the vegetation.•The coexistence approach method supplies quantitative values for four palaeoclimatic parameters.
Author Barrón, Eduardo
Bruch, Angela A.
Casas-Gallego, Manuel
Lassaletta, Luis
Montoya, Plinio
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  organization: Departament de Geologia, Àrea de Paleontologia, Universitat de València, Doctor Moliner 50, 46100 Burjassot, Spain
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Keywords Late Miocene
Eastern Iberian Peninsula
Open vegetation
Palaeoclimate
Pollen analysis
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Snippet The present paper reports a complete palynological study of the Upper Turolian sediments outcropping at the Venta del Moro site (eastern Iberian Peninsula)....
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SubjectTerms Eastern Iberian Peninsula
Late Miocene
Open vegetation
Palaeoclimate
Pollen analysis
Title Vegetation and climate in the eastern Iberian Peninsula during the pre-evaporitic Messinian (late Miocene). Palynological data from the Upper Turolian of Venta del Moro (Spain)
URI https://dx.doi.org/10.1016/j.revpalbo.2015.01.001
Volume 215
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