Pollen counts of sediment core GeoB16205-4 from Parnaiba, NE Brazil

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Autores principales: Bouimetarhan, Ilham, Chiessi, Cristiano Mazur, González-Arango, Catalina, Dupont, Lydie M, Voigt, Ines, Prange, Matthias, Zonneveld, Karin A F
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2018
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author Bouimetarhan, Ilham
Chiessi, Cristiano Mazur
González-Arango, Catalina
Dupont, Lydie M
Voigt, Ines
Prange, Matthias
Zonneveld, Karin A F
author_facet Bouimetarhan, Ilham
Chiessi, Cristiano Mazur
González-Arango, Catalina
Dupont, Lydie M
Voigt, Ines
Prange, Matthias
Zonneveld, Karin A F
collection Datos científicos de ciencias marinas y ambientales
contents The semi-arid northeastern (NE) Brazil vegetation is largely dominated by Caatinga, one of the largest and richest dry forests in the world. Caatinga is a strategic biome, since it has borders with Cerrado, Atlantic forests and the Amazon, acting as a potential corridor (or barrier) for biotic interchange between these regions during evolutionary times. Therefore, accurate reconstructions of past vegetation, ecological and hydrological changes in this area are critical to understanding the dynamics of biome boundaries that may play an important role in dispersal and diversi!cation mechanisms and, more specifically, the link between the long-term climate variability and tropical biodiversity. Here, we present high-resolution palynological and elemental data from marine core GeoB16205-4 retrieved off the Parnaíba River mouth (NE Brazil) mainly covering the Younger Dryas (YD). We show that the YD interval was predominantly wet in NE Brazil, yet it was not homogenous and two distinct phases could be distinguished. A marked intensi!cation of wet conditions between ~12.3 and 11.6 cal kyr BP was recorded by the expansion of tropical rainforest and tree ferns. These results are in agreement with the transient TraCE-21k coupled climate model simulation. We infer that the second pluvial phase of the YD is related to a weak AMOC due to meltwater pulses in the North Atlantic, which forces a southward shift of the Intertropical Convergence Zone and its associated rainfall. Our records provide new evidence on the establishment of an “eastern forest corridor” in the nowadays semi-arid Caatinga allowing for past biotic interchanges of plant species.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_889701
institution PANGAEA
language en
publishDate 2018
publisher PANGAEA
record_format pangaea
spellingShingle Pollen counts of sediment core GeoB16205-4 from Parnaiba, NE Brazil
Bouimetarhan, Ilham
Chiessi, Cristiano Mazur
González-Arango, Catalina
Dupont, Lydie M
Voigt, Ines
Prange, Matthias
Zonneveld, Karin A F
056-4; Acacia; Acanthaceae; AGE; Alchornea; AMADEUS; Amaranthaceae/Chenopodiaceae; Ambrosia; Anacardiaceae; Arecaceae; Artemisia; Asteroideae; Bertiera-type; Borreria; Boscia-type; Burseraceae; Caesalpiniaceae; Cassia-type; Celtis; Center for Marine Environmental Sciences; Continental Slope Northeast Brazil; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Didynopamax; Ephedra distachya-type; Ephedra fragilis-type; Euphorbia-type; Fabaceae; Galium; GeoB16205-4; Gramineae; Gravity corer (Kiel type); Hedyosmum/Convolvulaceae; Ilex; Malvaceae; Maria S. Merian; MARUM; Melastomataceae; Mimosa-type; Mitracarpus; MSM20/3; Myricaceae; Particle, charred; Phyllanthus-type; Piliostigma; Plantago; Podocarpus; Pollen, total; Pollen and spores; Rhizophora; Rubiaceae spp.; Rutaceae; Scrophulariaceae/Solanaceae; SL; Spores total; Sporomorphs indeterminables; Stereospermum-type; Trichilia; Typha; Vernonia-type; Ziziphus
The semi-arid northeastern (NE) Brazil vegetation is largely dominated by Caatinga, one of the largest and richest dry forests in the world. Caatinga is a strategic biome, since it has borders with Cerrado, Atlantic forests and the Amazon, acting as a potential corridor (or barrier) for biotic interchange between these regions during evolutionary times. Therefore, accurate reconstructions of past vegetation, ecological and hydrological changes in this area are critical to understanding the dynamics of biome boundaries that may play an important role in dispersal and diversi!cation mechanisms and, more specifically, the link between the long-term climate variability and tropical biodiversity. Here, we present high-resolution palynological and elemental data from marine core GeoB16205-4 retrieved off the Parnaíba River mouth (NE Brazil) mainly covering the Younger Dryas (YD). We show that the YD interval was predominantly wet in NE Brazil, yet it was not homogenous and two distinct phases could be distinguished. A marked intensi!cation of wet conditions between ~12.3 and 11.6 cal kyr BP was recorded by the expansion of tropical rainforest and tree ferns. These results are in agreement with the transient TraCE-21k coupled climate model simulation. We infer that the second pluvial phase of the YD is related to a weak AMOC due to meltwater pulses in the North Atlantic, which forces a southward shift of the Intertropical Convergence Zone and its associated rainfall. Our records provide new evidence on the establishment of an “eastern forest corridor” in the nowadays semi-arid Caatinga allowing for past biotic interchanges of plant species.
title Pollen counts of sediment core GeoB16205-4 from Parnaiba, NE Brazil
topic 056-4; Acacia; Acanthaceae; AGE; Alchornea; AMADEUS; Amaranthaceae/Chenopodiaceae; Ambrosia; Anacardiaceae; Arecaceae; Artemisia; Asteroideae; Bertiera-type; Borreria; Boscia-type; Burseraceae; Caesalpiniaceae; Cassia-type; Celtis; Center for Marine Environmental Sciences; Continental Slope Northeast Brazil; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Didynopamax; Ephedra distachya-type; Ephedra fragilis-type; Euphorbia-type; Fabaceae; Galium; GeoB16205-4; Gramineae; Gravity corer (Kiel type); Hedyosmum/Convolvulaceae; Ilex; Malvaceae; Maria S. Merian; MARUM; Melastomataceae; Mimosa-type; Mitracarpus; MSM20/3; Myricaceae; Particle, charred; Phyllanthus-type; Piliostigma; Plantago; Podocarpus; Pollen, total; Pollen and spores; Rhizophora; Rubiaceae spp.; Rutaceae; Scrophulariaceae/Solanaceae; SL; Spores total; Sporomorphs indeterminables; Stereospermum-type; Trichilia; Typha; Vernonia-type; Ziziphus
url https://doi.org/10.1594/PANGAEA.889701