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  • 2015-2019  (16)
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  • 1
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (21 Seiten, 8,86 MB) , Diagramme, Illustrationen
    Language: German
    Note: Förderkennzeichen BMBF 01DH16030 , Verfasser dem Berichtsblatt entnommen , Laufzeit des Vorhabens: 01.12.2016 - 30.11.2019; Berichtszeitraum: 01.12.2016 - 30.11.2019 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden
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  • 2
    Publication Date: 2021-02-08
    Description: 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 diversification 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 intensification 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.
    Type: Article , PeerReviewed
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  • 3
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    PANGAEA
    In:  Supplement to: Zhao, Xueqin; Dupont, Lydie M; Cheddadi, Rachid; Kölling, Martin; Reddad, Hanane; Groeneveld, Jeroen; Ain-Lhout, Fatima Zohra; Bouimetarhan, Ilham (2019): Recent climatic and anthropogenic impacts on endemic species in southwestern Morocco. Quaternary Science Reviews, 221, 105889, https://doi.org/10.1016/j.quascirev.2019.105889
    Publication Date: 2023-03-03
    Description: Morocco is an area subject to recurrent severe droughts, desertification and an increasing land degradation. It is within a Mediterranean hotspot of biodiversity as it harbors many threatened endemic species such as the argan tree (Argania spinosa). In this context, past climate records are needed to analyze the impact of climate variability on the occurrence and future persistence of these endemic species. In order to evaluate the impact of past climate changes on the endemic Argan tree in southern Morocco, we reconstructed its modern range using an extensive pollen dataset. The modern pollen distribution off southwestern Morocco was then utilized to interpret the high-resolution pollen record with complementary micro-charcoal and XRF element records from a marine sediment core GeoB8601-3 off Cape Ghir in southwestern Morocco covering the last three millennia. This multi-proxy study has shown clear evidence of wetter conditions resulting in higher fluvial input which could be correlated with a negative mode of the North Atlantic Oscillation (NAO), in contrast to the published pollen and XRF element records from another nearby core that showed limited effect of climate changes. On the other hand, clear opposite trend between the pollen occurrences of Argania spinosa and the fire frequency was observed throughout our fossil record. The increase of Argania spinosa pollen occurrences, along with herbaceous taxa, and lower fire frequency might suggest an increase in human impact on the landscape leading to a sparse vegetation cover and subsequently increased erosion. The reconstructed pollen-based vegetation, micro-charcoal-based fire activities and geochemical changes in our marine record suggest interplay of climate and anthropogenic effects on the landscape.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
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    PANGAEA
    In:  Supplement to: Zhao, Xueqin; Dupont, Lydie M; Schefuß, Enno; Bouimetarhan, Ilham; Wefer, Gerold (2017): Palynological evidence for Holocene climatic and oceanographic changes off western South Africa. Quaternary Science Reviews, 165, 88-101, https://doi.org/10.1016/j.quascirev.2017.04.022
    Publication Date: 2023-11-28
    Description: Atmospheric and oceanographic interactions between the Atlantic and Indian Oceans influence upwelling in the southern Benguela upwelling system. In order to obtain a better knowledge of paleoceanographic and paleoenvironmental changes in the southern Benguela region during the Holocene, 12 marine surface sediment samples and one gravity core GeoB8331-4 from the Namaqualand mudbelt off the west coast of South Africa have been studied for organic-walled dinoflagellate cysts in high temporal resolution. The results are compared with pollen and geochemical records from the same samples. Our study emphasizes significantly distinct histories in upwelling intensity as well as the influence of fluvial input during the Holocene. Three main phases were identified for the Holocene. High percentages of cysts produced by autotrophic taxa like Operculodinium centrocarpum and Spiniferites spp. indicate warmer and stratified conditions during the early Holocene (9900-8400 cal. yr BP), suggesting reduced upwelling likely due to a northward shift of the southern westerlies. In contrast, the middle Holocene (8400-3100 cal. yr BP) is characterized by a strong increase in heterotrophic taxa in particular Lejeunecysta paratenella and Echinidinium spp. at the expense of autotrophic taxa. This indicates cool and nutrient-rich waters with active upwelling probably caused by a southward shift of the southern westerlies. During the late Holocene (3100 cal. yr BP to modern), Brigantedinium spp. and other abundant taxa interpreted to indicate fluvial nutrient input such as cyst of Protoperidinium americanum and Lejeunecysta oliva imply strong river discharge with high nutrient supply between 3100 and 640 cal. yr BP.
    Keywords: Center for Marine Environmental Sciences; MARUM; RAiN; Regional Archives for Integrated iNvestigations
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Bouimetarhan, Ilham; Dupont, Lydie M; Kuhlmann, Holger; Pätzold, Jürgen; Prange, Matthias; Schefuß, Enno; Zonneveld, Karin A F (2015): Northern Hemisphere control of deglacial vegetation changes in the Rufiji uplands (Tanzania). Climate of the Past, 11(5), 751-764, https://doi.org/10.5194/cp-11-751-2015
    Publication Date: 2024-03-06
    Description: In tropical eastern Africa, vegetation distribution is largely controlled by regional hydrology, which has varied over the past 20 000 years. Therefore, accurate reconstructions of past vegetation and hydrological changes are crucial for a better understanding of climate variability in the tropical southeastern African region. We present high-resolution pollen records from a marine sediment core recovered offshore of the Rufiji River delta. Our data document significant shifts in pollen assemblages during the last deglaciation, identifying, through changes in both upland and lowland vegetation, specific responses of plant communities to atmospheric (precipitation) and coastal (coastal dynamics and sea-level changes) alterations. Specifically, arid conditions reflected by a maximum pollen representation of dry and open vegetation occurred during the Northern Hemisphere cold Heinrich event 1 (H1), suggesting that the expansion of drier upland vegetation was synchronous with cold Northern Hemisphere conditions. This arid period is followed by an interval in which forest and humid woodlands expanded, indicating a hydrologic shift towards more humid conditions. Droughts during H1 and the shift to humid conditions around 14.8 kyr BP in the uplands are consistent with latitudinal shifts of the intertropical convergence zone (ITCZ) driven by high-latitude Northern Hemisphere climatic fluctuations. Additionally, our results show that the lowland vegetation, consisting of well-developed salt marshes and mangroves in a successional pattern typical for vegetation occurring in intertidal habitats, has responded mainly to local coastal dynamics related to marine inundation frequencies and soil salinity in the Rufiji Delta as well as to the local moisture availability. Lowland vegetation shows a substantial expansion of mangrove trees after ~ 14.8 kyr BP, suggesting an increased moisture availability and river runoff in the coastal area. The results of this study highlight the decoupled climatic and environmental processes to which the vegetation in the uplands and the Rufiji Delta has responded during the last deglaciation.
    Keywords: Acacia; AGE; Alchornea; Algae; Amaranthaceae/Chenopodiaceae; Area South of Mafia Island; Artemisia; Asteroideae; Borreria; Boscia-type; Butyrospermum; Caryophyllaceae; Cassia-type; Celtis; Center for Marine Environmental Sciences; Cleome; Combretaceae; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Euphorbia-type; Galium; GeoB12624-1; Gramineae; Gravity corer (Kiel type); Hymenocardia; Indigofera; Isoberlinia; Lycopodium spores added; Lycopodium spores counted; M75/2; M75/2_115-1; MARUM; Meteor (1986); Mimosa-type; Olea; Phyllanthus; Piliostigma; Plantago; Podocarpus; Pollen, total; Psydrax-type subcordata; Pterocarpus-type; Rhizophora; Rhus-type; SL; Spores; Stereospermum-type; Tamarindus-type indica; Typha; Uapaca; Vernonia-type; Ziziphus
    Type: Dataset
    Format: text/tab-separated-values, 1621 data points
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  • 6
    Publication Date: 2024-03-06
    Keywords: 261; Abies; Acacia; Acanthaceae; Age; Aizoaceae; Amaranthaceae/Chenopodiaceae; Apiaceae; Argania spinosa; Artemisia; Aruncus-type; Asphodelus-type; Asteroideae; Brassicaceae; Carlina-type; Caryophyllaceae; Cedrus; Centaurea-type; Center for Marine Environmental Sciences; Cichorioideae; Combretaceae; Concentricystes; Convolvulaceae; Cyperaceae; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dicoma-type; Ephedra distachya-type; Ephedra fragilis-type; Ericaceae; Euphorbia; Euphorbiaceae; Fabaceae; GeoB8601-3; Gravity corer (Kiel type); Humulus; Indeterminata; Jasminum; Juglans; Juniperus/Tetraclinis; Justicia-type; Labiatae; Laggera-type; Leguminosae; Liliaceae; M58/2; Malvaceae; Marker, added; Marker, found; MARUM; Mass; Meteor (1986); Myrtaceae; off Northwest Africa; Olea; Pacourina-type; Pentzia-type; Phillyrea; Phragmites-type; Pinaceae; Pinus; Pinus/Cedrus; Pistacia; Plantago; Poaceae; Pollen, total; Polygalaceae; Polygonum; Polypodiaceae; Pteris; Quercus ilex-type; Quercus robur-type; Ranunculaceae; Rhamnus; Rhus; Rumex; Rutaceae; Salix; Scrophulariaceae; Selaginella; SL; Solanaceae; Spores; Spores, monolete; Spores, trilete; Tamarix; Tsuga; Typha; Ulmus; Urticaceae; Xanthium-type; Ziziphus
    Type: Dataset
    Format: text/tab-separated-values, 3547 data points
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  • 7
    Publication Date: 2024-03-06
    Keywords: 261; 264; 266; 267; 270; 271; 273; Abies; Acacia; Agadir Canyon; Aizoaceae; Amaranthaceae/Chenopodiaceae; Apiaceae; Argania spinosa; Artemisia; Aruncus-type; Asphodelus-type; Asteroideae; Brassicaceae; Caryophyllaceae; Cedrus; Center for Marine Environmental Sciences; Cichorioideae; Cliffortia-type; Combretaceae; Concentricystes; Cyperaceae; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dicoma-type; Elevation of event; Ephedra; Ericaceae; Euphorbia; Euphorbiaceae; Event label; GeoB4210-1; GeoB6009-1; GeoB6010-1; GeoB6011-2; GeoB8601-1; GeoB8604-3; GeoB8606-2; GeoB8607-2; GeoB8610-2; GeoB8611-3; GeoB8613-7; Gravity corer (Kiel type); Indeterminata/varia; Jasminum; Juniperus/Tetraclinis; Labiatae; Latitude of event; Leguminosae; Longitude of event; M37/1; M45/5a; M58/2; Malvaceae; Marker, added; Marker, found; MARUM; Mass; Meteor (1986); MUC; MultiCorer; Myrtaceae; off Northwest Africa; Olea; Pentzia-type; Phillyrea; Pinus; Plantago; Poaceae; Pollen, total; Quercus ilex-type; Quercus robur-type; Rhamnus; SL; Solanaceae; Spores; Spores, trilete; Tamarix; Typha
    Type: Dataset
    Format: text/tab-separated-values, 550 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Bouimetarhan, Ilham; Chiessi, Cristiano Mazur; González-Arango, Catalina; Dupont, Lydie M; Voigt, Ines; Prange, Matthias; Zonneveld, Karin A F (2018): Intermittent development of forest corridors in northeastern Brazil during the last deglaciation: Climatic and ecologic evidence. Quaternary Science Reviews, 192, 86-96, https://doi.org/10.1016/j.quascirev.2018.05.026
    Publication Date: 2024-03-06
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 933 data points
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  • 9
    Publication Date: 2024-03-06
    Keywords: Acacia; Acanthaceae; Aizoaceae; Amaranthaceae/Chenopodiaceae; Apiaceae; Argania spinosa; Artemisia; Aruncus-type; Asphodelus-type; Asteroideae; Brassicaceae; Caryophyllaceae; Cedrus; Centaurea-type; Center for Marine Environmental Sciences; Cichorioideae; Combretaceae; Concentricystes; Convolvulaceae; Corylus; Cyperaceae; ECHo1-1a2; ECHo1-1a3; ECHo1-1a4; ECHo1-2a1; ECHo1-2a2; ECHo1-2a3; ECHo2-1a1; ECHo2-1a2; ECHo2-1a3; ECHo2-2a2; ECHo2-2a3; ECHo2-3a1; ECHo2-4a1; ECHo2-4a2; ECHo2-4a3; ECHo3-1a1; ECHo3-1a2; ECHo3-1a3; ECHo3-3a1; ECHo3-4a1; ECHo3-4a2; Ephedra; Ericaceae; Euphorbia; Euphorbiaceae; Event label; Fabaceae; Indeterminata; Jasminum; Juglans; Juniperus/Tetraclinis; Justicia-type; Labiatae; Leguminosae; Lotus-type; Marker, added; Marker, found; MARUM; Mass; Myrtaceae; Olea; Pentzia-type; Phillyrea; Pinus; Plantago; Poaceae; Pollen, total; Polygalaceae; Polygonaceae; Polygonum; Quercus ilex-type; Quercus robur-type; Rhamnus; Rhus; Rumex; Salix; Selaginella; Solanaceae; Spores; Spores, monolete; Spores, trilete; Tamarix; Tribulus; Typha; Ulmus; Urticaceae; Xanthium-type
    Type: Dataset
    Format: text/tab-separated-values, 1344 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Hahn, Annette; Miller, Charlotte; Andó, Sergio; Bouimetarhan, Ilham; Cawthra, Hayley C; Garzanti, Eduardo; Green, Andrew N; Radeff, Giuditta; Schefuß, Enno; Zabel, Matthias (2018): The provenance of terrigenous components in marine sediments along the east coast of southern Africa. Geochemistry, Geophysics, Geosystems, 19(7), 1946-1962, https://doi.org/10.1029/2017GC007228
    Publication Date: 2024-04-11
    Description: Terrestrial signals in marine sediment archives are often used for paleoclimatic reconstructions. It is therefore important to know the origin of the different terrestrial sedimentary components. The proximity to a river mouth is often the key location to determine the source. Especially in regions with strong ocean currents, such an assumption might,however, lead to considerable misinterpretations. To investigate the source of various terrigenous sediment fractions in southeastern Africa, a region with strong sediment redistribution, we have performed an extensive comparison between terrestrial material (pollen, plant lipids, detrital modes and heavy minerals as well as bulk inorganic geochemical composition) from potential source regions and the same components in the adjacent coastal and continental shelf sediments. Onshore the proxy‐indicators reflect small‐scale diversity in sampling locations and associated environments (riverbank sediments, flood deposits, suspension loads and soils). Nevertheless, the overall trends reflect significant environmental gradients along a SW to NE transect. We note a general comparability of the studied parameters between the continental and marine sediments regardless of their specific differences in transport and depositional characteristics. We propose that the influence of the Agulhas Current affects sediment deposition and distribution only seaward of the mid‐shelf and that pockets of sediment remain preserved in the lee of coastal protrusions where they are protected from erosion. This study provides the essential prerequisite to allow the attribution of temporal variations of compositional changes in marine sediment cores to environmental changes in southeastern Africa.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 6 datasets
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