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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2008
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| Online Access: | https://doi.org/10.1594/PANGAEA.830178 |
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| author | Kotthoff, Ulrich Pross, Jörg Müller, Ulrich C Peyron, Odile Schmiedl, Gerhard Schulz, Hartmut Bordon, Amandine |
| author_facet | Kotthoff, Ulrich Pross, Jörg Müller, Ulrich C Peyron, Odile Schmiedl, Gerhard Schulz, Hartmut Bordon, Amandine |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | To unravel the climatic and environmental dynamics in the borderlands of the Aegean Sea during the early and middle Holocene, and notably for the interval of sapropel S1 (S1) formation, we have analysed terrestrial palynomorphs from a marine core in the northern Aegean Sea. The qualitative results were complemented by quantitative pollen-based climate reconstructions. A land-sea correlation was established based on pollen data and sediment lightness measurements from the same core, and previously published benthic foraminifer data from a nearby core. The borderlands of the Aegean Sea underwent a transition from an open vegetation to oak-dominated woodlands between ~10.4 and ~9.5 ka cal BP. A coeval increase in winter precipitation suggests that moisture availability was the main factor controlling Holocene reforestation. The ~50% higher winter precipitation during S1 formation relative to "pre-sapropelic" conditions suggests a strong contribution from the borderlands of the Aegean Sea to the freshwater surplus during S1 formation. The humid and mild winter conditions during S1 formation were repeatedly punctuated by short-term climatic events that caused a partial deforestation and a reorganisation within the broad-leaved arboreal vegetation. In the marine realm, these events are documented by improved benthic oxygenation. The strongest event represents the regional expression of the 8.2 ka cold event and led to an interruption in S1 formation. Except for the interval of S1 formation, the pollen-derived winter temperatures correlate with the smoothed GISP2 K+ series. They support the previously published, marine-based concept that the intensity of the Siberian High strongly controlled the winter climate in the Aegean region. During S1 formation in the Aegean Sea, however, climate conditions in the borderlands were more strongly affected by the monsoonally influenced climate system of the lower latitudes. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_830178 |
| institution | PANGAEA |
| language | en |
| publishDate | 2008 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Palynomorphs from the Lateglacial and Holocene of the Mt-Athos Basin, Aegean Sea Kotthoff, Ulrich Pross, Jörg Müller, Ulrich C Peyron, Odile Schmiedl, Gerhard Schulz, Hartmut Bordon, Amandine Abies; Acer; Adiantum; AGE; Alisma; Alnus; Androsace; Apiaceae; Arctium; Armeria; Artemisia; Asphodelus; Asplenium; Asteraceae; Asteraceae undifferentiated; Betula; Botrychium; Brassicaceae; Butomus; Calluna; Cannabis; Capparis; Carpinus betulus; Carpinus orientalis; Carpinus orientalis/Ostrya-type; Caryophyllaceae; Caryophyllaceae undifferentiated; Celtis; Centaureaceae; Centaurea cyanus-type; Centaurea jacea-type; Centhranthus; Cerastium; Ceratonia; Cheilanthes; Chenopodiaceae; Cirsium; Cistus; Comment; Compositae; Compositae undifferentiated; Coniferae; Convolvulus; Cornus; Corylus; Counting, palynology; Crassulaceae; Crepis-type; Cryptogramma; Cyperaceae; Cystopteris; Daphne; Davallia; DEPTH, sediment/rock; Diphasium; Dipsacaceae; Drosera; Dryopteris; Duvalia; Echinops; Empetrum; Ephedra; Ephedra distachya; Ephedra fragilis; Equisetum; Erica; Ericaceae; Euphorbiaceae; Fabales; Fagus; Filipendula; Fragaria; Fraxinus; Galium; Gentiana; Geranium; Globularia; Gratiola; Gravity corer (Kiel type); Hedera; Helianthemum; Hippophae; Hottonia; Humulus; Isoetes; Iuglans; Juniperus; Knautia; Larix; Leuranthus; Ligustrum; Liliaceae; Liliaceae undifferentiated; Limonium; Linum; Loranthus; Lupinus; Lycopodium; Lycopodium, per unit sediment mass; Lycopodium (added); Lycopodium (counted); Lycopodium spores per tablet; Lycopodium tablets; Lycopodium tablets charge number; M51/3; M51/3_601-2; Mercurialis; Meteor (1986); Myrica; Myriophyllum; Number of trees; Nuphar; Olea; Oleaceae; Ophioglossum; Osmunda; Ostrya; Papaver; Phacelia; Phillyrea; Picea; Pilularia; Pinus; Plantaginaceae; Plantaginaceae undifferentiated; Plantago; Poaceae; Pollen, herbs; Pollen, total; Pollen, tricolpate; Pollen, tricolpate indeterminata; Pollen indeterminata; Polycarpon; Polygonum; Polypodium; Polystichum; Populus; Potentilla-type; Primulaceae; Primulaceae indeterminata; Pteridium; Quercus; Quercus cerris-type; Quercus ilex; Quercus robur; Ranunculaceae; Ranunculaceae indeterminata; Ranunculus; Rhamnus; Rosaceae; Rosaceae undifferentiated; Rubiaceae; Rumex; Salix; Sample mass; Sarcopoterium spinosum; Saxifraga; Scabiosa; Scleranthus; Scrophulariaceae; Scrophulariaceae undifferentiated; Selaginella; Silene; SL; SL152; Sorbus; Sparganium; Spergula; Spergularia; Sphagnum; Spores; Spores, monolete; Spores, trilete; Stellaria; Tamarix; Teucrium; Thalictrum; Thelypteris; Tilia; Typha; Ulmus/Zelkova; Urtica; Valeriana; Valerianella; Viola; Woodsia To unravel the climatic and environmental dynamics in the borderlands of the Aegean Sea during the early and middle Holocene, and notably for the interval of sapropel S1 (S1) formation, we have analysed terrestrial palynomorphs from a marine core in the northern Aegean Sea. The qualitative results were complemented by quantitative pollen-based climate reconstructions. A land-sea correlation was established based on pollen data and sediment lightness measurements from the same core, and previously published benthic foraminifer data from a nearby core. The borderlands of the Aegean Sea underwent a transition from an open vegetation to oak-dominated woodlands between ~10.4 and ~9.5 ka cal BP. A coeval increase in winter precipitation suggests that moisture availability was the main factor controlling Holocene reforestation. The ~50% higher winter precipitation during S1 formation relative to "pre-sapropelic" conditions suggests a strong contribution from the borderlands of the Aegean Sea to the freshwater surplus during S1 formation. The humid and mild winter conditions during S1 formation were repeatedly punctuated by short-term climatic events that caused a partial deforestation and a reorganisation within the broad-leaved arboreal vegetation. In the marine realm, these events are documented by improved benthic oxygenation. The strongest event represents the regional expression of the 8.2 ka cold event and led to an interruption in S1 formation. Except for the interval of S1 formation, the pollen-derived winter temperatures correlate with the smoothed GISP2 K+ series. They support the previously published, marine-based concept that the intensity of the Siberian High strongly controlled the winter climate in the Aegean region. During S1 formation in the Aegean Sea, however, climate conditions in the borderlands were more strongly affected by the monsoonally influenced climate system of the lower latitudes. |
| title | Palynomorphs from the Lateglacial and Holocene of the Mt-Athos Basin, Aegean Sea |
| topic | Abies; Acer; Adiantum; AGE; Alisma; Alnus; Androsace; Apiaceae; Arctium; Armeria; Artemisia; Asphodelus; Asplenium; Asteraceae; Asteraceae undifferentiated; Betula; Botrychium; Brassicaceae; Butomus; Calluna; Cannabis; Capparis; Carpinus betulus; Carpinus orientalis; Carpinus orientalis/Ostrya-type; Caryophyllaceae; Caryophyllaceae undifferentiated; Celtis; Centaureaceae; Centaurea cyanus-type; Centaurea jacea-type; Centhranthus; Cerastium; Ceratonia; Cheilanthes; Chenopodiaceae; Cirsium; Cistus; Comment; Compositae; Compositae undifferentiated; Coniferae; Convolvulus; Cornus; Corylus; Counting, palynology; Crassulaceae; Crepis-type; Cryptogramma; Cyperaceae; Cystopteris; Daphne; Davallia; DEPTH, sediment/rock; Diphasium; Dipsacaceae; Drosera; Dryopteris; Duvalia; Echinops; Empetrum; Ephedra; Ephedra distachya; Ephedra fragilis; Equisetum; Erica; Ericaceae; Euphorbiaceae; Fabales; Fagus; Filipendula; Fragaria; Fraxinus; Galium; Gentiana; Geranium; Globularia; Gratiola; Gravity corer (Kiel type); Hedera; Helianthemum; Hippophae; Hottonia; Humulus; Isoetes; Iuglans; Juniperus; Knautia; Larix; Leuranthus; Ligustrum; Liliaceae; Liliaceae undifferentiated; Limonium; Linum; Loranthus; Lupinus; Lycopodium; Lycopodium, per unit sediment mass; Lycopodium (added); Lycopodium (counted); Lycopodium spores per tablet; Lycopodium tablets; Lycopodium tablets charge number; M51/3; M51/3_601-2; Mercurialis; Meteor (1986); Myrica; Myriophyllum; Number of trees; Nuphar; Olea; Oleaceae; Ophioglossum; Osmunda; Ostrya; Papaver; Phacelia; Phillyrea; Picea; Pilularia; Pinus; Plantaginaceae; Plantaginaceae undifferentiated; Plantago; Poaceae; Pollen, herbs; Pollen, total; Pollen, tricolpate; Pollen, tricolpate indeterminata; Pollen indeterminata; Polycarpon; Polygonum; Polypodium; Polystichum; Populus; Potentilla-type; Primulaceae; Primulaceae indeterminata; Pteridium; Quercus; Quercus cerris-type; Quercus ilex; Quercus robur; Ranunculaceae; Ranunculaceae indeterminata; Ranunculus; Rhamnus; Rosaceae; Rosaceae undifferentiated; Rubiaceae; Rumex; Salix; Sample mass; Sarcopoterium spinosum; Saxifraga; Scabiosa; Scleranthus; Scrophulariaceae; Scrophulariaceae undifferentiated; Selaginella; Silene; SL; SL152; Sorbus; Sparganium; Spergula; Spergularia; Sphagnum; Spores; Spores, monolete; Spores, trilete; Stellaria; Tamarix; Teucrium; Thalictrum; Thelypteris; Tilia; Typha; Ulmus/Zelkova; Urtica; Valeriana; Valerianella; Viola; Woodsia |
| url | https://doi.org/10.1594/PANGAEA.830178 |