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Ancient plant remains with special reference to buckthorn, Frangula alnus Mill., pyrenes from Dascyleum, Balikesir, NW Turkey

100%

Donmez E. O., Akyol A. A., Karadag R., Torgan E., Iren K.

Acta Societatis Botanicorum Poloniae

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2017

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tom 86

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nr 1

Carbonized plant remains recovered from the ancient city Dascyleum (Daskyleion) in the province of Balıkesir in northwestern Turkey provide an outline of several phases of plant use in archaic, Hellenistic, and medieval times. At the study site, various crop plant remains of Near Eastern agriculture, including cereals (barley, Hordeum vulgare L. and bread/durum/rivet wheat, Triticum aestivum L. / T. durum Desf. / T. turgidum L.) and pulses [bitter vetch, Vicia ervilia (L.) Willd.; grass pea, Lathyrus sativus L. / L. cicera L.; fava bean, V. faba L.; and chickpea, Cicer arietinum L.] were found. Drupaceous fruits and pyrenes of buckthorn (Frangula alnus Mill.) were also found, probably representing dyes and/or medicines used by the inhabitants of the mound. Archaeometrical analyses of the ancient buckthorn pyrenes by high performance liquid chromatography with photodiode array detector (HPLC-PDA) provide chemical evidence for traces of ancient mordants remaining until the present day. Some of the pulse seed remains retrieved from the medieval layers at the study site were found to have been infested by bruchid beetles (Bruchidae).

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Development of plant communities in the Uroczysko Jezor peatbog indicated by analysis of macrofossil plant remains

84%

Urban D., Tokarz E.

Teka Komisji Ochrony i Kształtowania Środowiska Przyrodniczego

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2014

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tom 11

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Malacological and palynological evidence of Early Pleistocene cooling of the climate in the Carpathian Foreland

84%

Stworzewicz E., Granoszewski W., Wojcik A.

Folia Malacologica

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2012

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tom 20

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nr 1

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Carpological material as an indicator fen peatlands degradation

84%

Kolodziejczyk-Prazmo K., Tomaszewska K.

Polish Journal of Natural Sciences

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2017

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tom 32

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nr 4

The abandonment of agricultural use of drained fen peatlands contributes to intensified moorshing process and, consequently, faster of wetlands areas degradation. Peat mineralization causes the eutrophication of the habitat which, along with changing humidity, enables the presence of so-called non peat-forming plants. Among the seeds and fruit present in the top layer of degraded marshy soils, there may also be carpological material originating from non peat-forming plants. 12 soil profiles from selected post-marsh meadows in western Poland were the subject of this study. The studies found seeds and fruit of 69 plant species in moorsh layers, 42 of which were peat-forming species but as many as 27 were non peat-forming plants. Of the latter the most common were, among others, Juncus effusus and Juncus conglomeratus, Urtica dioica, which were characterized by the highest quantitativeness of fruit and seeds. Among the recorded non peat-forming species almost 50% belonged to Molinio-Arrhenatheretea class, which means they were species connected with semi-natural and anthropogenic meadows occurring on mineral or organic-mineral soils but also characteristic of muck emerging from degraded fen peatlands. Peat-forming species belonged to Phragmitetea and Scheuchzerio-Caricetea nigrae classes. Studies showed that the set of fruit and seeds of non peat-forming plants found in the upper layers of peat deposit was not dependent on the thickness or type of peat from which the moorsh originated, nor was it dependent on geographical location.

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Neogene leaf flora from Gnojna [Opole Prov., SW Poland]

84%

Krajewska K.

Acta Palaeobotanica

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1998

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tom 38

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nr 1

6

Mollusc shell accumulations in North-Eastern Alpine rivers and lakes

84%

Alexandrowicz S. W.

Bulletin of the Polish Academy of Sciences. Earth Sciences

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2001

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tom 49

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nr 2

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Revision of plant macrofossils from the Mazovian interglacial locality Nowiny Zukowskie [SE Poland]

84%

Velichkevich F. Y., Mamakowa K.

Acta Palaeobotanica

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2003

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tom 43

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nr 1

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Taxonomic revision of the collections of plant macrofossils from some localities of Poland now referred to the Vistulian Glaciation

84%

Velichkevich F. Y., Mamakowa K.

Acta Palaeobotanica

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1999

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tom 39

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nr 1

9

Zu Fossilinhalt Kohlegenese und Stratigraphie des Kohlebeckens von Lava in Nordgriechenland

67%

Antoniadis P. A., Rieber E.

Acta Palaeobotanica

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1997

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tom 37

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nr 1

Ograniczanie wyników

Ancient plant remains with special reference to buckthorn, Frangula alnus Mill., pyrenes from Dascyleum, Balikesir, NW Turkey

Development of plant communities in the Uroczysko Jezor peatbog indicated by analysis of macrofossil plant remains

Malacological and palynological evidence of Early Pleistocene cooling of the climate in the Carpathian Foreland

Carpological material as an indicator fen peatlands degradation

Neogene leaf flora from Gnojna [Opole Prov., SW Poland]

Mollusc shell accumulations in North-Eastern Alpine rivers and lakes

Revision of plant macrofossils from the Mazovian interglacial locality Nowiny Zukowskie [SE Poland]

Taxonomic revision of the collections of plant macrofossils from some localities of Poland now referred to the Vistulian Glaciation

Zu Fossilinhalt Kohlegenese und Stratigraphie des Kohlebeckens von Lava in Nordgriechenland