Studying the preservation of plant macroremains from waterlogged archaeological deposits for an assessment of layer taphonomy

2017 ◽  
Vol 246 ◽  
pp. 120-145 ◽  
Author(s):  
Ferran Antolín ◽  
Bigna L. Steiner ◽  
Örni Akeret ◽  
Christoph Brombacher ◽  
Marlu Kühn ◽  
...  
Keyword(s):  
2016 ◽  
Vol 72 (3-4) ◽  
pp. 239-250 ◽  
Author(s):  
Dieter Uhl ◽  
André Jasper

New discoveries of fossil plant macroremains from the Remigiusberg Formation (lowermost Rotliegend group) considerably enlarge our knowledge about the flora of the basal-most part of the lithostratigraphically defined Rotliegend group within the Saar-Nahe Basin in SW-Germany. Most taxa are plants that grew in relatively humid habitats near rivers, or around margins of the lake in whose sediments the plant macroremains were found. This, together with previously reported palynological data, suggests that the wetlands in which these plants grew were large enough to act as taphonomical barriers against the deposition of plant macroremains from dryer habitats. Based on some of the new taxa, it is also possible to constrain the base of the biostratigraphic Autunia conferta zone in this basin, a task that was not possible before, due to the scarcity of macrofloristic data from the basal Rotliegend group. The new data provide evidence that the upper part of the Remigiusberg Formation is probably not older than late Gzhelian. This corresponds to earlier biostratigraphic interpretations based on palaeozoological remains.


2008 ◽  
Vol 4 (2) ◽  
pp. 205-212 ◽  
Author(s):  
Ahmed G. Fahmy ◽  
Salah Khodary ◽  
Mohamed Fadl ◽  
Ibrahim El-Garf

2014 ◽  
Vol 64 (3) ◽  
pp. 281-309 ◽  
Author(s):  
Maria Barbacka ◽  
Grzegorz Pacyna ◽  
Anna Feldman-Olszewska ◽  
Jadwiga Ziaja ◽  
Emese Bodor

Abstract Plant macroremains from five boreholes in Poland were studied. Two of them (Huta OP-1 and Studzianna) from the northern margin of the Holy Cross Mountains, yielded several taxa. In the other three boreholes determinable fos-sil plants were sporadic, albeit important. Most of the taxa from the Huta OP-1 and Studzianna boreholes are typi-cal of the European Early Jurassic (Hettangian and Sinemurian). Both localities, although close to one another, show incertae sedis, Desmiophyllum harrisii phytes and conifers (a new species incertae sedis, Desmiophyllum harrisii Barbacka et Pacyna is herein proposed), which would suggest rather wet and warm conditions. This flora is typical of the European Province of the Euro-Sinian Region. In Studzianna the Siberian elements dominate, gymnosperms, mainly Czekanowskiales, which in-dicate a drier and colder environment. The palaeobotanical data correspond to the results of clay mineral studies, in particular the kaolinite/illite ratio in the source formations. The kaolinite content confirms a decrease in temperature and a reduction in rainfall in the late Early Hettangian and the latest Hettangian in the area.


The Holocene ◽  
2014 ◽  
Vol 24 (2) ◽  
pp. 188-197 ◽  
Author(s):  
Laura Caruso Fermé ◽  
Maria Teresa Civalero

1981 ◽  
Vol 59 (11) ◽  
pp. 2178-2188 ◽  
Author(s):  
Richard I. Ford

In 1855 Alphonse de Candolle challenged his contemporaries to describe and to explain the geographical and historical distribution of economic plants. It was only in the 20th century, however, that ethnobotany, the direct interrelationships between human populations and their plant environment, and paleoecology and archaeology could combine to delineate from antiquity the history of economic plant usages, to describe the ecological changes introduced by humans, and to detail the cultural determinants of new plant evolution.The prehistory of plant uses depends upon paleoecological and archaeological data. Pollen and plant macroremains have demonstrated that only during the past 2000 years in North America have humans expanded the number of taxa they used. Ecologically humans have become important agents for transforming the landscape during the same time period in areas where plant food production was practiced. Fire was the principle agent for clearing the land and plant husbandry intensified the disjunction of plant species. Humans, then, became significant ecological and evolutionary factors in the landscape with the introduction of domesticated cucurbits from Mexico in the eastern United States about 5000 years ago. It was not until 3000 years ago that indigenous North American Helianthus and Iva were domesticated and other plants were cultivated and introduced beyond their known ranges. In the Southwest com cultivation started 3000 years ago and spread rapidly as a staple and source of phytogeographical changes. Com-field farming in the past 1000 years by prehistoric Americans created new habitats and had the greatest effect on the geographical distribution of plants. Ethnobotany and its associated discipline, archaeobotany, have brought an indispensible complement to paleoecology and a new dimension to historical phytogeography.


2016 ◽  
Vol 43 ◽  
pp. 413-420
Author(s):  
Tjaša Tolar ◽  
Anton Velušček

The results of plant macroremains studies of the Eneolithic (c. 3160–3100 cal BC) lakeshore settlement at Stare gmajne on the Ljubljansko barje in Slovenia are presented. Archaeobotanical material was collected in two different ways: (1) systematic surface sampling from the cultural layer, and (2) judgement sampling from an incompletely burnt large loom-weight. The preservation state and the spectra of plant macroremains were different in both types of samples. The first study primarily deals with the waterlogged plant remains of various types and taxa, while the second deals with carbonised and half-carbonised cereal macroremains, mostly chaff. Both studies confirm the cultivation of main crops: emmer, einkorn and barley.


2015 ◽  
Vol 55 (1) ◽  
pp. 68-93 ◽  
Author(s):  
Renata Stachowicz-Rybka

Abstract Lacustrine sediments at the Łuków site bear a record of the Ferdynandovian interglacial, correlated with Marine Isotope Stage (MIS) 13-15, including two warm periods of interglacial rank (climatostratigraphic units Ferdynandovian 1 and 2) separated by cooling/glaciation (Ferdynandovian 1/2). On the basis of plant macroremains analysis, the type of local vegetation in the lake and its surroundings as well as changes in climate, trophic conditions and water level were reconstructed in detail. Ferdynandovian 1 was a time of development of tall sedge swamps. The presence of Najas marina and N. minor also suggests high levels of eutrophication, particularly in the younger part of the climatic optimum. The occurrence of Zannichellia palustris indicates habitats of variable water level and high salt content. In the terminocratic phase of Ferdynandovian 1, the communities showed the reoccurrence of Betula nana, B. humilis and Larix sp., the disappearance of thermophilous trees, and the intensification of succession processes linked to climate cooling. In the cool Ferdynandovian 1/2, Betula nana and Cenococcum geophilum increased their frequencies, most likely due to enhanced supply of mineral matter to the basin. During Ferdynandovian 2, the next climate warming of interglacial rank, communities of aquatic vegetation with the highest share of thermophilous taxa included the extinct Aldrowanda borysthenica, Brasenia borysthenica, and Scirpus atroviroides, as well as Cyperus glomeratus, a species not presently found in the flora of Poland. Another cooling in the Sanian 2 (Elsterian 2) glaciation is indicated by the development of peat communities, with numerous Carex sp., Menyanthes trifoliata, Eriophorum vaginatum, and Andromeda polifolia, accompanied by the extinct Carex paucifloroides, Caulinia macrosperma, and Potamogeton praemaackianus. The provided description of the Ferdynandovian succession includes taxa which are extinct, not found in the Polish flora nowadays, or characteristic of a climatic context. The identified species included Brasenia borysthenica, Aldrovanda borysthenica, Caulinia macrosperma, Potamogeton praemaackianus, Scirpus atroviroides, Cyperus glomeratus, Eleocharis praemaximoviczii, Nymphaea cinerea, and Ranunculus gailensis. It has not yet been resolved whether the flora of Łuków includes Euryale sp., a particularly important taxon.


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