Some macroscopic plant-remains reffered to the betulaceæ from the Karewa Deposits of Kashmir

1945 ◽  
Vol 22 (5) ◽  
pp. 257-273
Author(s):  
G. S. Puri
Keyword(s):  
Plant Remains ◽  
Karewa Deposits

‘Robenhausien’ in the Hunterian Museum

1981 ◽  
Vol 8 (1) ◽  
pp. 1-12
Author(s):  
Isobel M Hughes
Keyword(s):  
Organic Materials ◽  
Neolithic Period ◽  
Plant Remains ◽  
Neolithic Europe ◽  
The University

Summary A report is presented of a study of the material from Robenhausen and other sites of the Neolithic period in Switzerland, part of the Bishop Collection in the Hunterian Museum, the University of Glasgow. The material is described and its likely setting within the cultural sequence of the Swiss Neolithic is discussed. The importance of the collection is seen to lie in the finds of organic materials, artefacts and macroscopic plant remains, which afford a rare glimpse of detail in craftsmanship and husbandry in Neolithic Europe.

Perspective of using fusariosis resistant varieties of lupines in organic farming

2018 ◽  
Vol 1 (94) ◽  
pp. 45-50
Author(s):  
M.S. Korniychuk ◽  
N.V. Tkachenko
Keyword(s):  
Organic Farming ◽  
Crop Rotation ◽  
Crude Protein ◽  
Organic Production ◽  
High Protein ◽  
Mineral Fertilizers ◽  
Resistant Varieties ◽  
Plant Remains ◽  
Digestible Protein ◽  
Protein Feed

The expediency of fusarium resistant lupines usage in organic farming for improving soil fertility and producing high protein feed for livestock is justified in this article. Organic production excludes the use of mineral fertilizers and pesticides. In these circumstances, increases the value of cultures that positively affect the fertility of soils and their phytosanitary status. These crops include annual fodder lupine (yellow, white and angustifolia), especially varieties that are resistant to disease. Having the highest nitrogen-fixing ability among annual legume crops, lupins, depending on the type and conditions of cultivation, can accumulate from 80 to 300 kg/ha of environmentally pure symbiotic nitrogen in biomass. Plowing the green mass (30-45 t/ha) is equivalent to the corresponding amount of manure or introduction of 5-7 t/ha of ammonium nitrate. 30 kg/ha of phosphorus and 50 kg/ha of potassium are entering the soil with plant remains. Therefore, lupine provides itself with nutrients and still leaves up to 150 kg/ha of nitrogen in the soil after harvesting for subsequent crops in crop rotation. In organic production, fusariosis resistant varieties of lupines are also interesting as a source of high protein feeds for livestock. They are building up to 60 t/ha of biomass, which contains more than one ton of digestible protein. In grain of the fodder varieties contains 40-52% of crude protein, 5.5-6.0% of fat, 10-12% of sugar. The characteristic of fusarium resistant varieties of lupins (yellow, white and angustifolia), created in the NSC "Institute of Agriculture NAAS" and included in the Register of Plant Varieties of Ukraine is presented in this article. These varieties are practically not affected by fusariosis under the production conditions and do not require the use of fungicides during the growing season. They can be grown in crop rotation with a return period of 2-3 years, whereas for unstable it took 6-7 years. Because of the inability to use in organic farming fungicide to prevent crop losses from anthracnose, it is necessary to use predominantly angustifolia lupine varieties, which are now more tolerant to this disease, prevent sowing of infected seeds and adhere to crop rotation. Fusarium-resistant varieties of lupins are suitable for cultivation in poucous and sown crops, and in mixtures with other crops.

Plant Remains from Khirokitia in Cyprus

Paléorient ◽  
1975 ◽  
Vol 3 (1) ◽  
pp. 281-284 ◽  
Author(s):  
J. G. Waines ◽  
Nicholas P. Stanley Price
Keyword(s):  
Plant Remains

Gendered Places and Depositional Histories: Reconstructing a Menstrual Lodge in the Interior Northwest

2019 ◽  
Vol 84 (3) ◽  
pp. 400-419 ◽  
Author(s):  
Molly Carney ◽  
Jade d'Alpoim Guedes ◽  
Kevin J. Lyons ◽  
Melissa Goodman Elgar
Keyword(s):  
Low Temperature ◽  
Pacific Northwest ◽  
Thin Section ◽  
Archaeological Record ◽  
Columbia Plateau ◽  
The North ◽  
Plant Remains ◽  
History Of ◽  
Experimental Firing ◽  
River Inundation

This project considered the deposition history of a burned structure located on the Kalispel Tribe of Indians ancestral lands at the Flying Goose site in northeastern Washington. Excavation of the structure revealed stratified deposits that do not conform to established Columbia Plateau architectural types. The small size, location, and absence of artifacts lead us to hypothesize that this site was once a non-domestic structure. We tested this hypothesis with paleoethnobotanical, bulk geoarchaeological, thin section, and experimental firing data to deduce the structural remains and the post-occupation sequence. The structure burned at a relatively low temperature, was buried soon afterward with imported rubified sediment, and was exposed to seasonal river inundation. Subsequently, a second fire consumed a unique assemblage of plant remains. Drawing on recent approaches to structured deposition and historic processes, we incorporate ethnography to argue that this structure was a menstrual lodge. These structures are common in ethnographic descriptions, although no menstrual lodges have been positively identified in the archaeological record of the North American Pacific Northwest. This interpretation is important to understanding the development and time depth of gendered practices of Interior Northwest groups.

scholarly journals Holocene vegetation record of upland northern Calabria, Italy: Environmental change and human impact

The Holocene ◽  
2019 ◽  
Vol 29 (4) ◽  
pp. 633-647 ◽  
Author(s):  
Jan Sevink ◽  
Corrie C Bakels ◽  
Peter AJ Attema ◽  
Mauro A Di Vito ◽  
Ilenia Arienzo
Keyword(s):  
Bronze Age ◽  
Forest Decline ◽  
Human Impacts ◽  
Time Frame ◽  
Archaeological Record ◽  
Pollen Data ◽  
Plant Remains ◽  
Middle Bronze Age ◽  
Climatic Event ◽  
Mobile Pastoralism

Earlier studies on Holocene fills of upland lakes (Lago Forano and Fontana Manca) in northern Calabria, Italy, showed that these hold important palaeoecological archives, which however remained poorly dated. Their time frame is improved by new 14C dates on plant remains from new cores. Existing pollen data are reinterpreted, using this new time frame. Two early forest decline phases are distinguished. The earliest is linked to the 4.2 kyr BP climatic event, when climate became distinctly drier, other than at Lago Trifoglietti on the wetter Tyrrhenian side, where this event is less prominent. The second is attributed to human impacts and is linked to middle-Bronze Age mobile pastoralism. At Fontana Manca (c. 1000 m a.s.l.), it started around 1700 BC, in the higher uplands a few centuries later (Lago Forano, c. 1500 m a.s.l.). In the Fontana Manca fill, a thin tephra layer occurs, which appears to result from the AP2 event (Vesuvius, c. 1700 BC). A third, major degradation phase dates from the Roman period. Land use and its impacts, as inferred from the regional archaeological record for the Raganello catchment, are confronted with the impacts deduced from the palaeoarchives.

The contribution of archaeological plant remains in tracing the cultural history of Mediterranean trees: The example of the Roman harbour ofNeapolis

The Holocene ◽  
2015 ◽  
Vol 26 (4) ◽  
pp. 603-613 ◽  
Author(s):  
Emilia Allevato ◽  
Antonio Saracino ◽  
Silvio Fici ◽  
Gaetano Di Pasquale
Keyword(s):  
Cultural History ◽  
Plant Remains ◽  
History Of

Fossil Mosses from the Bisaccate Zone of the Mid-Eocene Allenby Formation, British Columbia

1974 ◽  
Vol 11 (3) ◽  
pp. 409-421 ◽  
Author(s):  
Marian Kuc
Keyword(s):  
British Columbia ◽  
Middle Eocene ◽  
Plant Tissues ◽  
Plant Remains ◽  
Lake Bottom ◽  
White Colour

New fossil taxa (Ditrichites fylesi, Muscites maycocki, M. ritchiei, Palaeohypnum jovet-asti and P. steerei); unnamed moss and moss-like fossils, detrital fragments of various plant tissues, and paleobotanical evidence of the bisaccate zone are described from the Middle Eocene Allenby Formation near Princeton, British Columbia. These remains occur in laminated, tuffaceous, silty and pyroclastic shale, deposited under lacustrine conditions.Detailed examination of the various laminae indicates that beds of white colour and composed of coarser silt grains are poor in fossils and could be related to periods of decreasing bioproduction; less silty and darker coloured beds are rich in macro- and microfossils and could be related to periods of extensive bioproduction. The rock features, lamination, and distribution of macrofossils indicate the slow and undisturbed accumulation of plant remains on a lake bottom.

Quantifying macroscopic plant remains

1992 ◽  
Vol 73 (1-4) ◽  
pp. 117-132 ◽  
Author(s):  
R.N.L.B. Hubbard ◽  
A. Clapham
Keyword(s):  
Plant Remains
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