Sustainability of agricultural and wild cereals to aerotechnogenic exposure

Author(s):  
Victor Chaplygin ◽  
Saglara Mandzhieva ◽  
Tatiana Minkina ◽  
Svetlana Sushkova ◽  
Ridvan Kizilkaya ◽  
...  
Keyword(s):  
1994 ◽  
Vol 59 (2) ◽  
pp. 238-263 ◽  
Author(s):  
Katherine I. Wright

Ground-stone tools and hunter-gatherer subsistence in late Pleistocene southwest Asia are examined in light of ethnographic and experimental data on processing methods essential for consumption of various plant foods. In general, grinding and pounding appear to be labor-intensive processing methods. In particular, the labor required to make wild cereals edible has been widely underestimated, and wild cereals were unlikely to have been “attractive” to foragers except under stress conditions. Levantine ground-stone tools were probably used for processing diverse plants. The earliest occurrence of deep mortars coincides with the glacial maximum, camp reoccupations, the onset of increasingly territorial foraging, and the earliest presently known significant samples of wild cereals. Two major episodes of intensification in plant-food processing can be identified in the Levant, coinciding respectively with the earliest evidence for sedentism (12,800-11,500 B.P.) and the transition to farming (11,500-9600 B.P.). The latter episode was characterized by rising frequencies of grinding tools relative to pounding tools, and suggests attempts to maximize nutritional returns of plants harvested from the limited territories characteristic of sedentary foraging and early farming. This episode was probably encouraged by the Younger Dryas, when density and storability of foods may have outweighed considerations of processing costs.


Plants ◽  
2018 ◽  
Vol 7 (3) ◽  
pp. 74 ◽  
Author(s):  
Eugene Rogozhin ◽  
Dmitry Ryazantsev ◽  
Alexey Smirnov ◽  
Sergey Zavriev

Cereal-derived bioactive peptides with antimicrobial activity have been poorly explored compared to those from dicotyledonous plants. Furthermore, there are a few reports addressing the structural differences between antimicrobial peptides (AMPs) from cultivated and wild cereals, which may shed light on significant varieties in the range and level of their antimicrobial activity. We performed a primary structure analysis of some antimicrobial peptides from wild and cultivated cereals to find out the features that are associated with the much higher antimicrobial resistance characteristic of wild plants. In this review, we identified and analyzed the main parameters determining significant antifungal activity. They relate to a high variability level in the sequences of C-terminal fragments and a high content of hydrophobic amino acid residues in the biologically active defensins in wild cereals, in contrast to AMPs from cultivated forms that usually exhibit weak, if any, activity. We analyzed the similarity of various physicochemical parameters between thionins and defensins. The presence of a high divergence on a fixed part of any polypeptide that is close to defensins could be a determining factor. For all of the currently known hevein-like peptides of cereals, we can say that the determining factor in this regard is the structure of the chitin-binding domain, and in particular, amino acid residues that are not directly involved in intermolecular interaction with chitin. The analysis of amino acid sequences of alpha-hairpinins (hairpin-like peptides) demonstrated much higher antifungal activity and more specificity of the peptides from wild cereals compared with those from wheat and corn, which may be associated with the presence of a mini cluster of positively charged amino acid residues. In addition, at least one hydrophobic residue may be responsible for binding to the components of fungal cell membranes.


Nature Plants ◽  
2018 ◽  
Vol 4 (2) ◽  
pp. 71-81 ◽  
Author(s):  
Anna Maria Mercuri ◽  
Rita Fornaciari ◽  
Marina Gallinaro ◽  
Stefano Vanin ◽  
Savino di Lernia
Keyword(s):  

Author(s):  
Graeme Barker

As Chapter 1 described, the origins of agriculture have been debated by archaeologists for most of the discipline’s history. The topic has been a particular focus of archaeological field and laboratory research from the middle of the twentieth century onwards. The number of suggested causes that has been proposed over the years for why prehistoric foragers might have become farmers appears almost endless, with everybody joining the party including the lunatic fringe (Table 10.1)! The main course of scholarly debate, though, has been conditioned partly by changing theoretical currents in archaeological thinking and perceptions of present-day or recent foraging and farming societies (Chapter 2) and partly by the application of improved methodologies (Chapter 3). In the regional studies that form the core of this book, I have concentrated primarily on the archaeological evidence left by prehistoric foragers and farmers, in all its richness, from stones to bones to rock art to starch grains (and more besides), though I have also made reference to the contributions of the several other disciplines that have contributed to the debate, including anthropology, ecology, ethnoarchaeology, genetics, geomorphology, linguistics, and palynology (pollen analysis). The next sections briefly review the principal themes that have emerged from those studies, as the basis for some concluding reflections on whether it is possible or desirable to arrive at an overarching explanation or set of explanations for why foragers became farmers. South-West Asia has probably been the focus of more debate on discussions about the origins of agriculture than anywhere else in the world. On the present evidence what can clearly be recognized as the Eurasian system of mixed farming (the cultivation of wheat and barley and the herding of sheep and goats) seems to have developed in this region very early in the Holocene. It underpinned the dramatic development of PPNB villages in and around the ‘hilly flanks’ of the Fertile Crescent some 1,000 years into the Holocene, c.8500 BC. The parts of South-West Asia where these villages came into being were also places where wild cereals, sheep, and goats were naturally located.


2016 ◽  
Vol 113 (15) ◽  
pp. 3997-4002 ◽  
Author(s):  
Gideon Hartman ◽  
Ofer Bar-Yosef ◽  
Alex Brittingham ◽  
Leore Grosman ◽  
Natalie D. Munro

The climatic downturn known globally as the Younger Dryas (YD; ∼12,900–11,500 BP) has frequently been cited as a prime mover of agricultural origins and has thus inspired enthusiastic debate over its local impact. This study presents seasonal climatic data from the southern Levant obtained from the sequential sampling of gazelle tooth carbonates from the Early and Late Natufian archaeological sites of Hayonim and Hilazon Tachtit Caves (western Galilee, Israel). Our results challenge the entrenched model that assumes that warm temperatures and high precipitation are synonymous with climatic amelioration and cold and wet conditions are combined in climatic downturns. Enamel carbon isotope values from teeth of human-hunted gazelle dating before and during the YD provide a proxy measure for water availability during plant growth. They reveal that although the YD was cooler, it was not drier than the preceding Bølling–Allerød. In addition, the magnitude of the seasonal curve constructed from oxygen isotopes is significantly dampened during the YD, indicating that cooling was most pronounced in the growing season. Cool temperatures likely affected the productivity of staple wild cereal resources. We hypothesize that human groups responded by shifting settlement strategies—increasing population mobility and perhaps moving to the warmer Jordan Valley where wild cereals were more productive and stable.


Euphytica ◽  
1984 ◽  
Vol 33 (3) ◽  
pp. 717-735 ◽  
Author(s):  
Eviatar Nevo ◽  
Avigdor Beiles ◽  
Yitzchak Gutterman ◽  
Nurith Storch ◽  
Diane Kaplan

2018 ◽  
pp. 83-89
Author(s):  
Евгений (Evgenij) Александрович (Аleksandrovich) Бондаревич (Bondarevich)

In the course of studying the content of free amino acids in dry and germinating grains of wild cereals, some biochemical features of their dynamics were revealed depending on the osmotic pressure. In most species, except Agropyron cristatum, a significant increase in the concentration of amino acids occurred in the control on the first day after the start of the experiment; in the subsequent period, their decrease was observed. For Agropyron cristatum, a decrease in the index and a smooth increase after the first day were observed. Under the influence of osmolyte, the tendency to mobilize amino acids has changed and in some species (Stipa krylovii, Melica virgata, Melica turczaninowiana) the maximum amounts were observed on the first day from the beginning of the experiment, in the others to the second day. The total amount of free amino acids in the control and in the test was not significantly different. There was also a rapid mobilization of proteinogenic amino acids with increasing osmotic stress for the widespread Stipa krylovii and Agropyron cristatum in the region. A similar trend was noted for the xerophyte Tripogon chinensis. For grasses with a narrow ecological niche, which are characterized by xeromesophilia, osmotic stress suppressed the rapid mobilization of free amino acids. The content of individual groups of amino acids under the influence of osmotic stress was characterized by significant differences for species of the Melica genus in the number of acidic amino acids, for Tripogon chinensis an increase in the content of basic amino acids, and for Agropyron cristatum by a decrease in their concentration.


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