Neogene of the mediterranean tethys and partethys: Stratigraphic correlation tables and sediment distribution maps, volumes 1 and 2

1991 ◽  
Vol 20 (2) ◽  
pp. 189-190
Author(s):  
Raymond L. Bernor
Bothalia ◽  
1983 ◽  
Vol 14 (3/4) ◽  
pp. 511-515 ◽  
Author(s):  
J. -P. Lebrun

THE FLORA IN THE SOUTHERN SAHARA MOUNTAIN MASSES: ILLUSIVE AND TRUE ENDEMIC SPECIES The mountain masses in the southern part of the Sahara, namely Hoggar, Tassili n 'Ajjer, Air, Tibesti, Ennedi, Jebel Marra and Gebel Elba, have fascinated botanists to such an extent that there has been successive and even multiple creation of new species. This situation can be partly explained by the fact that those who were interested in these areas, although undoubtedly world experts in the Mediterranean area, have less knowledge of the African tropical flora. As a result, certain botanical literature, some quite recent, abounds in binomials, some merely synonyms of older names of well-known species. The problem is aggravated by the fact that a number of authors do not keep up with recent literature. A breakdown of the 85 species previously accepted as endemics reveals that: 37 were incorrectly identified (Table I) ; 7 changed their names either for systematic or nomenclatural reasons (Table 2); I is known only from the type (Quezelia) and requires further collection; 31 belong to difficult genera and require further study (p. 513); and 9 are true endemics (p. 514). This study shows that the number of endemic species from the mountainous enclaves in the dry northern-tropical areas is considerably lower than previously estimated. With more material and with the aid of distribution maps, it is now possible to put the number of true endemics at 12 species.


2021 ◽  
Vol 14 (20) ◽  
Author(s):  
Rachna Pillai ◽  
Nisha Nayakkam Valappil ◽  
Dinesh Aynipulli Chulli Parambil

Zootaxa ◽  
2018 ◽  
Vol 4379 (2) ◽  
pp. 151
Author(s):  
LARA-SOPHIE DEY ◽  
ALIREZA SABOORI ◽  
SEYED HOSSEIN HODJAT ◽  
MAHDI TORK ◽  
FELIX PAHLOW ◽  
...  

Sphingonotus is a species-rich genus of band-winged grasshoppers (Oedipodinae), comprising more than 170 species, with its diversity hotspots in the Mediterranean, and in Central and Eastern Asia. Iran represents one of the countries with the highest species diversity for the genus with a total of 31 recorded species. However, no study so far has provided a faunistic overview and no identification keys are available. Here, we present an annotated list of all Sphingonotus species found in Iran derived from records from field observations, museum collections and literature data. Based on morphological and distribution data we synonymize Sphingonotus intutus Saussure, 1888 syn. nov. under Sphingonotus nebulosus persa Saussure, 1884 and Sphingonotus obscuratus transcaspicus Uvarov, 1925 syn. nov. under Sphingonotus obscuratus brunneri Saussure, 1884. We present images of representative specimens (mostly types) of all species, as well as distribution maps and ecological data. Finally, we provide an online key to all known species of Sphingonotus from Iran, which will continuously be updated. 


2020 ◽  
Vol 105 (2) ◽  
pp. 195-231
Author(s):  
Alicia Vicente ◽  
Mª Ángeles Alonso ◽  
Manuel B. Crespo

Biscutella L. ser. Biscutella (= Biscutella ser. Lyratae Malin.) comprises mostly annual or short-lived perennial plants occurring in the Mediterranean basin and the Middle East, which exhibit some diagnostic floral features. Taxa in the series have considerable morphological plasticity, which is not well correlated with clear geographic or ecologic patterns. Traditional taxonomic accounts have focused on a number of vegetative and floral characters that have proved to be highly variable, a fact that contributed to taxonomic inflation mostly in northern Africa. A detailed study and re-evaluation of morphological characters, together with recent phylogenetic data based on concatenation of two plastid and one nuclear region sequence data, yielded the basis for a taxonomic reappraisal of the series. In this respect, a new comprehensive integrative taxonomic arrangement for Biscutella ser. Biscutella is presented in which 10 taxa are accepted, namely seven species and three additional varieties. The name B. eriocarpa DC. is reinterpreted and suggested to include the highest morphological variation found in northern Morocco. Its treatment here accepts two varieties, one of which is described as new (B. eriocarpa var. riphaea A. Vicente, M. Á. Alonso & M. B. Crespo). In addition, the circumscriptions of several species, such as B. boetica Boiss. & Reut., B. didyma L., B. lyrata L., and B. maritima Ten., are revisited. Nomenclatural types, synonymy, brief descriptions, cytogenetic data, conservation status, distribution maps, and identification keys are included for the accepted taxa, with seven lectotypes and one epitype being designated here.


2021 ◽  
Author(s):  
Daphnie Galvez ◽  
Svenja Papenmeier ◽  
Alexander Bartholomä ◽  
Karen Helen Wiltshire

<p>Recent studies on seafloor mapping have presented different modelling methods to map and classify marine sediment distribution. However, are these methods classify different sediment classes the same way? And how do we choose the right model for a certain set of sediment classes? In this study, we aim to address these issues by using ensemble modelling to map the distribution of different sediment class on a dynamic, shallow continental shelf. Our data were derived from side-scan mosaics and multibeam data repeatedly collected from 2016 to 2018 in the Sylt Outer Reef (German Bight). We used a probabilistic approach for each class separately and then compared the predicted probability for each class, to see which class is more likely to be assigned to the location. Each sediment class was predicted using a combination of different classification modelling techniques, and then the result of these models was ensembled to produced one final prediction. This approach avoids selecting one single method, limits model selection bias and can provide information on the trends and variation across models.  Furthermore, we also looked on the temporal changes in sediment distributions by comparing the sediment class predictions from 2016 to 2018.</p><p>Our analysis suggest that combining different modelling techniques  (i.e. random forest, boosting regression trees etc.) provide higher predictive accuracy than using one single modelling method. The resulting sediment distribution maps are more objective and are produced faster than manual delineated maps often considered by stakeholders. We also identify some limitations in having small sample size and we proposed that by combining certain models and choosing the proper amount of pseudo-absence or background data can address this issue.</p>


Author(s):  
Graeme Barker

Africa, the cradle of humankind several million years ago, was also where anatomically modern humans first developed over 150,000 years ago. Yet our understanding of how these people eventually became farmers is still very limited. A generation ago Thurston Shaw commented that, in comparison with other parts of the world, ‘Africa lags behind. . . in relation to archaeological research and in knowledge about the beginnings of food production’ (Shaw, 1977: 108). Ann Stahl’s review of the topic a few years later made the same observation: ‘research into the origins of African agriculture lags ten to fifteen years behind studies of early agriculture elsewhere’ (Stahl, 1984: 19). In many regions, archaeologists in the 1970s and 1980s were still attempting to establish the most basic chronological framework of artefactual sequences, let alone recover the biological remains that could show when agricultural activities began (Hall, 1996). Many parts of the continent have endured decades of political unrest and military conflict, making archaeological fieldwork impossible for long periods. The equatorial forests are particularly under-researched because of the combination of political unrest, the difficulties of conducting fieldwork in forest, and poor preservation conditions of organic remains. Our understanding of the archaeological history of human settlement in these vast regions is still extremely rudimentary. For countries grappling with tremendous problems of underdevelopment, funding archaeologists in museums and universities can inevitably be a low priority. The number of professional archaeologists engaged in fieldwork on the African continent, indigenous Africans especially, is still extremely small. Distribution maps of archaeological sites are often primarily an indication of where archaeologists have been able to work. Despite these considerable challenges, however, recent studies have started to transformlong-standing ideas about when, how, and why people in Africa started to practise plant and animal husbandry (Fig. 8.1). The northern margins of the continent are Mediterranean in climate and environment, and the beginnings of farming there are best understood as part of the wider settlement history of the Mediterranean basin discussed in the next chapter. The Saharan desert in places reaches right to the coast, for example at Libya’s Gulf of Sirte, but elsewhere the Mediterranean zone can be up to 200 kilometres deep, notably in the mountainous region known as the Maghreb that embraces much of Morocco, northern Algeria, and northern Tunisia.


Antiquity ◽  
1932 ◽  
Vol 6 (22) ◽  
pp. 185-201 ◽  
Author(s):  
Miles Burkitt ◽  
V. Gordon Childe

When the Editor of ANTIQUITY approached the authors and suggested that some of his readers would welcome a visual table showing the occurrence and sequence of the different prehistoric cultures, the matter did not seem to be one of outstanding difficulty. When the time came, however, to produce the work, it was found to be quite otherwise. Perhaps the ideal method would have been to prepare a series of gigantic distribution maps of the area to be covered (Europe, the Mediterranean Basin and adjacent regions) during the different prehistoric periods. But the preparation and publication of such maps on a scale large enough to be at all helpful would have presented insuperable difficulties. The more diagrammatic method which has been adopted divides up the map into several geographical areas which will be found heading the various columns of the table. These areas have been chosen and arranged as conveniently as possible in the light of the general distribution of the early and later prehistoric cultures.It must always be remembered, however, that the spread of a culture from its area of origin corresponds to the ever-widening rings formed by a stone which is cast into a pond—its influence lessens as we get farther from the centre of diffusion. It is not easy to represent this lessening influence diagrammatically. Of course when the industries of a culture have spread widely over a neighbouring area, its name appears in the appropriate column of the table. Where, however, they are only very rarely found, perhaps as the last, faintest ripple of the circles, or where, as with the Solutrean culture in Spain south of the Pyrenees, they are only present in a small corner of the area adjacent to another thickly sprinkled area (France) whence they have clearly percolated, it would have presented an erroneous picture to have cited the culture-name.


2013 ◽  
Vol 71 (4) ◽  
pp. 867-881 ◽  
Author(s):  
Sigrid Elvenes ◽  
Margaret F. J. Dolan ◽  
Pål Buhl-Mortensen ◽  
Valérie K. Bellec

Abstract Maps of surficial sediment distribution and benthic habitats or biotopes provide invaluable information for ocean management and are at the core of many seabed mapping initiatives, including Norway's national offshore mapping programme MAREANO (www.mareano.no). Access to high-quality multibeam echosounder data (bathymetry and backscatter) has been central to many of MAREANO's mapping activities, but in order to maximize the cost-effectiveness of future mapping and ensure timely delivery of scientific information, seabed mappers worldwide may increasingly need to look to existing bathymetry data as a basis for thematic maps. This study examines the potential of compiled single-beam bathymetry data for sediment and biotope mapping. We simulate a mapping scenario where full coverage multibeam data are not available, but where existing bathymetry datasets are supplemented by limited multibeam data to provide the basis for thematic map interpretation and modelling. Encouraging results of sediment interpretation from the compiled bathymetry dataset suggest that production of sediment grain size distribution maps is feasible at a 1:250 000 scale or coarser, depending on the quality of available data. Biotope modelling made use of full-coverage predictor variables based on (i) multibeam data, and (ii) compiled single-beam data supplemented by limited multibeam data. Using the same response variable (biotope point observations obtained from video data), the performance of the respective models could be assessed. Biotope distribution maps based on the two datasets are visually similar, and performance statistics also indicate there is little difference between the models, providing a comparable level of information for regional management purposes. However, whilst our results suggest that using compiled bathymetry data with limited multibeam is viable as a basis for regional sediment and biotope mapping, it is not a substitute. Backscatter data and the better feature resolution provided by multibeam data remain of great value for these and other purposes.


Sign in / Sign up

Export Citation Format

Share Document