scholarly journals Restoration of Salinity in the Sivash Bay to Natural Levels after the Closure of the North Crimean Canal

Author(s):  
E. S. Eremina ◽  

The paper analyzes the salinity dynamics in the Sivash Bay after the closure of the NorthCrimean based on the data from field research carried out by MHI RAS in 2014–2020. Recent field data are compared with the literature data obtained in the period before the commissioning of the North Crimean Canal. Salinity in water samples taken during 18 expeditions to the Eastern and Southern Sivash at over 100 stations was determined using the refractometric method. It was shown that after the closure of the North Crimean Canal in 2014, there was a steep increase in salinity in the Eastern and Southern Sivash. It was determined that in the area of the Sivash Bay, the haline field changes non-uniformly. The data analysis showed that salinity increases from north to south (from the Eastern to Southern Sivash), moreover salinity values in the Southern Sivash can be several times higher than those in the Eastern Sivash. In spring 2014, salinity in the Eastern Sivash varied from 27 to 33 ‰, and in 2020, 6 years after the closure of the Canal, salinity increased significantly at all stations reaching 60–70 ‰. These values are comparable to those obtained before the start of the Canal in the 1950s. The highest salinity values were observed in the South Sivash: in 2013, it was 54 ‰ and in summer 2020, for the first time since the North Crimean Canal became operational, it reached 110 ‰, which almost corresponds to the salinity level observed in 1969.

1906 ◽  
Vol 3 (7) ◽  
pp. 301-310 ◽  
Author(s):  
F. R. Cowper Reed

A Small collection of fossils from the Bokkeveld Beds has recently been sent to me for identification by the South African Museum, and some of them have been generously presented to the Sedgwick Museum. Amongst this material it is interesting to find some genera not previously recorded from the Cape and some new species. The majority of the specimens are in the condition of internal casts, and hence present especial difficulties in their determination, so that in a few cases some uncertainty must remain as to the generic position of the fossils. However, I am able to record for the first time from these beds the occurrence of the well-known lamellibranchiate genus Buchiola, and of a shell which may be identified with Nyussa arguta, Hall, of the North American Devonian. The genus Buchiola occurs in argillaceous nodules from the Zwartberg Pass crowded with individuals of the species which I have named B. subpalmata and with a few examples of an undetermined species. No other associated fossils can be recognised in these nodules, but I am informed that an abundant fauna is found in the beds at this locality.


Author(s):  
Jonathan Kaplan ◽  
Federico Paredes Umaña

Chapter 4 abstracts and summarizes the very copious field data from the three lengthy field seasons at Chocolá, including the specific evidence obtained about the very extensive water control system that was discovered. Intensive grid excavations were undertaken in five operations: Mound 15, the northernmost part of the elite north sector, Mounds 6 and 7, in the southern part of the north sector, Mound 2, in the central administrative sector, and Mound 5, in the south sector. Accordingly, our three field seasons provide the specific evidence and artifacts we have been able to use to understand the clearly hierarchical structure of the ancient society and city. Of particular importance for a better understanding of the material underpinnings of Chocolá is our research at Mound 5, in the south, where we believe cacao arboriculture was developed for long-distance trade in the Preclassic period.


Author(s):  
Avraham Faust

Chapter 4 (‘Under the Empire: Settlement and Demography in the Southwestern Margins of the Assyrian Empire in the Seventh Century BCE’) describes the settlement and demography in the period of Assyrian control. Comparing the detailed information available from the region with that provided in Chapter 2 allows us to estimate what were the consequences of the imperial takeover. The evidence shows that the provinces in the north were mostly devastated, whereas the client kingdoms prospered and, moreover, for the first time in history the south flourished more than the north. The dramatic decline in the north is also exemplified by the large number of place names that were forgotten following the Assyrian conquests. The chapter ends with an appendix on the demographic significance of deportations.


Zootaxa ◽  
2009 ◽  
Vol 2009 (1) ◽  
pp. 1-26 ◽  
Author(s):  
JOACHIM SCHMIDT ◽  
MATTHIAS HARTMANN

The genus Pristosia Motschulsky, 1865 was so far only known to be highly diverse in the North-Western Himalaya and present in the Eastern Himalaya. Only a single female specimen has been documented in the literature from the Nepal Himalaya and was described as P. dahud Morvan, 1994. During a study of comprehensive carabid beetle material collected throughout Nepal, which has been deposited at several museums and private collections, a large number of Pristosia specimens from six species have been identified. The only fully winged species P. crenata (Putzeys, 1873), which is widely distributed in South East Asia, was found near Dailekh and is herewith reported for the Nepalese fauna for the first time. The Eastern Himalayan species P. amaroides (Putzeys, 1877) is reported for the first time in Nepal as well and occurs in Eastern Nepal at several localities east of the Arun river. At least four species occur in the Western and Far Western Nepal Himalaya, of which three are described as new to science: P. glabella sp. n. and P. nepalensis sp. n. from the Api Himal, and P. similata sp. n. from the Saipal Himal. An presumably additional new species is known from the north-western slope of the Dhaulagiri Himal, but is represented by a single immature female specimen only, which does not allow for a sufficient species diagnosis. The male external and genital characters of P. dahud Morvan, 1994 are now described for the first time. This species is considered to be polytypic and the geographic subspecies P. dahud polita ssp. n. is described from the south slope of the Kanjiroba Himal. The species P. atrema (Andrewes, 1926) and P. championi (Andrewes, 1934), which occur in the Kumaon Himalaya close to the Nepalese border, are redescribed based on the examination of the type material. Diagnostic features, especially for the male genitalia of all taxa mentioned above, are figured and a key to the species from Nepal is presented. Instead of a phylogenetic analysis, which is needed for Pristosia but not achievable at present, preliminary species groups for species dealt with are proposed: The Eastern Himalayan P. amaroides species group (monotypic), the P. atrema species group with six species from the Kumaon and Western Nepal Himalaya, the P. championi species group with two species from the Kumaon and Western Nepal Himalaya, and the South East Asian P. crenata species group (monotypic). Based on the distributional and ecological data presented in this study, species of the genus Pristosia with reduced hind wings seem to be absent from the entire Central Nepal Himalaya, and the only Eastern Nepalese species, P. amaroides, prefers largely different habitat conditions compared to the species from Western Nepal. Based on biogeographical hypotheses of other Himalayan carabid beetle genera presented in previous studies by the senior author, the observed species groups of Pristosia are considered to be further examples for Tertiary Tibetan faunal components of the Himalaya. Following a diversification of the genus within the Tertiary of Southern Tibet, speciation occurred and these species groups originated from founder populations that moved into the Nepal Himalaya. The colonization of the geologically younger High Himalaya has taken place independently for each of the terminal groups via different dispersal routes and during different periods of mountain uplift.


2021 ◽  
Vol 1 (8) ◽  
Author(s):  
Yuni Iswahyu Ratih ◽  
Daeng Achmad Suaidi ◽  
Samsul Hidayat

Garbage is matter which is serious enought to society especially in the main city. Increasing number of society will affect to increasing garbage either as resulted. Volume of garbage which al ways increase without measuring last process of garbage will appear many problems for example, leachate seepage. Leachate is a liquid waste resulted of biology decomposition. Leachate soaks to bottom groundwater will affect decreasing level of field water and allergy on the skin. The aim of this research is to know leahate accumulation and direct seepage arround landfill Sekoto. The method will be conducted by field research by geoelectric configuration diple-dipole. Firstly, the writter survey the location to know the condition of research. Then collected data with 5 line arround landfill Sekoto use resistivitymeter. The data will be process using software Res2dinv and Voxler. Software Res2dinv to show the leachate seepage base on resistivity rock value. Software Voxler is used to show direct seepage as 3 dimension. The research finding shows that lye had been permeated in the south of garbage-can with the leachate seepage reaching 6.79 meters. While, in the north of garbage-can, there was no leachate seepage found. In the west road of Garbage Dump and near to leachate waste pipe, it had been found the leachate seepage reaching 11.8 meters. In summary, the direction of leachate seepage in Garbage Dump is congruence with river flow and the distribution of leachate horizontally.


2021 ◽  
Author(s):  
◽  
Sanjay Paul Samuel

<p>The Paleocene interval within the Canterbury Basin has been relatively understudied with respect to the Neogene and Cretaceous intervals. Within the Paleocene interval is the Tartan Formation and the Charteris Bay Sandstone, which are potential source and reservoir rocks respectively. These two formations have not been previously mapped in the offshore Canterbury Basin and their limits have not been defined. This study utilises a database of nearly 12,000km of 2D seismic data together with data from four open–file wells and sidewall core samples from three wells and newly availiable biostratigraphic information to better constrain the chronostratigraphical interpretation of seismic data. Seismic mapping together with corroboration from well correlation and core lithofacies analysis revealed new insights into the development of the offshore Canterbury Basin through the Paleocene. These include the delineation of the lateral extents and thicknesses of the Tartan Formation and Charteris Bay Sandstone and location of the palaeo shelf–slope break and also the development of a new well correlation panel that incorporates the Tartan Formation for the first time.  This study presents four new paleogeographic maps for the offshore Canterbury Basin that significantly improves our understanding of the development of the basin during the Paleocene. These maps show that during the Earliest Paleocene, the mudstones of the Katiki Formation were being deposited in the south of the study area, with the siltier sediments of the Conway Formation being deposited in the north. The coarser grained Charteris Bay Sandstone was deposited from Early to possibly Middle Paleocene in the northeast. The mudstones of the Moeraki Formation were being deposited in the south at this time. From Middle to Late Paleocene, the mudstones of the Moeraki Formation were deposited in the south and these mudstones onlapped against the Charteris Bay Sandstone which remained as a high in the north. The Tartan Formation was deposited during the Late Paleocene in the central and southern areas of the offshore Canterbury Basin, during a relative fall in sea–level. Deposition had ceased in the north of the study area or erosion possibly removed Late Paleocene sediments from there. During the Latest Paleocene, the mudstones of the Moeraki Formation were deposited over the Tartan Formation in the central and southern parts of the offshore Canterbury Basin with the northern area undergoing erosion, sediment bypass or both.</p>


2021 ◽  
Author(s):  
◽  
Sanjay Paul Samuel

<p>The Paleocene interval within the Canterbury Basin has been relatively understudied with respect to the Neogene and Cretaceous intervals. Within the Paleocene interval is the Tartan Formation and the Charteris Bay Sandstone, which are potential source and reservoir rocks respectively. These two formations have not been previously mapped in the offshore Canterbury Basin and their limits have not been defined. This study utilises a database of nearly 12,000km of 2D seismic data together with data from four open–file wells and sidewall core samples from three wells and newly availiable biostratigraphic information to better constrain the chronostratigraphical interpretation of seismic data. Seismic mapping together with corroboration from well correlation and core lithofacies analysis revealed new insights into the development of the offshore Canterbury Basin through the Paleocene. These include the delineation of the lateral extents and thicknesses of the Tartan Formation and Charteris Bay Sandstone and location of the palaeo shelf–slope break and also the development of a new well correlation panel that incorporates the Tartan Formation for the first time.  This study presents four new paleogeographic maps for the offshore Canterbury Basin that significantly improves our understanding of the development of the basin during the Paleocene. These maps show that during the Earliest Paleocene, the mudstones of the Katiki Formation were being deposited in the south of the study area, with the siltier sediments of the Conway Formation being deposited in the north. The coarser grained Charteris Bay Sandstone was deposited from Early to possibly Middle Paleocene in the northeast. The mudstones of the Moeraki Formation were being deposited in the south at this time. From Middle to Late Paleocene, the mudstones of the Moeraki Formation were deposited in the south and these mudstones onlapped against the Charteris Bay Sandstone which remained as a high in the north. The Tartan Formation was deposited during the Late Paleocene in the central and southern areas of the offshore Canterbury Basin, during a relative fall in sea–level. Deposition had ceased in the north of the study area or erosion possibly removed Late Paleocene sediments from there. During the Latest Paleocene, the mudstones of the Moeraki Formation were deposited over the Tartan Formation in the central and southern parts of the offshore Canterbury Basin with the northern area undergoing erosion, sediment bypass or both.</p>


2019 ◽  
Vol 62 (2) ◽  
pp. 101-125
Author(s):  
Margret Mathes-Schmidt ◽  
Ioannis Papanikolaou ◽  
Klaus Reicherter ◽  
Aggelos Pallikarakis

Event deposits of high-energy waves in the Eastern Thermaikos Gulf and Kassandra Peninsula (Northern Greece) are investigated, and evidence for the 479 BC "Herodotus tsunami" is described for the first time. One of the first historical descriptions of tsunami waves and its effects on Persian troops near Potidaea in 479 BC was made by Herodotus. Sedimentary traces of tsunamis were investigated in cores from different areas from Angelochori in the north to the ruins of ancient Mende in the south (Kassandra peninsula). Evidence for one, locally two high-energy events, on the coasts of Chalkidiki is found. These layers are preserved in flat and lagoonal areas at least from 100 m of the present-day beach. Within ancient Mende, a high-energy layer was encountered. Besides a vast amount of ceramics, the layer also contains articulated bivalve shells. These were dated to a time span between 712 and 521 cal yrs BC by radiocarbon including a reservoir effect of 400 ± 40 years. Resulting ages resemble the time the tsunami mentioned by Herodotus in 479 BC. Deposits of a further event affecting the Thermaikos Gulf were dated between the 7 th to 10 th cent. AD.


2019 ◽  
Vol 157 (10) ◽  
pp. 1658-1692 ◽  
Author(s):  
H. Nøhr-Hansen ◽  
S. Piasecki ◽  
P. Alsen

AbstractA palynostratigraphic zonation is for the first time established for the entire Cretaceous succession in NE Greenland from Traill Ø in the south to Store Koldewey in the north (72–76.5° N). The zonation is based on samples from three cores and more than 100 outcrop sections. The zonation is calibrated to an updated ammonite zonation from the area and to palynozonations from the northern North Sea, Norwegian Sea and Barents Sea areas. The palynozonation is primarily based on dinoflagellate cyst and accessory pollen. The Cretaceous succession is divided into 15 palynozones: seven Lower Cretaceous zones and eight Upper Cretaceous zones. The two lowermost zones are new. The following five (Lower Cretaceous) zones have already been described. Two of the Upper Cretaceous zones are new. The zones have been subdivided into 20 subzones, 11 of which have been described previously and one of which has been revised/redefined. Nine subzones (Upper Cretaceous) are new. More than 100 stratigraphical events representing more than 70 stratigraphic levels have been recognized and presented in an event-stratigraphic scheme.


Author(s):  
Valentina Bobykina ◽  
Valentina Bobykina ◽  
Boris Chubarenko ◽  
Boris Chubarenko ◽  
Konstantin Karmanov ◽  
...  

For the first time, the quantitative characteristics of the Vistula Spit shore dynamics based on the ground-based monitoring data for 2002-2015 were presented. On the sea shore, 3 sections can be distinguished by the direction of coastal processes, i.e. the stable section to the north of the Strait of Baltiysk, the eroded 4-km section to the south of the Strait of Baltiysk, with maximum erosion rate up to 2 m/year; in the remaining area of the Spit (21 km) to the Polish border there is an alternation of stable, eroded and accumulative areas. Since 2011, a steady erosion (in the stable segments of the third section) and general weakening of the erosion rate (in the second section) have been recorded. 50% of the length of the lagoon shore was the subject to annual active erosion (0.2 - 1.4 m/year). The beaches of the sea and lagoon shores of the Vistula Spit were mainly composed of medium sands. The alongshore variability in particle size distribution on the sea and lagoon shores (according to the 2015 survey data) actually fail to correlate with long-term dynamic processes, with the exception of the steadily eroded 4-kilometer area on the sea coast to the south of the Strait of Baltiysk. Variations in the composition of sediment along the shore on the shoreline are most likely associated with the results of the latest wave processing (or storm processing and eolian transport in the case of an average beach sample).


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