scholarly journals Expanding the geographical distribution of Rhynchocypris czekanowskii (Dybowski, 1869) (Cypriniformes, Cyprinidae) in the basin of the Yenisei River, Eastern Siberia, Russia

Check List ◽  
2019 ◽  
Vol 15 (3) ◽  
pp. 369-374
Author(s):  
Ivan Vladimirovich Zuev ◽  
Sergei Mikhailovich Chuprov ◽  
Anastasiya Vyacheslavovna Zueva
Keyword(s):  
Geographical Distribution ◽  
River Basin ◽  
River Basins ◽  
Middle Part ◽  
Water Bodies ◽  
The Arctic ◽  
Eastern Siberia ◽  
Yenisei River ◽  
Small Water ◽  
The Yenisei River

The currently known geographical distribution of Chekanovskii’s Minnow, Rhynchocypris czekanowskii (Dybowski, 1869), is limited only by the lower reaches of the arctic river basins in which this species lives. We report R. czekanowskii from the small water bodies of middle part of Yenisei river basin, expanding its distribution to the south of the river basin to 55°51ʹ41ʺ N latitude, more than 100 km south from previously known occurrences of this species.

scholarly journals Assessment of sediment and organic carbon exports into the Arctic ocean: The case of the Yenisei River basin

2019 ◽  
Vol 158 ◽  
pp. 118-135 ◽  
Author(s):  
C. Fabre ◽  
S. Sauvage ◽  
N. Tananaev ◽  
G. Espitalier Noël ◽  
R. Teisserenc ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Arctic Ocean ◽  
River Basin ◽  
The Arctic ◽  
Yenisei River ◽  
The Arctic Ocean ◽  
The Yenisei River

Identification of sibling species in the genus Eucyclops from water-bodies of Ukraine and Russia using crossbreeding studies

2014 ◽  
Vol 25 (1-2) ◽  
pp. 61-68 ◽  
Author(s):  
V. I. Monchenko ◽  
L. P. Gaponova ◽  
V. R. Alekseev
Keyword(s):  
Cryptic Species ◽  
River Basin ◽  
Black Sea ◽  
Species Complex ◽  
River Basins ◽  
Water Bodies ◽  
Similar Species ◽  
Basin Water ◽  
Different Populations ◽  
Baltic Sea Basin

Crossbreeding experiments were used to estimate cryptic species in water bodies of Ukraine and Russia because the most useful criterion in species independence is reproductive isolation. The problem of cryptic species in the genus Eucyclops was examined using interpopulation crosses of populations collected from Baltic Sea basin (pond of Strelka river basin) and Black Sea basin (water-reservoires of Dnieper, Dniester and Danube rivers basins). The results of reciprocal crosses in Eucyclops serrulatus-group are shown that E. serrulatus from different populations but from water bodies belonging to the same river basin crossed each others successfully. The interpopulation crosses of E. serrulatus populations collected from different river basins (Dnipro, Danube and Dniester river basins) were sterile. In this group of experiments we assigned evidence of sterility to four categories: 1) incomplete copulation or absence of copulation; 2) nonviable eggs; 3) absence of egg membranes or egg sacs 4) empty egg membranes. These crossbreeding studies suggest the presence of cryptic species in the E. serrulatus inhabiting ecologically different populations in many parts of its range. The same crossbreeding experiments were carries out between Eucyclops serrulatus and morphological similar species – Eucyclops macruroides from Baltic and Black Sea basins. The reciprocal crossings between these two species were sterile. Thus taxonomic heterogeneity among species of genus Eucyclops lower in E. macruroides than in E. serrulatus. The interpopulation crosses of E. macruroides populations collected from distant part of range were fertile. These crossbreeding studies suggest that E. macruroides species complex was evaluated as more stable than E. serrulatus species complex.

Human biogeography and climate change in Siberia and Arctic North America in the fourth and fifth millennia BP

1990 ◽  
Vol 330 (1615) ◽  
pp. 665-670 ◽  
Keyword(s):  
North America ◽  
The Arctic ◽  
Polar Regions ◽  
Before Present ◽  
Yenisei River ◽  
Northeastern Asia ◽  
Time Period ◽  
The Yenisei River ◽  
Historical Relation ◽  
Small Tool

This paper explores the relation between the geographic shifts in prehistoric hunting populations and changes in climate between 4500 and 3000 before present (BP) within the polar regions from the Yenisei River in Siberia to Greenland. We have chosen this time period because major human geographic changes occurred over much of northeastern Asia and northern North America, and because these changes appear to be linked, at least in part, to a palaeoclimatic fluctuations. The cultures under consideration have been termed the Early and Middle Neolithic (Syalakh and Bel’kachi) in Siberia and the Arctic Small Tool Tradition (with such local variants as Denbigh, Independence I, Pre-Dorset, and Sarqaq) in North America. Despite these terminological differences, these groups shared such a close similarity in their technology and adaptive patterns that they must have once shared a direct historical relation.

scholarly journals Widening the geographical distribution of Pimelodus mysteriosus Azpelicueta 1998 (Siluriformes: Pimelodidae) to the upper Paraná River, with diagnosis for syntopic congeners

2015 ◽  
Vol 15 (3) ◽  
Author(s):  
Gabriel de Carvalho Deprá ◽  
Renata Rúbia Ota ◽  
Fagner de Souza ◽  
Weferson Júnio da Graça ◽  
Carla Simone Pavanelli
Keyword(s):  
Geographical Distribution ◽  
River Basin ◽  
River Basins ◽  
Paraná River ◽  
River Floodplain ◽  
Parana River ◽  
Paraguay River ◽  
Upper Paraná River Floodplain ◽  
Upper Paraná River ◽  
Upper Paraná River Basin

Pimelodus mysteriosus Azpelicueta 1998, previously known only from the lower Paraná and Paraguay River basins, has been also recorded in the upper Paraná River floodplain. The only congeners occurring in syntopy with P. mysteriosus in the upper Paraná River basin are P. maculatus and P. ornatus. New diagnostic characters between P. mysteriosus and P. maculatus are provided.

scholarly journals Reconstruction of Rain Flood at the Adagum River on the Basis of Mathematical Models for Discharge Formation

2013 ◽  
pp. 87-104
Author(s):  
Keyword(s):  
Water Quality ◽  
Surface Water ◽  
River Basin ◽  
River Basins ◽  
Water Bodies ◽  
Practical Application ◽  
Protective Measures ◽  
Surface Water Bodies ◽  
Discharge Formation ◽  
Water Quality Objectives

The authors developed and presented a method of setting objectives in terms of surface water bodies’ water quality; it was elaborated and specified in accordance with the results of its application at a number of river basins. An algorithm of water/protective measures prioritizing in a river basin on the basis of water quality objectives was proposed. Practical application of the proposed approaches was illustrated by examples from the Scheme of Water Bodies; Integrated Use and Protection for the Ob River basin.

scholarly journals Changes of Hydrological Components in Arctic Rivers Based on Multi-Source Data during 2003–2016

Water ◽  
2021 ◽  
Vol 13 (24) ◽  
pp. 3494
Author(s):  
Hao Wu ◽  
Min Xu ◽  
Mengyan Zhu
Keyword(s):  
Global Warming ◽  
River Basin ◽  
Hydrological Cycle ◽  
River Basins ◽  
Surface Flow ◽  
Base Flow ◽  
The Arctic ◽  
Current Case ◽  
Annual Cycles ◽  
Earth’S System

The hydrological cycle of the Arctic river basin holds an important position in the Earth’s system, which has been significantly disturbed by global warming. This study analyzed recent changes in the hydrological components of two representative Arctic river basins in Siberia and North America, the Lena River Basin (LRB) and Mackenzie River Basin (MRB), respectively. The trends were diagnosed in hydrological components through a comparative analysis and estimations based on remote sensing and observational datasets during 2003–2016. The results showed that the annual precipitation decreased at rates of 1.9 mm/10a and 18.8 mm/10a in the MRB and LRB, respectively. In contrast, evapotranspiration (ET) showed increasing trends, with rates of 9.5 mm/10a and 6.3 mm/10a in the MRB and LRB, respectively. Terrestrial water storage (TWS) was obviously decreased, with rates of 30.3 mm/a and 18.9 mm/a in the MRB and LRB, respectively, which indicated that more freshwater was released. Contradictive trends of the runoffs were found in the two basins, which were increased in the LRB and decreased in the MRB, due to the contributions of the surface water and base flow. In addition, the mean annual cycles of precipitation, ET, TWS, runoff depth, surface flow and base flow behaved differently in both magnitudes and distributions in the LRB and MRB, the trends of which will likely continue with the pronounced warming climate. The current case studies can help to understand the recent changes in the Arctic hydro-climatology and the consequence of global warming in Arctic river basins.

scholarly journals Unprecedented acceleration of winter discharge of Upper Yenisei River inferred from tree rings

2021 ◽  
Author(s):  
Irina Panyushkina ◽  
David M Meko ◽  
Alexander Shiklomanov ◽  
Richard D Thaxton ◽  
Vladimyr Myglan ◽  
...  
Keyword(s):  
Arctic Ocean ◽  
River Discharge ◽  
Ring Width ◽  
Ocean Modeling ◽  
The Arctic ◽  
Yenisei River ◽  
South Siberia ◽  
The Arctic Ocean ◽  
The Yenisei River ◽  
The Impact

Abstract The Yenisei River is the largest contributor of freshwater and energy fluxes among all rivers draining to the Arctic Ocean. Modeling long-term variability of Eurasian runoff to the Arctic Ocean is complicated by the considerable variability of river discharge in time and space, and the monitoring constraints imposed by a sparse gauged-flow network and paucity of satellite data. We quantify tree growth response to river discharge at the upper reaches of the Yenisei River in Tuva, South Siberia. Two regression models built from eight tree-ring width chronologies of Larix sibirica are applied to reconstruct winter (Nov–Apr) discharge for the period 1784-1997 (214 years), and annual (Oct–Sept) discharge for the period 1701–2000 (300 years). The Nov–Apr model explains 52% of the discharge variance whereas Oct–Sept explains 26% for the calibration intervals 1927–1997 and 1927-2000, respectively. This new hydrological archive doubles the length of the instrumental discharge record at the Kyzyl gauge and resets the temporal background of discharge variability back to 1784. The reconstruction finds a remarkable 80% upsurge in winter flow over the last 25 years, which is unprecedented in the last 214 years. In contrast, annual discharge fluctuated normally for this system, with only a 7% increase over the last 25 years. Water balance modeling with CRU data manifests a significant discrepancy between decadal variability of the gauged flow and climate data after 1960. We discuss the impact on the baseflow rate change of both the accelerating permafrost warming in the discontinuous zone of South Siberia and widespread forest fires. The winter discharge accounts for only one-third of the annual flow, yet the persistent 25-year upsurge is alarming. This trend is likely caused by Arctic Amplification, which can be further magnified by increased winter flow delivering significantly more freshwater to the Kara Sea during the cold season.

scholarly journals Hydrological Variability and Changes in the Arctic Circumpolar Tundra and Its Largest Pan-Arctic river Basins from 2002 to 2016

2017 ◽  
Author(s):  
Kazuyoshi Suzuki ◽  
Koji Matsuo ◽  
Dai Yamazaki ◽  
Kazuhito Ichii ◽  
Yoshihiro Iijima ◽  
...  
Keyword(s):  
River Basin ◽  
River Basins ◽  
The Arctic ◽  
Lena River ◽  
North American Continent ◽  
The North ◽  
Hydrological Variability ◽  
Basin Scale ◽  
Northern Regions ◽  
Terrestrial Water

The Arctic freshwater budget is critical for understanding the climate in the northern regions. However, the hydrology of the Arctic circumpolar tundra region (ACTR) and the largest pan-Arctic rivers are still not well understood. In the present paper, we analyze the spatiotemporal variations in terrestrial water storage (TWS) of the ACTR, including three of its largest pan-Arctic river basins (Lena, Mackenzie, Yukon), using monthly Gravity Recovery and Climate Experiment (GRACE) data from 2002 to 2016. Together with global land reanalysis, river runoff, and inundation extent area (IEA) data, we identify declining TWS trends throughout the ACTR that we attribute largely to increasing evapotranspiration driven by increasing summer air temperatures. In terms of regional changes, large and significant negative trends in TWS are observed mainly over the North American continent. At basin scale, we show that, in the Lena River basin, the autumnal TWS signal persists until the winter of the following year, while in the Mackenzie River basin, the TWS levels in the autumn and winter has no significant impact on the following year. As global warming is expected to be particularly significant in the northern regions, our results are important for understanding future TWS trends, with possible further decline.

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