Korytarz ekologiczny doliny Odry pdf
Korytarz ekologiczny doliny Odry pdf Korytarz ekologiczny doliny Odry pdf
Summary • 336 km-long tract of the Middle Oder from Brzeg Dolny to the mouth of the Warta River; the Oder in this part is classified as a class II waterway, • 124 km-long reach of the Lower Oder, between the mouth of the Warta River and the town of Szczecin; regulated in the last century by means of groins, with significantly better exploitation conditions than the Middle Oder; this part belongs to class III and IV waterways. There are 23 dams along the whole length of the river, the last of them being „Brzeg Dolny”. Construction of the next one – „Malczyce” is planned at 300 km. The flood control system of the Oder is not restricted to flood control levees, built along the riverbed. It also includes polders, used as terrains scheduled for inundation, by high waters. The 10 most important polders have a total area of 6.4 thousand hectares, while their retention capacity is 75 million cubic metres. Currently the Wroc³aw Design Bureau „Navicentrum” is completing The studies of adaptation of the Oder River to the European system of waterways. The study examines the possibilities of joining the (so called) III Regional Class – east of the Elbe as well as the option of being included in the Vb International European Class. The class III option assumes, inter alia, the construction of the Malczyce dam (km 300.) and construction of new locks in places where old, single locks exist. The class Vb option requires the construction of many dams up to Hohensaaten (km 667.). According to this alternative, the channelized part of the river would be extended by 367 kilometres (so far the channelized part ois 187 kilometres long). At present, an intermediary option is being considered. Flora and vegetation of the Oder and its valley The ecological corridor formed by the Oder and its valley is an important route for plant migration, mainly used by mountainous species which spread along the Oder and can extend this way far into the lowlands. Along the valley of the Oder they expand their range in the Northern and North-Western directions. The Oder constitutes the eastern limit of the range of a group of atlantic species, though some of them can also be found further to the east. These species expand their ranges along the Oder, most often in the south-eastern direction. Some of them reach as far as the Carpathian and Sudeten Foreland. Toruñ-Eberswald preglacial stream valley, of which part constitutes the Freienwalde Basin, is a route of migration of xerothermic species from Turingen towards the north-east. A number of mediterranean species have arrived via this route, including: Quercus pubescens and Lithospermum purpureo-caeruleum. The ecological corridor of the Oder valley is also used for expansion by plants of foreign origin, which found their place in Poland in contemporary times (e.g. Impatiens glandulifera, Rubus americanus, Impatiens capensis). The habitat diversity of the Oder valley produces large diversity within its plant communities. Their clear zonation is caused by a gradient of environmental factors, first of all the 207
Korytarz ekologiczny doliny Odry soil- moisture factor. Water and wetland communities are found in the water and its direct vicinity, while in the estuary area – halophilous communities occur. A more distant locations are taken up by rushes and alder carrs. In places where water is not present on the surface through the whole year but only at inundations, there are riverside carrs and their substitutional communities – riverside meadows. On the highest terraces, outside the zone of direct flooding, there are dry oak hornbeam stands, which have often been changed into arable fields by Man. The edges of the valley are covered by communities not directly associated with the river – beech forests, mixed forests, grass communities and xerothermic scrubs. In total, 94 plant communities were reported from the Oder valley, belonging to almost all known classes of plant communities in Poland. However, the real vegetation of the Oder valley is very different from the potential vegetation. Most of the area is highly reshaped by Man and the primeval system of plant formations has been changed. Halophilous communities are found exclusively in the Oder estuary. They are best developed in Œwina Gate, and some are also present along the coast of Szczecin Bay. Due to the low salinity of the Baltic near the Polish coast, those communities are usually poor when compared with Western Europe, but their state of preservation is much better in the Oder estuary than in the remaining part of the Polish coast. Water and wetland communities (in total 42 communities, belonging to 4 different classes) as well as marshy meadows and lowland bogs (14 communities) are present in large numbers. The most interesting among them is Caricetum buxbaumii – calcyphilous plant association. Its occurrence in Poland is limited to the surroundings of Szczecin and £êczna- -W³odawa Lakeland. The richest and best developed xerothermic communities are found on the Lower Oder, between Kostrzyñ and Szczecin. In total 9 xerothermic and thermophilous grasslands have been found here, of which the most interesting are sub-xerothermic grassland communities with feather grass – Potentillo-Stipetum. Since 15 forest communities have been found in the Oder valley and on its wings, of which a thermophilous oak forest with Quercus pubescens and Lithospermum purpureo- -caeruleum (Lithospermo-Quercetum subboreale) develops in Poland exclusively in the valley of the Lower Oder, on the steep slopes of the proglacial stream valley, near Bielinek. Ichthyofaunistic analysis of the Oder and its tributaries The uppermost stretch of the river is the region of barbel (Barbus barbus). However, down to Opole, where the river changes its nature into the region of bream (Abramis brama), the leading species, Barbus barbus, as well as typical accompanying species Chondrostoma nasus and Thymallus thymallus are absent in the river, eliminated by an overtly high concentration of pollutants. From Opole to the Szczecin Bay, the Oder is physiographically a region of bream, with all typical fish species. An important role in the distribution of fish in the Oder is played by its pollution gradient, which changes along length of the river. The poorest ichthyofauna is observed in the region of barbel, where species of the highest environmental requirement should occur. This situation is, in fact, caused by high pollution. In the lower stretch of the Oder (the region of 208
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- Page 246 and 247: Bibliografia CELIÑSKI F. 1967. Not
- Page 248 and 249: Bibliografia CZWA£GA T., WOLSKI D.
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- Page 252 and 253: Bibliografia JANKOWSKI W. 1993a. Oc
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<strong>Korytarz</strong> <strong>ekologiczny</strong> <strong>doliny</strong> <strong>Odry</strong><br />
soil- moisture factor. Water and wetland communities are found in the water and its direct<br />
vicinity, while in the estuary area – halophilous communities occur. A more distant locations<br />
are taken up by rushes and alder carrs. In places where water is not present on the surface<br />
through the whole year but only at inundations, there are riverside carrs and their<br />
substitutional communities – riverside meadows. On the highest terraces, outside the zone<br />
of direct flooding, there are dry oak hornbeam stands, which have often been changed into<br />
arable fields by Man. The edges of the valley are covered by communities not directly associated<br />
with the river – beech forests, mixed forests, grass communities and xerothermic<br />
scrubs. In total, 94 plant communities were reported from the Oder valley, belonging to<br />
almost all known classes of plant communities in Poland. However, the real vegetation of<br />
the Oder valley is very different from the potential vegetation. Most of the area is highly<br />
reshaped by Man and the primeval system of plant formations has been changed.<br />
Halophilous communities are found exclusively in the Oder estuary. They are best developed<br />
in Œwina Gate, and some are also present along the coast of Szczecin Bay. Due to the<br />
low salinity of the Baltic near the Polish coast, those communities are usually poor when<br />
compared with Western Europe, but their state of preservation is much better in the Oder<br />
estuary than in the remaining part of the Polish coast.<br />
Water and wetland communities (in total 42 communities, belonging to 4 different<br />
classes) as well as marshy meadows and lowland bogs (14 communities) are present in large<br />
numbers. The most interesting among them is Caricetum buxbaumii – calcyphilous plant<br />
association. Its occurrence in Poland is limited to the surroundings of Szczecin and £êczna-<br />
-W³odawa Lakeland.<br />
The richest and best developed xerothermic communities are found on the Lower Oder,<br />
between Kostrzyñ and Szczecin. In total 9 xerothermic and thermophilous grasslands have<br />
been found here, of which the most interesting are sub-xerothermic grassland communities<br />
with feather grass – Potentillo-Stipetum.<br />
Since 15 forest communities have been found in the Oder valley and on its wings, of<br />
which a thermophilous oak forest with Quercus pubescens and Lithospermum purpureo-<br />
-caeruleum (Lithospermo-Quercetum subboreale) develops in Poland exclusively in the<br />
valley of the Lower Oder, on the steep slopes of the proglacial stream valley, near Bielinek.<br />
Ichthyofaunistic analysis of the Oder and its tributaries<br />
The uppermost stretch of the river is the region of barbel (Barbus barbus). However, down<br />
to Opole, where the river changes its nature into the region of bream (Abramis brama), the<br />
leading species, Barbus barbus, as well as typical accompanying species Chondrostoma<br />
nasus and Thymallus thymallus are absent in the river, eliminated by an overtly high concentration<br />
of pollutants. From Opole to the Szczecin Bay, the Oder is physiographically a region<br />
of bream, with all typical fish species.<br />
An important role in the distribution of fish in the Oder is played by its pollution gradient,<br />
which changes along length of the river. The poorest ichthyofauna is observed in the<br />
region of barbel, where species of the highest environmental requirement should occur. This<br />
situation is, in fact, caused by high pollution. In the lower stretch of the Oder (the region of<br />
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