Temat: southern Baltic - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: The comparison of the forecasted and measured currents in the deep part of the Southern Baltic Sea in 1999
Autorzy:: Krzymiński, W.
Powiązania:: https://bibliotekanauki.pl/articles/972854.pdf
Data publikacji:: 2001
Wydawca:: Instytut Morski w Gdańsku
Tematy:: Southern Baltic Sea
forecasts
HIROMB
Opis:: This paper presents results of the investigation carried out in frame of research project of Institute of Meteorology and Water Management Maritime Branch in Gdynia (IWM-MB) in the y ear 2000. The goal of the project was to determine the conformity of the sea current forecasts for the layer 8 - I 2 meters of the open sea part of the Southern Baltic Sea, as produced by the hydrodynamic model of the Baltic Sea- HIROMB [5}, with the measurements. Contrary to the results of previous experiments as in the case of the POLRODEX ones [7, 8, 9}, during present study it was expected to detect behaviour of the model far from the influence of the boundary like coastline as well as bottom friction in the shallow water areas. The analysed data were collected during five routine cruises of r/v Baltica organized by IWMMBsince February until September I999 [10], when cruise track started/rom the Gdansk Deep, next along the northern border of the Polish EEZ, ending in the Bomholm Deep area usually. On the basis of the current vectors recorded by means of the ship mounted ADCP as the 250 m average values in the layer 7.5 to 12.5 meters, mean values related to the model grid have been calculated and statistically assessed. These mean vectors have been used for compan·son of forecasted values. Consequently, the sets of values of the differences between measured and predicted currents were statistically evaluated both regarding the direction and the module of the currents as well as the current vector components (Vx, Vy) separately.
Źródło:: Biuletyn Instytutu Morskiego w Gdańsku; 2001, 28, 2; 55-64
1230-7424
2450-5536
Pojawia się w:: Biuletyn Instytutu Morskiego w Gdańsku
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: The comparison of the forecasted and measured currents in the deep part of the Southern Baltic Sea in 1999
Autorzy:: Krzymiński, W.
Powiązania:: https://bibliotekanauki.pl/articles/1920609.pdf
Data publikacji:: 2001
Wydawca:: Instytut Morski w Gdańsku
Tematy:: Southern Baltic Sea
forecasts
HIROMB
Opis:: This paper presents results of the investigation carried out in frame of research project of Institute of Meteorology and Water Management Maritime Branch in Gdynia (IWM-MB) in the y ear 2000. The goal of the project was to determine the conformity of the sea current forecasts for the layer 8 - I 2 meters of the open sea part of the Southern Baltic Sea, as produced by the hydrodynamic model of the Baltic Sea- HIROMB [5}, with the measurements. Contrary to the results of previous experiments as in the case of the POLRODEX ones [7, 8, 9}, during present study it was expected to detect behaviour of the model far from the influence of the boundary like coastline as well as bottom friction in the shallow water areas. The analysed data were collected during five routine cruises of r/v Baltica organized by IWMMBsince February until September I999 [10], when cruise track started/rom the Gdansk Deep, next along the northern border of the Polish EEZ, ending in the Bomholm Deep area usually. On the basis of the current vectors recorded by means of the ship mounted ADCP as the 250 m average values in the layer 7.5 to 12.5 meters, mean values related to the model grid have been calculated and statistically assessed. These mean vectors have been used for compan·son of forecasted values. Consequently, the sets of values of the differences between measured and predicted currents were statistically evaluated both regarding the direction and the module of the currents as well as the current vector components (Vx, Vy) separately.
Źródło:: Biuletyn Instytutu Morskiego w Gdańsku; 2001, 28, 2; 55-64
1230-7424
2450-5536
Pojawia się w:: Biuletyn Instytutu Morskiego w Gdańsku
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: The development of unconsolidated sedimentary coastal cliffs (Pobrzeże Kaszubskie, Northern Poland)
Autorzy:: Uścinowicz, G.
Jurys, L.
Szarafin, T.
Powiązania:: https://bibliotekanauki.pl/articles/2060378.pdf
Data publikacji:: 2017
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: cliff coast
landslides
soft sediments
Southern Baltic
Opis:: In the course of fieldwork based on geological and landslide mapping and spatial analyses of map information at least 2 types of landslides were identified. Type I: simple landslides developed in homogeneous and undisturbed rocks, for instance – loams, clays and sands. This type of landslide includes many examples developed mainly on the stretch (segment of the studied area) approximately between 132.25 and 133.50 km and 128.50 and 129.50 km of the Polish coastline. Type II: complex landslides in which the movement and displacement of rock masses occurs under complex geological and hydrogeological conditions. The complex factors are determined by phenomena such as glaciotectonics, discontinuities of rock layers and thrust zones; the slip surface occurs at considerable depths, and sometimes several slip surfaces can be distinguished. These landslide types are located in the vicinity of Jastrzębia Góra and Rozewie, near km 134 and 131.5. Prediction of the formation of this landslide types is difficult. Even if long-term observations are available, the mass movement, variable over time, is difficult to interpret. It is clear that the changes are continuous, but occur with varying intensity. Proper recognition of the types of mass movement is crucial to establishing the appropriate methods to prevent their development.
Źródło:: Geological Quarterly; 2017, 61, 2; 491--501
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Diatomological and geochemical evidence of littorina transgression in Pomeranian Bay, Southern Baltic Sea
Autorzy:: Kostecki, Robert
Janczak-Kostecka, Beata
Powiązania:: https://bibliotekanauki.pl/articles/2026722.pdf
Data publikacji:: 2010
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: diatoms
geochemistry
Littorina transgression
Pomeranian Bay
southern Baltic Sea
Opis:: This ar ti cle pres ents re sults of the anal y sis of 3 sed i ment cores taken from the bot tom of Pom er a nian Bay, south ern Bal tic Sea. These re sults are part of a larger pro ject that aims to de ter mine the char ac ter is tics and rate of the At lan tic ma rine ingression in the Pom er a nian Bay area. The main geo chem i cal el e ments and di a tom as sem blages from the cores were iden ti fied, re veal ing lac us trine sed i ments de pos ited dur ing the time of Ancylus Lake and ma rine sed i ments de pos ited dur ing the Littorina trans gres sion. Dis tinct changes in the geo chem i cal com po si tion and di a tom as sem - blages sug gest that the Littorina trans gres sion had a very large im pact on the en vi ron ment of Pom er a nian Bay.
Źródło:: Studia Quaternaria; 2010, 27; 27-33
1641-5558
2300-0384
Pojawia się w:: Studia Quaternaria
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 5.

Tytuł:: Phases of aeolian accumulation on the Vistula Spit (Southern Baltic Sea) in the light of TL dating and analysis of a digital elevation model
Autorzy:: Fedorowicz, S.
Wysiecka, G.
Zieliński, P.
Hołub, B.
Powiązania:: https://bibliotekanauki.pl/articles/2059003.pdf
Data publikacji:: 2012
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Southern Baltic
Vistula Spit
Holocene
dune ridges
TL dating
DEM
Opis:: The genesis of the Vistula Spit (Southern Baltic Sea) in the Postlitorina period is regarded as occurring by gradual addition of successive dune ridges along the entire length of the form. Based on the degree of soil profile development and radiocarbon dating of organic sediments three main stages of aeolian processes are usually recognized. GIS analysis of a digital elevation model (DEM) and thermoluminescence dating of dune sand supports the model of progressive development of dune ridges, and has identified four periods of intense aeolian activity. These were established 5860–5400, 1930–1610, 1200–900 years ago from the present, and from 500 years ago.
Źródło:: Geological Quarterly; 2012, 56, 2; 345-352
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 6.

Tytuł:: The first report on the establishment and spread of the alien clam Rangia cuneata (Mactridae) in the Polish part of the Vistula Lagoon (Southern Baltic)
Autorzy:: Warzocha, J.
Szymanek, L.
Witalis, B.
Wodzinowski, T.
Powiązania:: https://bibliotekanauki.pl/articles/47524.pdf
Data publikacji:: 2016
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: Rangia cuneata
Mactridae
clam
alien species
Vistula Lagoon
Southern Baltic
Źródło:: Oceanologia; 2016, 58, 1
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 7.

Tytuł:: Stages of the formation of the Łeba barrier-lagoon system on the basis of the geological cross-section near Rąbka (Southern Baltic Coast, Poland)
Autorzy:: Rotnicki, Karol
Alexandrowicz, Stefan W.
Pazdur, Anna
Goslar, Tomasz
Borówka, Ryszard K.
Powiązania:: https://bibliotekanauki.pl/articles/2026416.pdf
Data publikacji:: 2009
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: sand barriers
lagoons
Holocene barrier- lagoon system
Polska
southern Baltic coast
Opis:: The ar ti cle pres ents the re sults of a de tailed study of the geo log i cal struc ture of the £eba Bar rier in the R¹bka crosssec tion (South ern Bal tic, Po land). The bar rier sep a rates Lake £ebsko from the Bal tic. Five sed i men tary com plexes were dis tin guished there (M2–M6). The spa tial vari abil ity of the grain-size dis tri bu tion was ex am ined and suc ces sion stages of the mol lusc fauna oc cur ring in the in di vid ual sed i men tary com plexes were dis tin guished. Ra dio car bon dating was used to es tab lish the age of the most im por tant events dur ing the pro cess of for ma tion of the bar rier, which took place in the course of sev eral rel a tive sea-level changes. The first sed i men tary com plex (M2) at R¹bka is connected with the sec ond ingression (i2) of the Bal tic Sea (ca. 6,700–6,000 14C years BP), sea-level sta bi li za tion (6,000–5,500 14C years BP), and at last sea-level low er ing (5,500–5,000 14C years BP) in the re gion of the Gardno-£eba Coastal Plain. The sed i men tary com plex M3 de vel oped in a la goonal en vi ron ment when the bar rier was sit u ated north of its pres ent po si tion (5,000–3,000 14C BP). The next low er ing of the sea-level made the la goon shal lower and caused the emer gence of small but al ready subaerial stretches of bar rier land with a fresh wa ter fauna in the north (4,880±40 14C BP). With the next ingression stage (i3), which took place be tween 4,500 and 3,000 BP, the bar rier shifted to its pres ent-day po si tion and the la goon changed into a fresh wa ter lake. From 3,000 to 1,700 14C BP fos sil soil and peats de vel oped on the bar rier sur face as a re sult of an other sea-level low er ing. The last ingression stages (i4 and i5), youn - ger than 1,700 BP, built up the bar rier, prac ti cally in its to day’s lo ca tion (sed i men tary com plexes M4 and M5). The youn gest sed i men tary com plex (M-6) is rep re sented by pres ent-day beach sands.
Źródło:: Studia Quaternaria; 2009, 26; 3-24
1641-5558
2300-0384
Pojawia się w:: Studia Quaternaria
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 8.

Tytuł:: Chronology of the last ice sheet decay on the southern Baltic area based on dating of glaciofluvial and ice-dammed lake deposits
Autorzy:: Uścinowicz, Szymon
Adamiec, Grzegorz
Bluszcz, Andrzej
Jegliński, Wojciech
Jurys, Leszek
Miotk-Szpiganowicz, Grażyna
Moska, Piotr
Pączek, Urszula
Piotrowska, Natalia
Poręba, Grzegorz
Przezdziecki, Piotr
Uścinowicz, Grzegorz
Powiązania:: https://bibliotekanauki.pl/articles/2058614.pdf
Data publikacji:: 2019
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: southern Baltic area
deglaciation
Late Glacial
Słupsk Bank Phase
OSL dating
Opis:: The paper presents the results of the first OSL dating of glaciofluvial and ice-marginal lake sediments which occur between end moraines of the Słupsk Bank and the Polish coast. The sand and gravel of glaciofluvial deltas on the Słupsk Bank were deposited most likely during a period from 14.3 ±1.2 to 16.6 ±1.4 ka ago. The deposition of silty-sandy sediments of the ice-marginal lake is dated at 14.51 ±0.81 and 14.6 ±1.4 ka years. Likewise, dates ranging from 13.74 ±0.84 to 16.70 ±1.1 ka obtained from low sandy ridges, related to the southern range of the ice-marginal lake in the Gardno-Łeba Lowland, indicate the most likely timing of their deposition. It can be concluded that a short stop of the ice sheet on the Słupsk Bank took place approximately 15.2 ka ago, which could be correlated with the position of the ice sheet front in central Skåne and in northern Lithuania at that time. Older and younger results were also obtained, except the dates mentioned above. The older ages show little sunlight exposure of sediments during their deposition. The younger dates indicate a marine origin of the sediments and show that some parts of glaciofluvial sediments were redeposited and exposed to sunlight at a later stage, most probably when dead-ice blocks were melting.
Źródło:: Geological Quarterly; 2019, 63, 1; 193--208
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 9.

Tytuł:: Morpholithodynamical changes of the beach and the nearshore zone under the impact of submerged breakwaters — a case study (Orłowo Cliff, the Southern Baltic)
Autorzy:: Kubowicz-Grajewska, A.
Powiązania:: https://bibliotekanauki.pl/articles/49145.pdf
Data publikacji:: 2015
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: breakwater
beach
morpholithodynamics
Orlowo Cliff
Southern Baltic
Polish coast
nearshore zone
Źródło:: Oceanologia; 2015, 57, 2
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 10.

Tytuł:: Geochemistry of surface sediments of a coastal Lake Sarbsko (northern Poland)
Autorzy:: Woszczyk, Michał
Cieśliński, Roman
Spychalski, Waldemar
Powiązania:: https://bibliotekanauki.pl/articles/2026076.pdf
Data publikacji:: 2009
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: coastal lake
lake sediment geochemistry
Gardno-Łeba Coastal Plain
southern Baltic
Polska
Opis:: The main goal of the pre sented re search was to in ves ti gate spa tial dis tri bu tion of sur face sed i ments and to rec og nize re la tion ships be tween chem i cal com po si tion of wa ter and sed i ments in a coastal Lake Sarbsko (north ern Po land). The Lake Sarbsko is a fresh wa ter ba sin. The wa ter col umn is well ox y gen ated and wa ters ex hibit only mi nor spa tial vari - abil ity of chem i cal com po si tion in di cat ing rapid and good mix ing. Sur face sed i ments of Lake Sarbsko are strongly di - ver si fied with re spect to chem i cal com po si tion. The sed i ments of Lake Sarbsko are char ac ter ized by el e vated con tent of terrigenous sil ica in di cat ing en hanced in put of clastic ma te rial from the wa ter shed and/or in creased dy nam ics of the lake wa ters. More over, SiO2ter is strongly neg a - tively cor re lated with SiO2biog, or ganic mat ter and el e ment con tents, which ar gues for di lut ing ef fect of the for mer to - wards authigenic com po nents of sed i ments. Ba si cally, terrigenous sil ica (quartz) con tent is high est in the lake shores and de clines to wards the lake cen ter. Biogenic sil ica, or ganic mat ter and most of el e ments dis play re versed ten dency. CaCO3 was en coun tered in three iso lated ar eas, where it co-oc curs with FeS. It is an tic i pated that pre cip i ta tion of cal - cite in Lake Sarbsko re sulted from postdepositional pro cesses. Spa tial dis tri bu tion of Fe, Mn, Ca, Mg, Na and K in Lake Sarbsko is also gov erned by their geo chem i cal af fin i ties to or ganic mat ter (Fe), Fe/Mn ox ides (Fe, Mn), sulphides (Fe), clay min er als (Na, K, Mg, Mn) and car bon ates (Ca, Mn).
Źródło:: Studia Quaternaria; 2009, 26; 41-53
1641-5558
2300-0384
Pojawia się w:: Studia Quaternaria
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 11.

Tytuł:: Alien species of fish parasites in the coastal lakes and lagoons of the Southern Baltic
Autorzy:: Morozinska-Gogol, J.
Powiązania:: https://bibliotekanauki.pl/articles/47573.pdf
Data publikacji:: 2009
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: parasite
alien species
aquaculture
Baltic Sea
Southern Baltic
fish parasite
coastal lake
lagoon
infected fish
Opis:: Alien species are now found all over the world. New fish parasites have been unintentionally introduced with infected alien fish imported for aquaculture or have sometimes spread with their intermediate invertebrate hosts transported in the ballast waters of ships. Four alien fish parasites have been recorded in Polish coastal lakes and lagoons, all parasitising eels. Three were introduced with the final host – the Japanese eel – introduced for aquaculture (Anguillicola crassus, Pseudodactylogyrus anguillae and Pseudodactylogyrus bini) and one (Paratenuisentis ambiguus) with its sole intermediate host (Gammarus tigrinus).
Źródło:: Oceanologia; 2009, 51, 1; 105-115
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 12.

Tytuł:: Late glacial and holocene environmental changes in the Southern Baltic Sea area based on malacofauna investigations
Autorzy:: Krzymińska, J.
Koszka-Maroń, D.
Pikies, R.
Przezdziecki, P.
Powiązania:: https://bibliotekanauki.pl/articles/1182436.pdf
Data publikacji:: 2018
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: późny glaciał
holocen
malakofauna
południowy Bałtyk
Late Glacial
Holocene
Southern Baltic Sea
malacofauna
Opis:: Zmiany klimatyczne, a za tym daleko idące zmiany środowiska w późnym glacjale i holocenie na obszarze południowego Bałtyku mogą być wyjaśniane także przez badania fauny mięczaków. Na obszarze południowego Bałtyku w okresie późnego glacjału występowały gatunki słodkowodne wskazujące na klimat zimny, takie jak: Armiger crista f. cristatus, Gyraulus laevis, Lymnaea peregra, Pisidium casertanum, Pisidium casertanum f. ponderosa, Pisidium milium, Pisidium nitidum, Pisidium obtusale f. lapponicum, Valvata cristata, Pisidium conventus. Akumulacja jeziorna w słodkowodnych zbiornikach strefy przybrzeżnej kontynuowała się w okresie wczesnego holocenu. W tym czasie oprócz gatunków słodkowodnych, zimnolubnych pojawiły się gatunki mięczaków i małżoraczków słodkowodnych, o wyższych wymogach termicznych (Bithynia tentaculata, Physa fontinalis, Pisidium amnicum). Świadczy to o ociepleniu się klimatu w okresie preborealnym. Zrastanie przybrzeżnych zbiorników rozpoczęło się w okresie borealnym i trwało również w okresie atlantyckim. W tym czasie miały miejsce wlewy wód morskich do zbiorników. Wskaźnikiem tego jest liczne występowanie morskich gatunków takich jak: Hydrobia ulvae, Hydrobia ventrosa, Cerastoderma glaucum, Mytilus edulis, Macoma balthica. W osadach piaszczystych w okresie subborealnym i subatlantyckim zdecydowanie przeważała fauna morska.
Źródło:: Polish Geological Institute Special Papers; 2018, 30; 1--70
1507-9791
Pojawia się w:: Polish Geological Institute Special Papers
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 13.

Tytuł:: Sedimentation rates and dating of bottom sediments in the Southern Baltic Sea region
Autorzy:: Suplińska, M. M.
Pietrzak-Flis, Z.
Powiązania:: https://bibliotekanauki.pl/articles/146241.pdf
Data publikacji:: 2008
Wydawca:: Instytut Chemii i Techniki Jądrowej
Tematy:: sedimentation rate
210Pb
137Cs
239,240Pu
Southern Baltic
bottom sediment
Opis:: Sedimentation rates and dating of bottom sediments were estimated in two sampling stations of the Gulf of Gdańsk and in four stations in the open sea area. Estimations were based on vertical distributions of 210Pb, 137Cs and 239,240Pu activity concentrations in sediment core samples taken in 1998–2007. Two dating models based on changes of activity concentrations of 210Pbunsup were used: 1) CF:CS (Constant Flux Constant Sedimentation rate-model) and 2) CRS (Constant Rate of Supply-model). 137Cs and 239,240Pu were applied as time markers. 137Cs originates mostly from the Chernobyl accident in 1986, whereas 239,240Pu comes from the global fallout in 1963. The validation of the 210Pb methods was performed by activity peak of 137Cs and 239,240Pu. Sediment accumulation rate (g·cm–2·y–1) was constant along sediment core. Annually accumulated layer, (mm·y–1) decreased with sediment depth in all the locations. In the Gulf of Gdańsk sedimentation rate in the upper layer was about 3.6 mm·y–1, and it decreased in the deeper layers to about 1.1 mm·y–1. Sedimentation rates in the open sea area were lower than in the gulf region and the lowest was observed in the Bornholm Deep, being about 0.95 mm·y–1 in the upper layer and 0.35 mm·y–1 in the deeper layer. The growth of a 5 cm thick layer took 27–37 years in the Gulf of Gdańsk, and 61–105 years in the open sea area. It is suggested that the mean values obtained from the models would give a most reliable estimation of the sedimentation rates.
Źródło:: Nukleonika; 2008, 53, suppl. 2; 105-111
0029-5922
1508-5791
Pojawia się w:: Nukleonika
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 14.

Tytuł:: Composition of phytoplankton in the Puck Bay and the open Baltic Sea
Struktura fitoplanktonu w Zatoce Puckiej oraz na otwartym Morzu Bałtyckim
Autorzy:: Świacka, Klaudia
Michnowska, Alicja
Maculewicz, Jakub
Przednowek, Izabela
Ogrodowczyk, Iga
Kozic, Sebastian
Powiązania:: https://bibliotekanauki.pl/articles/2179169.pdf
Data publikacji:: 2017-12-31
Wydawca:: Uniwersytet Pedagogiczny im. Komisji Edukacji Narodowej w Krakowie
Tematy:: phytoplankton
Puck Bay
Southern Baltic Sea
blooms
fitoplankton
Zatoka Pucka
Morze Bałtyckie
zakwity
Opis:: The Puck Bay is an area characterised by specific hydrodynamic conditions that determine the distribution and composition of phytoplankton. The aim of this study was to investigate the differences in the phytoplankton composition and the content of photosynthetic pigments between the Puck Bay and open Baltic Sea. The material was collected from four stands which were localised in the inner and outer part of Hel Peninsula. In this study, it has been demonstrated that the composition of individual species of phytoplankton differed between stands in the inner and outer part of the Puck Bay. This investigation has also shown that the number of phytoplankton taxa was similar in three stands and it was much lower on the last stand (Stand 4). The differences in the concentration of photosynthetic pigments between all stands have also been observed.
Zatoka Pucka jest obszarem charakteryzującym się specyficznymi warunkami hydrodynamicznymi, które determinują rozmieszczenie i skład fitoplanktonu. Głównym celem niniejszej pracy było zbadanie różnic w składzie taksonomicznym fitoplanktonu oraz zawartości barwników fotosyntetycznych pomiędzy Zatoką Pucką, a otwartymi wodami Morza Bałtyckiego. Materiał zebrano z czterech miejsc zlokalizowanych po wewnętrznej, jak i zewnętrznej, części Półwyspu Helskiego. W pracy wykazano, że istnieją różnice w składzie taksonomicznym fitoplanktonu między wewnętrzną i zewnętrzną częścią Zatoki Puckiej. Niniejsza praca pokazała, że liczba taksonów fitoplanktonu na stanowiskach 1, 2 i 3 była zbliżona i znacznie wyższa niż na stanowisku 4. Zaobserwowano również różnicę w stężeniach barwników fotosyntetycznych między badanymi stanowiskami.
Źródło:: Annales Universitatis Paedagogicae Cracoviensis Studia Naturae; 2017, 2; 27-35
2543-8832
2545-0999
Pojawia się w:: Annales Universitatis Paedagogicae Cracoviensis Studia Naturae
Dostawca treści:: Biblioteka Nauki