Zmiany składu gatunkowego i wskaźników struktury zbiorowisk roślinnych w latach 2001‑2018 na wybranych powierzchniach stałych w Kampinoskim Parku Narodowym = Changes of species composition and structural indices among plant communities in 2001‑2018 on selected permanent plots in Kampinos National Park

2021 ◽  
Vol 93 (3) ◽  
pp. 413-443
Author(s):  
Jerzy Solon ◽  
Anna Otręba ◽  
Anna Andrzejewska ◽  
Piotr T. Zaniewski

On the basis of 2001, 2007, 2012 and 2018 phytosociological records obtained from 52 permanent plots distributed across Poland’s Kampinos National Park, it proved possible to determine main directions of change in the ecological character of undergrowth. Reference to similarity of species composition on the plots between 2001 and 2018 allowed for the identification of Groups: A (occurring in boggy alder forest habitats, and comprising communities at different successional stages), B (coniferous and mixed-coniferous forests), C (oak-hornbeam forests and similar communities) and D (vegetation representing different dynamic stages of the succession from non-forest to forest communities). Irrespective of each plot’s unique history, the above Groups of plots could be characterised in line with specific sets of features subject to directional change during the period under analysis. Where Group A communities were concerned, a rise in the level of ground water and a decline in the content of organic carbon in soil were experienced, with the result that fen sedge species (Scheuchzerio-Caricetea) came to play a reduced role, even as there was a steadily-increasing role for species associated with communities flooded at least periodically (hence Potamogetonetea and Bidentetea). This was accompanied by a decrease in the number of shrub species and an increase in the number of bryophyte species. There were also increases in the proportions of geophytes and species associated with habitats more abundant in nitrogen. Group B communities were likewise subject to rising water tables, albeit changes not reflected directly in differing vegetation characteristics. The carbon: nitrogen ratio in soils here increased, as did numbers of species characteristic of undergrowth, as well as the bryophyte layer. Nevertheless, where undergrowth species were concerned, the role of those typical for open sandy grasslands (Koelerio-Corynephoretea) is seen to be declining, with this inter alia denoting increased shares of species either tolerant of shade or avoiding full illumination. There has also been a decline affecting hemicryptophytes, even as species associated with more nitrogen-rich habitats have come to account for greater shares. Where Group C communities encountered higher water levels, certain patches present in wetter habitats saw increases in the role played by species characteristic for class Bidentetea. The sorption capacities of soils here decreased, while values for the C: N ratio rose. Tree and shrub species came to be fewer in number as numbers of undergrowth species rose. There were also increases in the roles of species characterising moist verges (Galio-Urticenea), as well as geophytes. Group D communities likewise encountered rising groundwater levels, but did not seem to experience directional change otherwise, within their phytocoenoses. The sorption capacity of their soils nevertheless decreased. Overall, it was possible to note increases over the period in question when it came to numbers of species present in the tree, undergrowth and bryophyte layers. However, while the role of species characteristic for class Nardo-Callunetea increased, that of Trifolio-Geranietea species declined. And, while correlations between vegetation and soil characteristics proved to be different for each of the four groups of communities, there was no precluding model parameters differing significantly from one year of measurement to another.

2014 ◽  
Vol 14 (1-2) ◽  
pp. 163-191 ◽  
Author(s):  
Maria Lisiewska

The investigations on the role of macromycetes in various forest communities of the Świętokrzyski National ark were performed in the years 1964-1968. Fruit bodies growing on the soil, in the litter and on wood were studied on 13 permanent plots. Attention was paid to effects of atmospheric conditions on the fruiting of fungi and to the seasonal aspects of macromycetes.


2021 ◽  
Author(s):  
Rebecca Weissinger ◽  
Dana Witwicki

The goal of Northern Colorado Plateau Network (NCPN) riparian monitoring is to determine long-term trends in hydrologic, geomorphic, and vegetative properties of wadeable streams in the context of changes in other ecological drivers, stressors, and processes. This information is intended to provide early warning of resource degradation and determine natural variability of wadeable streams. This report summarizes NCPN monitoring of Courthouse Wash in Arches National Park (NP) from 2010 to 2019. The focus of this report is to (1) present geomorphology and vegetation data from five reaches monitored in Courthouse Wash from 2010 to 2015, and (2) examine patterns in water availability at one monitoring reach from November 2010 to December 2019. Vegetation sampling and geomorphology surveys were suspended in 2016 due to budget cuts; this report presents baseline data for future comparisons. The NCPN has five monitoring reaches located between the inflow of Sevenmile Canyon, a major tributary, and the terminus of Courthouse Wash, at the Colorado River. Two reaches (2, 5) are located in Upper Courthouse Wash, and three (1, 4, 7) in Lower Courthouse Wash. Hydrologic monitoring wells are installed only at Reach 1. During our monitoring period, which included drought years in 2012 and 2018 and a wetter-than-average period from fall 2013 to 2014, groundwater levels showed steep declines corresponding to the start of the growing season each year. Hot, dry summers and falls in 2012, 2018, and 2019 showed the deepest troughs in groundwater levels. Active monsoon years helped elevate summer and fall groundwater levels in 2013 and 2014. Continued monitoring will help us better understand the relationship of climate and water availability at this reach. A geomorphic survey was completed once for reaches 2, 4, and 7, and twice for reaches 5 and 1. Powerful floods during our monitoring period resulted in aggradation of the channel in reaches 5 and 1, which were first surveyed in March 2013. Flooding in September 2013 resulted in an average of 0.24 meters of deposition found in the channel thalweg at Reach 1 in March 2014. Storm events in May 2014 caused additional aggradation. In March 2015, an average of 0.41 meters of deposition was recorded in the channel thalweg at Reach 5, with 0.32 meters of deposition between the vegetation transect headpins compared to the 2013 data. The riparian vegetation recorded at our monitoring reaches is consistent with an open-canopy Fremont cottonwood woodland with a diverse understory. Canopy closure ranged from 29% to 52%. Measurements were sensitive enough to detect a 10% reduction in canopy closure at Reach 5 during a pest infestation in June 2013. Canopy closure subsequently rebounded at the reach by 2015. Total obligate and facultative wetland cover ranged from 7% to 26%. Fremont cottonwood seedlings, saplings, and overstory trees were present at all reaches, indicating good potential for future regeneration of the canopy structure. These data can serve as a baseline for comparison with future monitoring efforts. One area of management concern is that exotic-plant frequency and cover were relatively high in all monitoring reaches. Exotic cover ranged from 2% to 30%. High exotic cover was related to years with high cover of annual brome grasses. High cover of exotic grasses is associated with increased wildfire risk in southwestern riparian systems, which are not well-adapted to fire. Managers should be prepared for this increased risk following wet winters that promote annual brome grass cover. Beaver activity was noted throughout bedrock-constrained reaches in Courthouse Wash. Beaver activity can reduce adjacent woody riparian vegetation cover, but it also contributes to maintaining a higher water table and persistent surface water. Climate change is likely to be an increasingly significant stressor in Courthouse Wash, as hotter, drier conditions decrease water levels and increase drought stress...


2019 ◽  
Vol 23 ◽  
pp. 1-7 ◽  
Author(s):  
Ekaterina Kozlova ◽  
Anna Popkova ◽  
Svetlana Mazina ◽  
Vladimir Pešić

Fouling communities with the dominance of phototrophs such as cyanobacteria, algae, bryophytes, and ferns are formed in the illuminated zone of the caves. These communities includes also heterotrophic species—bacteria and micromycetes, often with the high abundance of the latter, indicating significant role of micromycetes for the developing of fouling communities.In this study we examined the micromycete species composition in the phototrophic communities of five caves, i.e., Golubinja Pećina, Veluštica Pećina, Njegoš Pećina, Vrbačka jama, Jama ER-1 located on the territory of Lovćen National Park in the southwestern Montenegro. Species identification was performed using standard approaches and cultivation methods. In total, 35 species of micromycetes were identified from the phototroph communities of the studied caves. Our study revealed that the species composition of micromycetes was unique for each of the investigated cave. The most frequent species was Rhizopus stolonifer, identified from Golubinja Pećina, Vrbačka jama, and Jama ER-1. Two species, i.e., Aspergillus terreus (found in Veluštica Pećina and Jama ER-1), and Cladosporium oxysporum (found in Golubinja Pećina and Veluštica Pećina) were found each in two caves, whereas all other species were reported from a single cave.


Author(s):  
David Genter ◽  
Lee Metzgar

Until recently, little attention has been directed to the bat fauna of GTNP. The role of bats in ecosystems is more significant than previously thought. Also, the public's awareness of bats is growing and as part of routine interpretive needs, the NPS must have factual information on all animals in the Park. A baseline survey was conducted to determine species composition, distribution, abundance, and habitat use of bats in Grand Teton National Park, Wyoming. The principal objectives are: 1. Obtain information on species occurrence and distribution within the Park; 2. Assess the population status for bat species present; 3. Identify rare species in the Park and identify management needs to ensure the viability of these species in GTNP; and 4. Evaluate potential conflicts with human activities.


2011 ◽  
Vol 72 (4) ◽  
pp. 339-356 ◽  
Author(s):  
Andrzej Jaworski ◽  
Dorota Jakubowska

Dynamika zmian budowy, struktury i składu gatunkowego drzewostanów o charakterze pierwotnym na wybranych powierzchniach w Pienińskim Parku Narodowym


2018 ◽  
Vol 7 (4) ◽  
pp. 191
Author(s):  
Sherwan Sh. Qurtas

Recharge estimation accurately is crucial to proper groundwater resource management, for the groundwater is dynamic and replenished natural resource. Usually recharge estimation depends on the; the water balance, water levels, and precipitation. This paper is studying the south-middle part of Erbil basin, with the majority of Quaternary sediments, the unconfined aquifer system is dominant, and the unsaturated zone is ranging from 15 to 50 meters, which groundwater levels response is moderate. The purpose of this study is quantification the natural recharge from precipitation. The water table fluctuation method is applied; using groundwater levels data of selected monitoring wells, neighboring meteorological station of the wells, and the specific yield of the aquifers. This method is widely used for its simplicity, scientific, realistic, and direct measurement. The accuracy depends on the how much the determination of specific yield is accurate, accuracy of the data, and the extrapolations of recession of groundwater levels curves of no rain periods. The normal annual precipitation there is 420 mm, the average recharge is 89 mm, and the average specific yield is around 0.03. The data of one water year of 2009 and 2010 has taken for some technical and accuracy reasons.


2012 ◽  
pp. 66-77 ◽  
Author(s):  
I. A. Lavrinenko ◽  
O. V. Lavrinenko ◽  
D. V. Dobrynin

The satellite images show that the area of marshes in the Kolokolkova bay was notstable during the period from 1973 up to 2011. Until 2010 it varied from 357 to 636 ha. After a severe storm happened on July 24–25, 2010 the total area of marshes was reduced up to 43–50 ha. The mean value of NDVI for studied marshes, reflecting the green biomass, varied from 0.13 to 0.32 before the storm in 2010, after the storm the NDVI decreased to 0.10, in 2011 — 0.03. A comparative analysis of species composition and structure of plant communities described in 2002 and 2011, allowed to evaluate the vegetation changes of marshes of the different topographic levels. They are fol­lowing: a total destruction of plant communities of the ass. Puccinellietum phryganodis and ass. Caricetum subspathaceae on low and middle marches; increasing role of halophytic species in plant communities of the ass. Caricetum glareosae vic. Calamagrostis deschampsioides subass. typicum on middle marches; some changes in species composition and structure of plant communities of the ass. Caricetum glareosae vic. Calamagrostis deschampsioides subass. festucetosum rubrae on high marches and ass. Parnassio palustris–Salicetum reptantis in transition zone between marches and tundra without changes of their syntaxonomy; a death of moss cover in plant communities of the ass. Caricetum mackenziei var. Warnstorfia exannulata on brackish coastal bogs. The possible reasons of dramatic vegetation dynamics are discussed. The dating of the storm makes it possible to observe the directions and rates of the succession of marches vegetation.


2019 ◽  
Author(s):  
G. Lynn Wingard ◽  
◽  
Miriam C. Jones ◽  
Sarah E. Bergstresser ◽  
Bethany L. Stackhouse ◽  
...  

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