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International Journal on Algae
SJR: 0.216 SNIP: 0.322 CiteScore™: 0.4

ISSN Печать: 1521-9429
ISSN Онлайн: 1940-4328

Выпуски:
Том 22, 2020 Том 21, 2019 Том 20, 2018 Том 19, 2017 Том 18, 2016 Том 17, 2015 Том 16, 2014 Том 15, 2013 Том 14, 2012 Том 13, 2011 Том 12, 2010 Том 11, 2009 Том 10, 2008 Том 9, 2007 Том 8, 2006 Том 7, 2005 Том 6, 2004 Том 5, 2003 Том 4, 2002 Том 3, 2001 Том 2, 2000 Том 1, 1999

International Journal on Algae

DOI: 10.1615/InterJAlgae.v20.i2.20
pages 121-134

Assessment of the Reactions of Algal Communities to Influence of Climatic Factors in the North-Western Black Sea Ecosystem

G. G. Minicheva
Institute of Marine Biology, NAS Ukraine 37, Pushkinskaya St., 65011 Odessa, Ukraine
V. N. Bolshakov
Institute of Marine Biology, NAS of Ukraine, 7 Pushkinskaya St., Odessa 65011, Ukraine
E. S. Kalashnik
Institute of Marine Biology, NAS of Ukraine, 7 Pushkinskaya St., Odessa 65011, Ukraine
A. B. Zotov
Institute of Marine Biology, NAS of Ukraine, 37 Pushkinskaya St., Odessa 65011, Ukraine
A. V. Marinets
Institute of Marine Biology, NAS of Ukraine, 7 Pushkinskaya St., Odessa 65011, Ukraine

Краткое описание

The paper gives an overview of methodological problems (i.e., methods and indicators) in assessing the reactions of algae communities to climatic factors. We discuss the resistance of algal communities to the fluctuations and anomalous impact of climatic factors (solar energy flow, water temperature, precipitation, and river runoff) with reference to various life forms of Black Sea algae. To assess the reaction of algal communities impacted by climatic factors, a number of methodological approaches are proposed. It is necessary to carry out a comparison of the variability of both climatic factors and plant communities at appropriate levels of organization in natural systems (local, regional, and global). The changeability of climatic factors and algal communities must be measured using unified methods and indicators (variability, anomalies, etc.), and within the same time intervals (monthly, seasonally, and annually). Authors propose to use the ratio of oscillation coefficients (VR, %) for the structural-functional parameters of algal communities, and climatic factor indices: (VR)algae communities/(VR)climatic factors, as a measure of "stability" in different life forms of algae. For a sound conclusion about the significant impact of climatic factors on plant communities, we proposed to use the criterion of a significant (more than 30%) deviation of structural-functional parameters of algae communities from several years on a regional level. Analysis of the original results of both long-term observations (1997-2016) and the model period (2008-2009) made it possible to assess the stability of macrophytobenthos, phytoplankton, and microepiphyton to fluctuations in climatic factors, as well as their anomalous manifestations. High-natural stability of algal communities of the northwestern part of the Black Sea (NWBS) ecosystems to variability of climatic factors, as well as the synchronism of anomalous reactions of algae with anomalous climatic conditions is noted. It includes intra- and inter-annual synchronicity of the oscillation coefficient (VR, %) of climatic factors (water temperature, solar energy flow) and morphofunctional parameters of algae (phytobenthos, phytoplankton, and epiphyton). Cases of violation to such synchronism may indicate the effect of a group of third factors not related to climatic conditions, for example, changes in nutrient concentrations, biotope disturbance, etc. For the period of 1978-2016, synchronieity of the dynamics between climatic anomalies and structural-functional parameters of algal communities of the NWBS was recorded. Annual anomalies of climatic factors, exceeding 20% of the regional norm, cause evident restructuring of algal communities. Particularly strong anomalous reactions of plant communities (35-60% from the regional norm) were recorded in 2002-2003 under the long-term anomaly of water temperature and in 2010 under combination of high anomalies of two factors: the Danube runoff (45%) and water temperature (22%).


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