Research on the phenology of certain herbaceous species in Macin Mountains National Park

Similar documents
THERMAL AND WATER RISK AGRO-METEOROLOGICAL PARAMETERS AND THEIR IMPACT ON WINTER WHEAT CROPS (Triticum aestivum L.) IN MUNTENIA REGION

THE MAXIMUM QUANTITIES OF RAIN-FALL IN 24 HOURS IN THE CRIŞUL REPEDE HYDROGRAPHIC AREA

POTENTIAL EVAPOTRANSPIRATION AND DRYNESS / DROUGHT PHENOMENA IN COVURLUI FIELD AND BRATEŞ FLOODPLAIN

Studies on adaptation capacity of Carpathian ecosystems/landscape to climate change

Ganbat.B, Agro meteorology Section

Global Biogeography. Natural Vegetation. Structure and Life-Forms of Plants. Terrestrial Ecosystems-The Biomes

Biomes and Climate Relationships

Climate change in Croatia: observations and modeling

DROUGHT MONITORING BULLETIN

Drought Monitoring in Mainland Portugal

STUDIES ON PHENOLOGICAL CHARACTERISTICS OF DIFFERENT FOREST TREES OF SOUTH GUJARAT, INDIA

Geographical location and climatic condition of the

MODELLING FROST RISK IN APPLE TREE, IRAN. Mohammad Rahimi

Climate Change Impact on Air Temperature, Daily Temperature Range, Growing Degree Days, and Spring and Fall Frost Dates In Nebraska

A COMPARATIVE STUDY OF OKLAHOMA'S PRECIPITATION REGIME FOR TWO EXTENDED TIME PERIODS BY USE OF EIGENVECTORS

DROUGHT IN MAINLAND PORTUGAL

Plant Water Stress Frequency and Periodicity in Western North Dakota

AN EXCESSIVELY FROSTY MONTH - JANUARY 1963

Dawood Public School Secondary Section Class VII

Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate

PHYSICAL PROPERTIES TAHOE.UCDAVIS.EDU 8

Research note UDC: 911.2:511.58(497.16) DOI:

PH YSIC A L PROPERT IE S TERC.UCDAVIS.EDU

soils E) the Coriolis effect causes the moisture to be carried sideways towards the earth's oceans, leaving behind dry land masses

Name of research institute or organization: Federal Office of Meteorology and Climatology MeteoSwiss

Constructing a typical meteorological year -TMY for Voinesti fruit trees region and the effects of global warming on the orchard ecosystem

Our climate system is based on the location of hot and cold air mass regions and the atmospheric circulation created by trade winds and westerlies.

Analysis of Rainfall and Other Weather Parameters under Climatic Variability of Parbhani ( )

Department of Dendrology, University of Forestry, 10 Kl. Ohridski blvd., Sofia 1756, Bulgaria, tel.: *441

A summary of the weather year based on data from the Zumwalt weather station

Global Patterns Gaston, K.J Nature 405. Benefit Diversity. Threats to Biodiversity

Vermont Soil Climate Analysis Network (SCAN) sites at Lye Brook and Mount Mansfield

SEASONAL AND DAILY TEMPERATURES

Attribution of Estonian phyto-, ornitho- and ichtyophenological trends with parameters of changing climate

Observed and near future projections of weather extremes in Romania

CHAPTER-11 CLIMATE AND RAINFALL

WHAT CAN MAPS TELL US ABOUT THE GEOGRAPHY OF ANCIENT GREECE? MAP TYPE 1: CLIMATE MAPS

The Relationship between Vegetation Changes and Cut-offs in the Lower Yellow River Based on Satellite and Ground Data

DIFFERENTIATION OF AVOCADO BLOSSOM BUDS IN FLORIDA

Drought in Southeast Colorado

Weather and Climate in Canada. October 2 nd, 2017

Why the Earth has seasons. Why the Earth has seasons 1/20/11

Workshop on Drought and Extreme Temperatures: Preparedness and Management for Sustainable Agriculture, Forestry and Fishery

World Geography Chapter 3

Meteorology. Circle the letter that corresponds to the correct answer

The Palfai Drought Index (PaDI) Expansion of applicability of Hungarian PAI for South East Europe (SEE) region Summary

Meteorology. Chapter 15 Worksheet 1

CLIMATE CHANGE IMPACTS ON ICE REGIME OF THE RIVERS IN MONGOLIA

Students will work in small groups to collect detailed data about a variety of living things in the study area.

SWIM and Horizon 2020 Support Mechanism

Banu C. 1, Banu T. 1, Moatăr Mihaela 1, Ştefan Carolina 1, Banu T. 1, Stanciu S. 2

Unit 2 Text Worksheet # 2

THE SIGNIFICANCE OF AIR TEMPERATURE OSCILLATIONS IN THE LAST DECADE IN SPLIT - CROATIA

Winter (December 1, 2015, to February 29, 2016)

DROUGHT ASSESSMENT USING SATELLITE DERIVED METEOROLOGICAL PARAMETERS AND NDVI IN POTOHAR REGION

16 Global Climate. Learning Goals. Summary. After studying this chapter, students should be able to:

Preliminary Runoff Outlook February 2018

Application and verification of the ECMWF products Report 2007

remain on the trees all year long) Example: Beaverlodge, Alberta, Canada

Climate Dataset: Aitik Closure Project. November 28 th & 29 th, 2018

Our Living Planet. Chapter 15

forest tropical jungle swamp marsh prairie savanna pampas Different Ecosystems (rainforest)

Summary and Conclusions

UNIT 1. WEATHER AND CLIMATE. PRIMARY 4/ Social Science Pedro Antonio López Hernández

Analysis of Historical Pattern of Rainfall in the Western Region of Bangladesh

About some anomalies in precipitation regime in Bulgaria

COLD AND HEAT WAVES IN THE BARLAD PLATEAU BETWEEN

Chapter 3 Section 3 World Climate Regions In-Depth Resources: Unit 1

Mozambique. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1

Environmental Factors to Consider during Planning of Management for Range Plants in the Dickinson, North Dakota, Region,

Weather Conditions during the 1992 Growing Season

Canada only has 7 of these biomes. Which biome do you think does not exist in Canada and why?

November 2018 Weather Summary West Central Research and Outreach Center Morris, MN

Plant responses to climate change in the Negev

Climate: long term average weather. Use climograph to display climate data. Climograph

Climate of Columbus. Aaron Wilson. Byrd Polar & Climate Research Center State Climate Office of Ohio.

Lecture Outlines PowerPoint. Chapter 20 Earth Science 11e Tarbuck/Lutgens

TUNDRA. Column 1 biome name Column 2 biome description Column 3 examples of plant adaptations

2011 National Seasonal Assessment Workshop for the Eastern, Southern, & Southwest Geographic Areas

WEATHER AND CLIMATE SCIENCE

Climate Outlook through 2100 South Florida Ecological Services Office Vero Beach, FL September 9, 2014

Colorado State University, Fort Collins, CO Weather Station Monthly Summary Report

Natural Disasters and Storms in Philadelphia. What is a storm? When cold, dry air meets warm, moist (wet) air, there is a storm.

South & South East Asian Region:

Changing Hydrology under a Changing Climate for a Coastal Plain Watershed

What is Climate? Understanding and predicting climatic changes are the basic goals of climatology.

The agroclimatic resource change in Mongolia

The Global Scope of Climate. The Global Scope of Climate. Keys to Climate. Chapter 8

THE RISKS ASSOCIATED TO THE HOARFROST PHENOMENON IN THE WEST PLAIN

TEXAS WILDLAND FIRE POTENTIAL WINTER/SPRING 2018/2019

JRC MARS Bulletin global outlook 2017 Crop monitoring European neighbourhood

Malawi. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1

Chapter 8. Biogeographic Processes. Upon completion of this chapter the student will be able to:

Climatology. Rainfall and Temperature Regimes. Myriam Traboulsi. The rainfall regime

Operational MRCC Tools Useful and Usable by the National Weather Service

2011 Year in Review TORNADOES

Effect of El Niño Southern Oscillation (ENSO) on the number of leaching rain events in Florida and implications on nutrient management

DYNAMICS OF OUTDOOR RADON AND THORON PROGENY CONCENTRATIONS IN SOME GEOGRAPHICAL AREAS OF ROMANIA *

Climate Classification

PRATICOLA PHYTOCOENOSES ON TULCEA HILLS

Transcription:

Volume 16(1), 278-284, 2012 JOURNAL of Horticulture, Forestry and Biotechnology www.journal-hfb.usab-tm.ro Research on the phenology of certain herbaceous species in Macin Mountains National Park Gherghişan Ecaterina 1 * 1 Brad Segal High School Tulcea *Corresponding author. Email: egherghisan@yahoo.com Abstract The studies performed in Pricopan Peak- Macin Mountains National Park, between 2005 and 2009, sought to emphasize the correlation between specific climatic elements of the area and the phenological phases of 50 herbaceous species within the park. Phenological observations were carried out continuously in key territories and areas covered by all types of pytocenosis. Climatic diagrams were created using the Gaussen-Walter system for climate representation. The data obtained was expressed quantitatively which is more conclusive than a descriptive expression. The results of this research show that multiannual variations of ecological factors influenced the phenological phases and the vegetation was able to adapt to changing ecological factors. The results of the study shows that the differences in phenological phases are evident, however not profound, and their occurrence is correlated to the higher or lower levels of arid climate within the studied periods of time. The research ensures the scientific basis necessary in creating maps of phenological aspects useful in planning ecological reconstruction of natural eco-systems, and of the exploitation of natural resources within the park area. These observations may also be used to restrict tourist s access in designated areas during certain periods of time, in the strict protected areas and to preserve local biodiversity (Petrescu, 2007). Key words biodiversity, climate diagram, Pricopan peak, biological forms, phenophases Macin Mountains flora is characterized by richness and diversity; in regard to the composition, its composition is similar to the flora of Turkey, the Crimea and in neighboring Moldova, Bulgaria and Serbia (1, 6). Currently, in the Macin Mountains, there are only descriptive research studies regarding flora and vegetation, as well as their distribution based on physical and geographical factors (1, 7, 15). An analytical study of environmental factors and their relationship to the vital processes of the plants has been carried out on the Babadag Plateau (3, 6). An overview of the relationship between vegetation and ecological factors of cause-effect is difficult to achieve (3). Such complex ecological research "in stationary" (11) on the distribution of phenophases, correlated with the character of local climatic factors, were made in Macin Mountains only in woody species (9). Thus the special character of these researches, which takes the statistical issues important to the park, but which cannot be generalized on a large scale than North Dobrogea Plateau. Research results, provide scientific substantiation for the phenaspects mapping, which can be used as a basis for planning work in ecological reconstruction of natural ecosystems, and natural resource exploitation activities in the park area. These observations also serve tourists access regulation in certain areas and / or periods, in the integral protection zones, to preserve local biodiversity unaltered (17). Methods Observations were made in Pricopan Peak- Macin Mountains National Park, between 2005-2009 and we monitored the development of phenophases in 50 herbaceous species, coupled with the dynamics of climatic elements, temperature and rainfall. Observations were carried out in "key areas" which is the general picture of environmental conditions in the park: height, sunny slopes and shady slopes, foot of slope with sunny and shaded exhibition, wide and narrow valley and wet. Study on phenaspects requires systematic works of field data collection, determination of species (2, 5, 18) and data processing according to the methodology used in the specialty literature (3, 6, 10, 11). In selecting taxa for priority observation were made for those considered threatened (14), and those with high percentage of park plant associations (16). Findings were performed on phenological populations in large areas containing 40-50 individuals of all species proposed for research. Calendar of data 278

collection plan was drawn up having in view that observations are carried out in grassland steppe, characterized by dominance of species with fastgrowing herbaceous species. Starting in January and February when vernal plants spring up and when vernal sap starts from trees and shrubs, findings were made at 5-6 days, and from March to April in 4-5 days. From the second decade of April to the end of June when the park runs all phenophases, the observations were made at shorter intervals at 3-4 days. In July and August, during the ripening of fruit, coloring or drying of leaves and stems of herbaceous species, observations were needed again at 4-5 days and in September and October when the leaves start coloring, fruit ripening and woody species to disseminate, observations were made at 5-6 days. In October and throughout December observations were made for monitoring the presence of late flowering plants, observations were made weekly. The phase was considered the first since its alert until the last individuals of the population. For example, flowering phenophase was considered as follows: appearance of first flowers, mass flowering, withering of first flowers, and end of flowering. To correlate conducting phenophases with climate elements we used data provided by the Environmental Protection Tulcea Agency, closest Macin Mountains venue research. To correlate conducting phenophases with climate elements we used data provided by the Environmental Protection Tulcea Agency, closest Macin Mountains venue research. For climate representation, climatic diagrams were created using the Gaussen-Walter system. For the temperate climate, the right scale for temperature representation (T) and precipitation (P) is T/P = 1:2 which defines humid and arid periods, and T/P =1:3 scale which allows for the separation of the dry periods (3, 11). Results and Discussions 1. Climate characterization based on diagrams A comparative analysis of the temperature Fig. 1 Gaussen-Walter climatic diagram for Macin Mountains area: a- meteorological station; b- altitude; c- years of observation; d- annual mean temperature; e- annual mean precipitations; f- monthly mean temperature of the coldest month; g- absolute minimum temperature; h- average temperature of the hottest day; i- absolute maximum temperature; k- period of minimum temperatures, below 0ºC; l- monthly mean temperature curve; m- precipitation curve ½ scale; n- precipitation curve, 1/3 scale; o-drought periods; p- dry periods; r- wet periods. 279

between 2005-2009 shows that 2007 was characterized by the highest isothermal values: 10 % higher than the average of 2005, 12% higher than 2006 and 2009 and 4.6% higher than 2008. Regarding the monthly mean temperature, 2007 had the highest values, while the differences between the other years were 1-2ºC (22). The mean monthly rainfall curve has 2 maximum, one in June, when summer begins and another one in autumn. For Dobrogea, multiannual climatic tables show the first wet maximum in June as well (19, 21). According to the classification system of the climates (8, 20), Pricopan Peak is characterized by moderate continental climate, with sub-mediterranean influences due to the distribution in precipitation, with two annual maximums, at the beginning and at the end of the vegetation phase and relatively high mean annual temperature (11ºC). The results of the climate analysis, the number and length of dry periods shows that 2007 (13) and 2009 had a climate less favorable to vegetation. 2. Phenological Results Vegetative phase. Seedling emergence occurs in January with Crocus reticulatus and in February with Lamium amplexicaule, Ranunculus illyricus, Poa bulbosa, Rumex acetosella, Holosteum umbellatum. The comparative observations carried out during the five years of research reveal slight variations indicate the existence of a relationship between temperature and intensity of physiological processes in plants (3). Thus, seedling emergence was possible in January due to positive temperatures (>0ºC), in 2005 (2.4ºC), 2007, 2008 (0.4ºC) and 2009 (0.8ºC). January 2005 was the coldest month (-3.9ºC) and the least favorable to the vegetation. The peak vegetative phase occurs in March at 47% species, slightly decreases in April (27.8% species) while in May only 3.6% of species show fully grown vegetative shoots and floriferous stems. The end of leafing occurs in mid June in Allium guttatum, while with Sempervivum zeleborii the vegetative phase lasts longer until September-October. Flower budding phase starts in January with Crocus reticulatus and slightly decreases towards the end of June. Flower buds can still be observed at the end of July in a few species: Moehringia grisebachii, Dianthus nardiformis, Allium guttatum, Allium flavum ssp.tauricum, Helichrysum arenarium, and in August by Silene compacta, Linaria genistifolia, and Sempervivum zeleborii. Phenological variations of 5 to 20 days recorded for the beginning of this phase can be correlated with the variations in air temperature (1-2ºC) recorded during this month and also with freezing days, air humidity, wind direction and intensity. Fig. 2 Leafing beginning in herbaceous species, between 2005-2009 in the commencement of the vegetative phase, a fact that was correlated to the corresponding temperature values of this phenological phase (fig.2). In 2007 the vegetative phase was observed commencing in January for more than 50% of the species. The early start in 2007 may be due to the very mild (5.2ºC average) and humid winter (159.5 l/m ² ) of 2006 and high average temperatures recorded in January 2007 (5.3ºC), compared to the average temperature of the other years (22). These results Flowering phase occurs from the second half of January with Crocus reticulatus, followed in February with Gagea minima and later in March with Lamium amplexicaule, Gagea pusilla, Holosteum umbellatum, Alyssum alyssoides, and Viola odorata. Data collected in the field reveals variations regarding the commencement of flowering phase of herbaceous species. Thus, flowering phase began in the second half of January only between 2007-2009. The delay of this phenophase past January 2006 can be 280

correlated with low temperatures below 0ºC recorded for the month (-3.9ºC). Mass flowering in more than 50% of species (Fig. 3) is made from mid-may and throughout June including. For most of the gramineae species (Phleum phleoides, Melica ciliata ssp. taurica, Festuca ssp.capitatum, Solidago virgaurea, Alyssum murale, which typically bloom in fall and regeneration flowers: Moehringia grisebachii, Silene compacta, Campanula romanica, Dianthus nardiformis, Achillea coarctata, Thymus zygioides, Silene cserei. Although a vernal plant, Viola odorata distinguishes by early (advance) Fig. 3 Mass flowering in herbaceous species, between 2005-2009 valesiaca etc.), peak flowering occurs in June as well. Starting with July, the number of herbaceous species in the flowering phase decreases (with approximately 25%), continuing in August (with approximately 10%), while in September only Linaria genistifolia, Silene compacta, Alyssum murale, Solidago virgaurea, Campanula romanica, Dianthus nardiformis, Allium flavum show flowers. In Dobrogea water is the restrictive factor for vegetation (6, 16), as a result of the annual variation in the climate (11), physiological modifications in plants occur (3). This would explain peak flowering in June, before the long drought periods in July and August (fig.1) Once again the correlation between flowering and temperature levels was established. Species such as Allium flavum and Allium guttatum, show flowers in June 2007 (23.2ºC) and in July in the other years of the research (average 23ºC). Viola odorata, Holosteum umbellatum, Gagea pusilla show flowers in the second decade of March in 2007, 2008 (8ºC) and in the first decade of April in 2005, 2006 and 2009 (average of 10.5ºC). Important to note is the presence of late flowering plants (12, 3). Thus in late autumns of the years 2008 (24.X), 2007 (10.X) and 2006 (09. XII) there were flowers in: Linaria genistifolia, Sempervivum zeleborii, Teucrium polium flowering d in December of 2006. Fructification was observed the earliest in February with Crocus reticulatus, Gagea minima, Gagea pusilla, Holosteum umbellatum and the latest in August with Sempervivum zeleborii, Linaria genistifolia, Veronica spicata, Centaurea salonitana. As far as fruit ripening (fig.4), the phase begins in March in 3.6% of species (Crocus reticulatus, Gagea minima i.e.), increases slightly in April in 5.6% of species (Gagea pusilla, Tussilago farfara, Scilla bifolia) while in May is present in 11.2% of species (Muscari racemosum, Holosteum umbellatum, Viola odorata). Peak fructification occurs in approximately 75% of the species in June (Alyssum saxatile, Ranunculus illyricus, Potentilla recta, Stipa lessingiana, Poa bulbosa etc.) July (Vincetoxicum hirundinaria, Allium rotundum, Phleum phleoides, Sedum urvillei, Thymus zygioides etc.) and the first half of August (Achillea coarctata, Allium guttatum, Convolvulus cantabricus, Festuca valesiaca, Dianthus nardiformis Silene cserei, Teucrium chamaedrys, Campanula romanica). Ripen fruits are observed in September in (Solidago virgaurea, Linaria genistifolia, Silene compacta), and in October in the species with extended flowering phase (Solidago virgaurea, Linaria genistifolia, Moehringia grisebachii, Campanula romanica etc.). 281

Fig. 4 Ripening fruit mass in herbaceous species, between 2005-2006 Peak fructification occurs in June, July and August and is correlated to the presence of dry and semi-dry periods. The prolonged drought of April-May 2007 (fig.1) accelerated the flowering phase in aestival species, followed by fruit ripening in July with a highest value (39%) of the analyzed periods. The drought of April 2009 was short, with no intensity and followed by a very wet period, and therefore had less influence upon vegetation. As a result the phenophase was not different from other years of the research. End of vegetative phase occurs very early (01.03.2007) in Crocus reticulatus, and other geophyte species (Gagea minima, Gagea pusilla, Muscari racemosum, Scilla bifolia), and vernal plants (Anthemis austriaca, Tragopogon dubius, Sanguisorba minor etc.), the end of vegetative phase is observed in the second half of April and the first decade of May (fig.5). Peak in leaf and stalk coloration and drying occurs for approximately 74% of herbaceous species, starting with the last decade of June (Leontodon Fig. 5 Vegetation end in herbaceous species, between 2005-2009 282

crispus, Achillea coarctata, Melica ciliata, Lychnis viscaria, Iris sintenisii, Hieracium pilosella etc.) until the second decade of August (Thymus zygioides, Silene cserei, Centaurea salonitana, Helichrysum arenarium, Rumex acetosella). In most of plants, the beginning of leaf coloration or drying occurs before the end of flowering phase. Vegetative pause is distinct with a layer of dried annual and perennial herbaceous plants whose aerial parts remain intact during the winter such as: gramineae (Stipa capillata, Festuca valesiaca, Melica ciliata etc.), and other species: Achillea coarctata, Silene compacta, Linaria genistifolia, Verbascum compacta, Solidago virgaurea, Moehringia grisebachii, Dianthus nardiformis etc.). Vegetative shoots are noticeable starting with July in Leontodon crispus, Tragopogon dubius, in August in Phlomis tuberosa, Hieracium cymosum and in September- October in Achillea millefolium and Achillea coarctata. Vegetative pause starts in chamaeophytes in July, with Alyssum saxatile, Lychnis viscaria, continues in September (Thymus zygioides, Alyssum murale etc.) and October (Campanula romanica, Teucrium polium etc.). Entry at rest does not match the species analyzed, aspect that can be correlated with expression Fig. 6 Dormant vegetative phase in biological forms phlomoides, Centaurea solstiţialis, and Centaurea difussa. Vegetative pause begins the earliest in March (fig.6), with geophytes (4) such as Crocus reticulatus, followed in April-May by Gagea, Scilla bifolia, Muscari racemosum, Orchis simia, Iris suaveolens, and in June with Polygonatum odoratum, Allium rotundum while Allium guttatum and Allium flavum start the latest, in September. Vegetative pause occurs the earliest in May with teropyte species such as Holosteum umbellatum, but for most of them (approximately 60%) the vegetative pause occurs in July (Alyssum alyssoides, Anthemis austriaca, Tragopogon dubius etc.) and the latest in November (Silene compacta). Hemicryptophytes enter their vegetative pause the earliest in June, with Poa bulbosa, Stipa lessingiana etc. For approximately 37% of them, vegetative pause occurs in September (Achillea millefolium, Viola odorata, Phleum phleoides, Veronica spicata etc.), however there are species beginning their vegetative pause in November (Silene of climatic factors. Thus advancing in the phenophases in 2007, was determined by the duration (122 days) and intensity of drought (fig. 1), which coincided with a growing season almost all species in the park. A special aspect of phenological observations was the high abundance of different species in some years. Thus 2005, 2006 were years of Silene compacta (in 2007, 2008 was rare), 2007 favorable to Potentilla recta, Stipa lessingiana, Campanula rapunculus, 2008 was the year for Althaea pallida (rare in 2005, 2006, 2007 ) and Alyssum murale (rare in 2005, 2006), 2006 a favorable year to Campanula sibirica. The time interval 2005-2009, Pulsatilla balcana was observed only in 2006, and Orchis purpurea only in 2007. Conclusions Multiannual variations of ecological factors influenced the phenological phases, vegetation having a well known ability to adapt to changing ecological factors. Differences in phenological phases are evident, 283

however not profound, and their occurrence is correlated to the higher or lower levels of arid climate within the studied periods of time. These results regarding the phenophases development correlated with the dynamics of climatic factors support the hypothesis that a major climate change would have consequences on biodiversity through species extinction in the park. No doubt, the dynamic character of the climate constitutes one of the main causes of changes within the phenological phases. However, the process itself may be as well influenced by other factors such as: wind direction and intensity, atmospheric humidity, changes in landscape, sudden variations in temperature, and pollution. Bibliography 1.Andrei, M., Popescu, A. -1967- Characterization of Peak Pricopan and the surrounding flora. St. and Cerc. Biolog., Botanical Series, T.19, Nr.1, p. 33-34, Bucharest. 2.Beldie, Al. -1979- Romanian flora, I-II. Academy Publishing House, Socialist Republic of Romania. 3.Bîndiu, C., Dihoru, GH., Doniţă, N., Drăguţ, N., Eliescu, GR., Hondru, N., Ionescu, M. A., Mărgărit, GR., Mocanu, V., Niculescu-Burlacu, F., Popescu- Zeletin, I., Zamfirescu, A. -1971- Ecology researches in Babadag Plateau. Academy Publishing House, Socialist Republic of Romania. 4.Braun-Blanquet, J. -1964- Pflanzensoziologie, Grundzüge der Vegetationskunde, Springer-Verlag, Wien-New York. 5.Ciocârlan, V. -2009- Illustrated Flora of Romania. Ceres Publishing House, Bucharest. 6.Dihoru, Gh., Doniţă, N. -1970- Flora and vegetation Babadag Plateau, Academy Publishing House, Socialist Republic of Romania. 7.Dinu, C. -1990- Need to preserve flora and vegetation of Cheia zone, Macin Mountains, Protection of nature and the environment, T. 34, 1-2, Bucharest, p. 45-49. 8.Gaussen, H. -1965- Délimitation des aires de végétation selon le climat, XII-e Congrès de l Union internationale des Instituts de recherches forestières, Oxford, Rapport, vol.i, Londra, 1958, p. 134-137. 9.Gherghişan Ecaterina-2011- Studies regarding phenology of several woody species in Peak Pricopan area, Annals of the University of Craiova, Biology series, Horticulture, agricultural product processing technology, Environmental Engineering, Vol. XVI (LII), p.160-166. 10.Ivan, D., Donită, N., -1975- Methods for the study of vegetation ecological and geographical (Multiplication of the Bucharest University Center) 11.Ivan, D. -1979- Phytocenology and vegetation R.S.R., Didactic and Pedagogical Publishing House, Bucharest. 12.Maevschi, F.P. -1961- Osenniaia Flora, Moscova. 13.Maheras, P., Tolika, K., Tegoulias, I., -2008- Le bilan thermique de l anne 2007: un retour vers l avenir?, XXI ème colloque de l Association Internationale de Climatologie, Université Paul- Valéry-Montpellier III,. Editeur scientifique Freddy VINET, p. 425-430. 14.Oltean, M., Negrean, G., Popescu, A., Roman, N., Dihoru, G., Sanda, V., Mihăilescu, S. -1994- Red List of higher plants in Romania. Studies, synthesis and documentation of Ecology, No. 1, Romanian Academy, Bucharest. 15.Petrescu, M -2000- Das măcin Gebirge-Flora und Vegetation, Carinthia II, Klagenfurt, 87-101. 16.Petrescu, M -2004- Research on biodiversity of forest ecosystems in North Dobrogea. Publisher Neremia Napocae, Tulcea. 17.Petrescu, M -2007- Dobrogea and the Danube Delta, flora and habitat conservation, Natural Sciences Series, No.2. Tulcea. 18.Săvulescu, T. -1952-1976- Flora of Romanian People's Republic, I-XIII, Bucharest. 19.Stoenescu, St. M. -1958- Some new data to summary characterize the climate of Dobrogea, in Achievements in Peoples Republic of Romania geography during 1947-1957, State Publishing House, Bucharest, p.48-57. 20.Walter, H. -1963- La productivité du tapis végétal, Lejennia, Rév. Bot. (Liège), 22, août (nouvelle série), p. 1-13. *** -1960- Geographical monograph of Romanian People's Republic, vol I. ***- 2005, 2006, 2007, 2008, 2009 Environmental status report in Tulcea County, Environmental Protection Tulcea Agency. 284