research article

Study of Multielement Concentration in Bulgarian Black Sea Green Macroalgae

Alexander Strezov*, Emilia Nikolova

Department of Radio Chemistry and Radio Ecology, Sofia University, Bulgaria

*Corresponding author: Alexander Strezov, Department of Radio Chemistry and Radio Ecology, Sofia University, Bulgaria. Email: astrezov@abv.bg

Received Date: 20 June, 2018; Accepted Date: 03 July, 2018; Published Date: 09 July, 2018

Citation: Strezov A, Emilia N (2018) Study of Multielement Concentration in Bulgarian Black Sea Green Macroalgae. Curr Trends Oceanogr Mar Sci: CTOMS-103. DOI: 10.29011/ CTOMS-103.100003

1.                   Abstract

The ecological status at eight coastal locations (Shabla, Kaliakra, Tuzlata, Ravda, Ahtopol, Sinemoretz and Rezovo) along the Bulgarian Black Sea coast was studied by determining of 32 elements in 121 samples of eight green Macroalgae species Ulva rigida, Ulva lactuca, Enteromorpha, Enteromorpha compressa, Cladophora vagabunda, Cladophora coleotrix, Chaetomorpha gracilis and Bryopsis plumosa during the period 1996-2011. The element concentrations were determined by Energy Dispersive X Ray Fluorescence Analysis (EDXRFA).

Results for 19 elements in the three most widespread green algae Ulva rigida, Enteromorpha intestinalis, Cladophora vagabunda, are compared in all the locations along the Bulgarian coast to evaluate the level of accumulated elements. It was shown that Ulva rigida and Bryopsis plumosa species accumulate studied elements less than the other species and the heavy metal concentration in green Macrophytes from Tuzlata, Ravda and Sinemoretz is higher compared to the other locations.

The obtained data show that no serious contamination by hazardous elements in green algae along the Black Sea shore during the studied period was found and some of the studied green algae species are suitable for heavy metal assessment in Black Sea marine ecosystems. The obtained results establish a database for element concentration in green Macroalgae and their ecological impact on marine ecosystems along the Bulgarian Black Sea coast.

2.                   Keywords: Black Sea; Green Macroalgae; Trace Metals; XRFA Method

1.                   Introduction

The ecological monitoring of marine ecosystems can be performed by controlling marine organisms that have been successfully used as bio-indicators. The bio monitors are important indicators for evaluation of various contaminants impact on marine ecosystems. Macroalgae have been used as indicators for trace elements, because of their accumulation capacity and influence along the trophic chaining the marine environment [1-3]. Algae can bio concentrate amounts of biologically significant elements in their tissues. Some elements are essential for aquatic plant growth and their biological uptake is a function of the free element concentration in seawater. However, increase in element concentrations above certain values can be toxic to marine biota. Some algae have mutation capability so they can survive the ecological stress of the contamination. The determination of widespread bio monitors will allow comparison of accumulated element concentrations over large areas [4-5].

The Black Sea is a low salinity basin, half-isolated from the Mediterranean and its hydrology and phytobentos concentration is different from the other seas in the same area. Toxic elements (and nuclides) are introduced by airborne contaminants, rivers, oil pollution or by direct discharge of industrial wastes into the sea. Trace elements are transported via the seawater currents, coming from the Danube and other rivers. The ecological conditions at the coastal zone are diverse which results in element concentration variations in algae depending on many factors - species type, geographical location, season etc.

Green Macroalgae have been extensively used to monitor marine pollution in various geographical areas [6-9]. Green algae are among the widespread at the Bulgarian Black Sea coast, some of them (Ulva rigida, Enteromorpha intestinalis, Cladophora vagabunda) can be met at almost all areas, so they are appropriate for comparative assessment of contaminants concentration in different geographical areas. Green Macroalgae species have been used as bio-indicators in the Black Sea and other marine environments in neighboring seas [10-15]. Trace element concentrations in Black Sea green alga species have been determined by other authors [16-19] while data about heavy and toxic metals at the Bulgarian Black Sea coastal zone is scarce and insufficient. The purpose of this paper is to study the level and accumulation of 32 elements in eight macrophytes, collected from nine locations along the Bulgarian Black Sea coast during the period 1996 - 2011. It is important to determine whether these algae can be used as bio-indicators for some element pollution and evaluate the impact on the marine ecosystem habitat. Energy-dispersive X-Ray fluorescence method (EDXRFA) was used for trace element determination.[20-21]. This method was applied because of its Multielement capability, nondestructive analysis, simple sample preparation, relative little time consuming, sufficient sensitivity, accuracy and good reproducibility. Compared to ICP, the amount of analyzed sample is bigger (30 g), which reduces the influence of inhomogeneity error.

2.                   Materials and Methods

Sampling sites in this study were selected to cover the whole Bulgarian coastline from north to south - Shabla, Kaliakra, Tuzlata, Rossenetz, Ravda, Sozopol, Ahtopol, Sinemoretz and Rezovo and to possess abundant algae species. Eight green Macroalgae species (Ulva rigida, Ulva Lactuca, Enteromorpha  Enteromorpha compressa, Cladophora vagabunda, Cladophora coleotrix, Chaetomorpha gracilis, and Bryopsis plumosa) were collected during the period between spring 1996 and spring 2011.The algae were collected in the subtidal zone at 1 - 4 m depth and those abundantly covered with epiphyte were ejected. The samples were rinsed in clean seawater, followed by distilled water, dried to constant weight (85°C) and the grinded 0.5 grams of three subsamples.

Three spectrometric systems are available in EDXRFA Lab. The first one is equipped with Si(Li) detector with 12 mm Be window and 170 eV energy resolution at 5.9 KevMN-Kaline (PGT). The data are acquired with a multichannel analyzer (AX-1), interfaced to a personal computer, that applies specialized software for data acquisition and spectra processing. This system is combined with an exciting head, based on an annular source 241Am (3.7 GBq) (AMERSHAM) and three types of secondary targets (Mo, Dy, Sn) in two excitation modes - transition and reflection in order to select the desired exciting energy. For determination of heavy elements, which are essential for biology the system uses secondary target of Dy, that allows detection of elements down to the Z = 50. This construction permits the measurement of great number of elements with a high sensitivity by achieving the desirable experimental conditions of low background level and at a high count rate.

The second system is equipped especially for light element analysis with Si pin diode detector, Peltie cooling, with 7 mm Be window and 160 eV (KETEK). The determination is performed with three radionuclide sources 55Fe(AMERSHAM) by means of an exciting head, especially designed for low Z elements. In this case the construction, the distances between the source and sample and sample-detector are greatly reduced and optimized, which allows elements with atomic number Z = 13 to 25 to be analyzed.

The third system is equipped with SDD detector with 0.7 mm Be window and 170 eV energy resolution at 5.9 KevMN-Kline (KETEK). An exciting head with source of 238Pu is specially designed for analyzing of elements with Z between 17 and 35. This head is very suitable for analyzing very low concentrations of these elements. The calibration procedures for each spectrometer are based on set of international standards like Bowen’s kale, orchard leaves, grass (IAEA - V10), fish flesh (IAEA), copepod (IAEA), Nettle etc. The results were checked with IAEA standard - lichen. Lichen was chosen because of the similar matrix with the green algae due to their similar biochemistry. The Lab has also taken part in two International Inter compression Projects - Worldwide Proficiency Test for X-Ray Laboratories PTXRFIAEA/05 and 06 IAEA (2009). The LLD for elements with Z between 13 and 14 is about 1000 µg/g, for Z between 15 and 20 - about 500 µg/g, for Z between 22 and 56 about 1 to 2 µg/g. The LLD for elements Hg, Pb and U is about 5 µg/g.

3.                   Results and Discussion

There is a dependence between microelement bio sorption and their function in the organism. Most intensively accumulated are those microelements that play a major part in the metabolism. A considerable number of elements form stable complexes with proteins, phosphates and lipids. Fe, MN, and Co take part in enzyme formation and as complex compounds participate in exchange reactions. The enriched in elements lipids from algae play a major biogeochemical role for the processes of fixation, transport and sedimentation in the hydrosphere.

The selected green Macroalgae species are suitable for application because they possess potential qualities to be used as bio-indicators, the algae are sufficiently widespread, characteristic for the studied areas, possess enough biomass and are easily collected; and they react to the environmental changes. 32 elements have been measured using EDXRFA in 121 green algae samples - 25 for Ulva rigida, 20 for E17 for C. vagabunda, 14 for Ulva lactuca etc. in the period 1996 - 2011. Data for 19 elements are presented in this paper. The concentrations of some elements are below the LLD limits of the method and the specific spectrometric systems. The concentrations of the most interesting macro and trace elements are presented in tables and graphs.

It is interesting to evaluate the impact of elements accumulation in a certain algae species in all locations along the Black Sea coast. This evaluation can be done at sites where multiple sampling has been performed during the years and where most of most abundant algae were collected. For this reason, we have chosen Ulva rigida, E. intestinalis and C. vagabunda species to assess the ecological status of the coast. The results for 19 detected elements (Figure 1) concentrations in the three most widespread green Macroalgae species from the Bulgarian Black Sea coast, are presented in (Table 1) for Ulva rigida (Figure 2-6) (Table 2) for E. intestinalis (Figure 7-11) and in (Table 3) for C. vagabunda (Figure 12 -16). The measured high element concentrations in algae (2000 - 50000 µg/g) are those for the microelements - Al, Si, P, S Cl, K, Ca, the highest of which are for Cl and S. Cl is essential for the algae metabolism and these high concentrations are understandable. The amount of S in marine algae is much higher, then the terrestrialplants, which is probably due to the dissolved sulfates in the sea water which are sorted by the algae. Fe, Br and Sr concentrations are with one or two orders of magnitude higher than the other elements in all algae species.

The overall Fe mean value obtained for Ulva rigidia 510 mg/g and the variation range is wide (300 – 1100 mg/g ). The concentration of Fe in E. intestinalis is twice higher, compared to Ulva rigida, the mean value being about 1100 µg/g (except Sizemore Autumn’96 - 1840 µg/g and Rossenetz Spring’05 - 2885 µg/g). The mean Fe concentration in Cladophora vagabunda is close to E. intestinalis with exception of Tzarevo Spring`96 - 6680 mg/g. It is clear that the two green Cladophora and Enteromorpha species accumulate twice higher Fe concentration than Ulva species.

The results for MN in  Ulva vary in very narrow limit (the mean value 70 ± 3mg/g). The same is true for the results MN in E. intestinalis which are also close (the mean value 70 ± 3mg/g) like in Ulva rig. except two samples, (Rezovo Summer’00 – 38 µg/g, Sizemore Spring’03 - 140 µg/g) which means that MN concentration is almost constant, independent of sampling time and location. The situation for MN in Cladophora is quite different – in one third of the samples the concentration is about 50 µg/g, while in the other samples the concentration is four times higher except Tuzlata Spring`99 - 371 µg/g and Ahtopol Spring`05 - 430 µg/g. The element Cu and Zn belong to the group of biologically important metal ions and their compounds can be found as trace metals in the biosphere. Cu and Zn are essential for organisms’ life and its toxicity is connected with the concentrations of other essential elements and some marine algae show an ability to accumulate Cu and Zn. Trace metals should be monitored because they play an important role in metabolism and their high or low concentrations can be equally harmful to the living organisms.

Cu and Zn concentration in Ulva rigida, are presented in The Cu values in Ulva, Enteromorpha and Cladophora are close – many of the samples are in the range of 5 - 7 µg/g (while the mean Zn value is 38 ±3 µg/g) except several samples where the concentrations are three or four times higher. Cu and Zn concentrations are almost constant in the uncertainty limit of the method and are also independent of sampling time and location. Two sampling sites (Bjala and Pomorie) have considerably higher Cu and Zn concentration. The case with the Rossenetz location (Sping’05 - 111 µg/g) is completely different – there is a copper mine in the vicinity and the concentration of all elements is completely different than all other sites due to the human mining activity.

Copper concentration determined in algae during the present investigation is comparable with those reported by for algae collected from Crimean coast at the Black Sea, while for lead (nonessential element, but it is present in all biomaterials) the concentrations are lower than those found by Burdin. Pb is found in seawaters mainly in the form of different organic compounds. As it is seen from Pb and Sn data for the three green algae in the highest lead concentration is measured in spring 1996 - 1998, while the concentrations decrease during the next sampling period. The measured concentration for Pb is close to typical Pb obtained for the terrestrial plants.

The concentration of Sn in Ulva are relatively constant (mean 11 ± 3 µg/g), except Bjala (28 µg/g). The Sn values for E. intestinalis vary more and are higher than the other two green algae samples and are close to those measured in marine sediments.  Cd concentration in Ulva (~4 µg/g) was measured only in four samples from Tuzlata (2), St. Constantine & Elena and Ahtopol. Cd is not measured in all samples for the other green algae (in Enteromorpha - 4, and C. vagabunda only two sites). The overall concentration of Pb, Sn and Cd in the sample Tuzlata Spring 98 is three times higher than all other measured algae samples.

It should be pointed out that some samples differ substantially from the others, which can be attributed to the various factors affecting elements accumulation and the specific conditions of studied locations especially depending on the sampling time (mainly spring). Another example for great deviation of elements values is the data (mg/g) for Ulva rigida in Bjala location Spring 2004 and C. vagabunda in Tzarevo Spring`1996. The concentration of halogen elements Cl, Br and I, which are biologically important for the algae and marine biota, were measured also in Ulva rigida, E. intestinalis and C. vagabunda. The obtained average value for Br and I are close for both green algae Ulva rigida, E. intestinalis (360 µg/g - for Br and 47 µg/g for I. while the Br value in Cladophora is twice lower. Lower values were measured for E. intestinalis from Tuzlata Autumn 2005, Sinemorez Autumn 1996, Sinemorez Autumn 2002, suggesting seasonal dependence. The measured Cl values in E. intestinalis and C. vagabunda are higher (mean value 30800 µg/g) compared to those of Ulva r. (22400 µg/g). The values in half of the samples in Cladophora are twice higher than the other samples.

The concentration of alkaline earth elements Ca, Sr and Ba was obtained for Ulva rigida, E.intestinalis and C. vagabunda The data for Ulva and Enteromorpha showed no specific dependence on location or time of sampling while the Cladofora values varied to a greater extent. The average value for Sr in Ulva rigida is lower (~150 µg/g) than those for Enteromorpha (~340 µg/g) and Cladophora(~280 µg/g) with several samples with much higher values. The average value for the barium concentration for the three algae is close (~40 µg/g) also with few exceptions. The Ba value in Tzarevo Sping`96 is exceptionally high 300 µg/g but the sampling was performed close to the area of the port. We have investigated several other green algae - Ulva lactuca, Bryopsis plumosa, Enteromorpha compressa, Cladophora coleotrix, Chaetomorpha gracilis. The data obtained for Ulva lactuca species were from locations Rusalka, Bjala, Tzarevo and Sizemore at the Bulgarian Black Sea coast. The determined element concentrations are similar to those, obtained for Ulva rigida. The concentrations of the most of elements in Bjala location are higher compared to the other sites (like Ulva rigida) – for Fe – 1125 ± 50 µg/g, Cu – 14 ± 2 µg/g, Zn – 78 ± 5 µg/g, Br - 807 ± 20 µg/g, Ba - 84 ± 5 µg/gSn - 28 ± 2 µg/g, Rb – 23 ± 2 µg/g. MN concentration is twice higher in two locations (Sinemorez Spring`98, Tzarevo Autumn`02) than the rest sites. Unlike Ulva rigida species, in Ulva lactuca Cd was measured only in two locations - Tzarevo Autumn`02 - 4 ± 1 µg/g, Sinemorez Spring`05 - 6 ± 1 µg/g.

The data for Enteromorpha compressa are similar to those of  E. intestinalis. The same is true for both the Cladophora algae species (e.g. higher concentration of I). The measured values for the different elements in Chaetomorphagracilis are closer to C. vagabunda, than to the two green Ulva rigida and Enteromorphavaga. Special attention should be about the green alga Bryopsis plumosa. The elements from alkaline earth group -Sr and Ba are accumulated to much higher extent – two to four orders of magnitude (~30000 µg/g for Ba (~50 µg/g for the other green algae); ~4000 µg/g for Sr (~200 for the others). The concentrations of I is ~2000 µg/g (~50 µg/g for the others). We have measured [13] radio metrically the Ra daughter isotope concentrations and also found three orders of magnitude higher concentration compared to all other algae. This comes to confirm the specific accumulation of alkaline earth elements by the green alga Bryopsis plumosa.

4.                   Conclusion

The concentrations of 32 elements have been determined in eight Black Sea green Macroalgae from nine locations along the Bulgarian Black sea coast during the period 1996-2011. If Fe data during the monitoring period are compared, no clear seasonal or location dependence can be observed. It has been shown that Ulva rigida and Bryopsis plumosa species accumulate studied elements less than the other species and the element concentration in green macrophytes from Tuzlata, Ravda and Sinemoretz is higher compared to the other locations.

The obtained data show that no serious artificial pollution along our shore and element concentrations in algae during the studied period demonstrate considerably constant accumulation pattern. The studied green algae species are suitable for assessment of element behavior in Black Sea marine ecosystems (especially Ulva, Enteromorpha and Cladophora) and can be used as bio-indicators species for the ecological status of the ecosystem, together with the abiotic element concentration in the ecosystem (water, sediment). This work contributes to the evaluation of for heavy metal concentration in green Macroalgae and their ecological impact on marine ecosystems along the Bulgarian Black Sea coast. 


Figure 1:   Map of sampling locations.



Figure 2:  Fe concentration in Ulva species.



Figure 3: MN, Cu, Zn concentration in Ulva species.



Figure 4: Sn and Pb concentration in Ulva species.



Figure 5:Sr and Ba concentration in Ulva species.



Figure 6:  Br and I concentration in Ulva species.



Figure 7: Fe concentration in Enteromorpha species.



Figure 8: MN, Cu and Zn concentration in Enteromorpha species.



Figure 9: Cd, Sn and Pb concentration in Enteromorpha species.



Figure 10: Br and I concentration in Enteromorpha species.



Figure 11: Cd, Sn and Pb concentration in Enteromorpha species.



Figure 12: Fe concentration in Cladophora species.



Figure 13: MN, Cu and Cu concentration in Cladophora species.



Figure 14: Cd, Sn and Pb concentration in Cladophora species.



Figure 15: Ba and Sr concentration in Cladophora species.



Figure 16: Br and I concentration in Cladophora species.


 

Site

Season

Si

P

S

Cl

K

Ca

Ti

Cr

Mn

Fe

Cu

Zn

Br

Rb

Sr

Sn

I

Ba

Pb

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

Tuzlata

Spring

10250

2900

21750

45100

18800

14100

30

31

73

710

2

39

380

21

140

12

47

23

13

1996

±500

±300

±500

±1600

±400

±500

±3

±3

±2

±25

±1

±2

±15

±2

±3

±2

±2

±2

±2

Tuzlata

Autumn

7700

2750

21800

29400

13700

12300

28

 

71

500

2

 

290

14

110

10

26

29

23

1996

±500

±250

±500

±1300

±400

±300

±2

 

±2

±20

±1

 

±11

±2

±8

±1

±1

±1

±2

Ahtopol

Autumn

7600

2650

23500

18700

11000

11100

35

 

72

415

 

 

210

6

100

 

28

12

3

1996

±1500

±300

±800

±1200

±850

±500

±3

 

±3

±20

 

 

±15

±2

±8

 

±3

±2

±2

Ravda

Autumn

8000

2500

26800

14300

11500

10300

27

34

74

460

5

27

258

20

121

12

52

22

20

1996

±800

±300

±1000

±900

±700

±350

±2

±2

±2

±10

±1

±3

±4

±2

±5

±3

±3

±2

±5

Sinemorez

Autumn

10500

2100

13300

36850

14700

13300

32

 

65

730

10

33

336

10

152

 

70

112

6

1996

±1200

±250

±850

±1200

±850

±160

±2

 

±5

±35

±2

±2

±8

±2

±9

 

±4

±10

±3

Ahtopol

Summer

6700

2000

23200

11600

13200

10900

30

35

71

500

4

31

288

23

156

9

44

32

24

1997

±500

±200

±700

±200

±450

±200

±3

±3

±2

±20

±2

±2

±12

±2

±6

±2

±2

±3

±3

Maslen

Spring

7900

2200

17300

21300

17000

11100

23

55

73

450

5

34

372

22

109

12

48

28

30

nos

1998

±900

±500

±800

±850

±350

±120

±3

±5

±2

±30

±2

±3

±5

±3

±9

±2

±2

±3

±6

Ahtopol

Spring

7000

2200

23200

21200

11400

12300

24

 

73

440

3

 

371

15

160

16

56

40

10

1998

±850

±500

±1200

±1200

±400

±400

±1

 

±2

±5

±1

 

±15

±2

±7

±1

±4

±4

±2

Ravda

Spring

11000

2300

25000

14600

14200

11300

40

24

73

460

 

23

228

14

103

8

27

19

10

1999

±2000

±500

±600

±700

±800

±300

±5

±2

±2

±10

 

±2

±10

±3

±8

±2

±2

±3

±3

Shabla

Summer

11200

1470

23200

20600

12000

12400

47

 

71

650

1

11

453

22

106

6

39

14

9

2000

±1500

±200

±1200

±600

±120

±120

±3

 

±3

±30

±1

±2

±10

±2

±8

±2

±3

±2

±3

Kaliakra

Summer

8400

2600

27200

19000

11860

11070

31

30

71

480

3

48

464

20

116

12

79

26

6

2000

±800

±250

±2000

±1500

±1000

±600

±3

±3

±2

±20

±1

±4

±8

±2

±4

±2

±7

±3

±3

Ahtopol

Summer

15000

2500

30000

27120

13500

14000

64

30

73

460

2

33

378

16

156

11

48

21

7

2000

±1500

±250

±1000

±1000

±500

±500

±6

±3

±3

±25

±2

±2

±15

±2

±12

±2

±2

±2

±2

Sinemorez

Summer

11800

1700

26700

16600

15400

12150

57

32

73

610

5

20

225

12

153

8

30

28

16

2000

±1000

±220

±1000

±200

±600

±600

±5

±3

±2

±15

±2

±2

±5

±2

±7

±3

±3

±2

±4

Varvara

Autumn

9800

3400

28500

17300

16300

14800

37

40

69

600

3

26

254

9

303

10

43

20

10

1996

±850

±200

±1000

±600

±800

±850

±3

±4

±3

±40

±1

±2

±12

±2

±6

±3

±2

±3

±3

Shabla

Spring

12700

3000

29000

40200

11000

14200

44

 

68

560

6

 

400

16

114

13

41

45

5

2003

±1200

±250

±1500

±850

±750

±600

±4

 

±5

±30

±2

 

±7

±2

±10

±2

±2

±3

±5

Kaliakra

Spring

12500

3500

31250

24600

11800

12250

70

35

63

470

4

 

340

11

104

9

45

78

7

2003

±1000

250

±850

±1300

±800

±450

±5

±2

±6

±10

±1

 

±20

±2

±5

±1

±2

±5

±3

Tuzlata

Spring

13300

2600

30000

21400

11900

14200

37

34

54

360

1

10

383

9

305

13

40

60

10

2003

±400

±300

±650

±1000

±400

±700

±4

±4

±4

±20

±1

±2

±15

±2

±10

±2

±2

±4

±3

Bjala

Spring

16200

4100

16300

26200

23000

12400

50

 

72

950

22

81

820

20

92

28

66

120

 

2004

±1000

±400

±500

±1000

±1000

±200

±2

 

±5

±45

±2

±5

±20

±2

±5

±3

±5

±5

 

Ravda

Spring

10300

4100

26800

20100

15100

12200

50

 

 

300

 

24

390

11

131

12

57

27

12

2005

±1000

±400

±1200

±600

±400

±600

±5

 

 

±50

 

±3

±20

±2

±12

±3

±3

±3

±3

Pomorie

Spring

23000

1850

20700

19900

10300

15400

57

 

73

1100

23

30

284

10

262

14

51

72

3

2005

±2000

±150

±350

±750

±250

±1000

±5

 

±3

±100

±3

±2

±6

±2

±8

±2

±5

±4

±3

Perla

Autumn

11700

2450

22800

17400

15800

10900

56

23

61

480

6

25

262

10

140

8

37

18

5

2005

±500

±150

±1000

±1500

±1000

±600

±2

±2

±6

±10

±1

±2

±10

±2

±12

±2

±1

±2

±2

Varvara

Spring

8500

1800

26000

16600

11000

10800

27

 

70

435

5

 

450

12

86

6

40

5

 

2005

±500

±200

±1200

±300

±250

±150

±3

 

±5

±45

±2

 

±25

±2

±8

±2

±3

±2

 

Ahtopol

Spring

9500

2600

31800

21600

12000

11500

53

 

 

400

 

 

464

9

126

 

60

21

 

2005

±500

±250

±1500

±1100

±750

±500

±5

 

 

±20

 

 

±10

±1

±3

 

±6

±3

 

Rezovo

Spring

12500

2500

28600

15200

12600

11300

43

 

72

450

5

30

404

8

113

11

30

8

4

2005

±500

±200

±1000

±500

±500

±200

±2

 

±2

±25

±2

±3

±14

±2

±2

±2

±2

±3

±2

Sozopol

Autumn

9800

1900

28300

22000

13000

14500

16

32

67

470

9

30

311

12

195

13

68

10

5

2011

±800

±200

±800

±300

±500

±300

±3

±5

±5

±25

±3

±2

±5

±2

±8

±2

±3

±2

±5

 

Table 1:  Element concentratioin in Ulva rigida.



Site

Season

Si

P

S

Cl

K

Ca

Ti

Cr

Mn

Fe

Cu

Zn

Br

Rb

Sr

Sn

I

Ba

Pb

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

Ravda

Spring

10000

2200

18500

44200

15700

14400

35

 

72

822

5

336

7

143

7

38

30

11

1996

±2000

±250

±1000

±1200

±800

±300

±1

 

±2

±20

±1

 

±10

±2

±10

±2

±3

±3

±2

Sinemorez

Autumn

9000

1500

14800

25500

8600

17400

51

 

73

1840

1

33

233

16

576

8

51

148

7

1996

±900

±200

±1200

±1500

±500

±1100

±5

 

±2

±120

±1

±2

±12

±2

±6

±2

±3

±12

±3

Tuzlata

Spring

9400

2270

14400

27100

16600

12600

36

40

72

800

3

34

290

13

137

12

48

40

34

1998

±900

±400

±400

±750

±500

±300

±4

±5

±1

±30

±2

±4

±10

±2

±10

±2

±5

±2

±5

Shabla

Spring

10700

3300

20100

33600

8500

8700

32

 

73

480

8

50

540

16

327

7

64

56

5

1999

±2000

±300

±1400

±1200

±250

±500

±2

 

±1

±10

±2

±2

±8

±2

±10

±2

±3

±5

±2

Kaliakra

Spring

9700

2600

17600

32100

13800

13300

35

 

73

687

 

44

460

16

115

6

42

17

6

1999

±1500

±200

±200

±700

±300

±200

±2

 

±2

±23

 

±1

±2

±2

±4

±2

±4

±3

±3

Tuzlata

Spring

25800

2000

17600

23300

8000

24700

76

41

70

1070

10

31

346

21

735

7

48

50

7

1999

±2800

±300

±400

±600

±200

±1400

±7

±4

±3

±70

±2

±2

±16

±2

±25

±2

±4

±3

±3

Tuzlata

Summer

22000

2500

13300

23700

15100

14100

51

 

67

973

5

24

303

13

218

8

22

20

15

2000

±1000

±200

±300

±1200

±600

±800

±5

 

±6

±55

±2

±2

±10

±1

±10

±2

±3

±2

±5

Rezovo

Summer

13500

2300

15300

32000

12400

18100

67

35

38

1356

5

2

471

24

371

14

63

64

14

2000

±1000

±300

±1200

±2200

±750

±600

±2

±3

±4

±40

±48

±3

±13

±3

±15

±2

±2

±3

±4

st Konstan

Spring

12600

2400

26400

36600

17600

13500

51

 

74

470

3

 

406

28

123

17

56

20

8

tin,st Elena

2001

±1200

±180

±500

±1200

±800

±150

±5

 

±1

±6

±1

 

±24

±2

±2

±2

±2

±3

±3

Sinemorez

Autumn

17200

2800

27200

21000

26900

14700

40

 

58

870

6

32

183

18

193

12

18

50

20

2002

±2000

±200

±500

±1600

±1800

±300

±5

 

±3

±50

±31

±3

±11

±2

±10

±2

±2

±4

±3

Kaliakra

Spring

16000

4300

26000

49200

15500

15300

34

53

73

745

5

37

444

17

127

11

50

30

 

2003

±1000

±350

±1000

±2100

±500

±500

±3

±5

±3

±17

±2

±3

±22

±3

±5

±2

±1

±3

 

Tuzlata

Spring

22400

2700

21500

37600

16400

13400

52

 

71

1128

5

34

385

18

555

10

71

131

12

2003

±2000

±200

±750

±1000

±1200

±1100

±5

 

±2

±40

±2

±3

±16

±2

±25

±2

±3

±10

±2

Ahtopol

Spring

7300

1750

19900

19500

9800

11800

43

43

72

530

5

39

381

4

178

12

52

17

5

2003

±750

±150

±1200

±500

±200

±200

±3

±2

±1

±20

±1

±3

±13

±1

±5

±2

±5

±2

±2

Sinemorez

Spring

17600

2740

20600

9000

10000

5600

50

28

140

1415

2

33

2

33

212

12

20

48

10

2003

±2000

±200

±400

±800

±600

±250

±5

±3

±50

±120

±2

±2

±2

±2

±12

±2

±2

±4

±3

Rezovo

Spring

16600

1680

18200

10400

14500

16600

57

42

62

1470

10

45

375

9

325

5

30

19

 

2003

±1000

±200

±1000

±1000

±1200

±500

±3

±4

±6

±80

±2

±2

±15

±2

±15

±2

±2

±2

 

Tuzlata

Spring

16700

2800

19800

35500

10800

25250

47

34

71

820

10

35

301

14

910

13

34

62

 

2004

±1000

±200

±700

±500

±500

±750

±5

±3

±2

±20

±2

±2

±10

±1

±30

±2

±2

±3

 

Tuzlata

Spring

10400

3100

22800

54600

11200

15300

33

36

74

480

10

43

356

15

91

 

25

22

5

2004

±1000

±300

±1000

±1000

±500

±500

±2

±2

±2

±20

±2

±2

±5

±2

±7

 

±2

±2

±5

Rosenez

Spring

15500

2500

15600

26800

13700

14000

67

 

67

2885

111

35

434

19

203

14

86

65

 

2005

±1000

±300

±1000

±2000

±500

±400

±4

 

±5

±140

±4

±3

±20

±2

±10

±2

±2

±5

 

Ahtopol

Spring

13000

3800

21700

36300

12700

20100

52

30

72

510

8

33

360

15

910

10

88

32

13

2005

±1200

±200

±1100

±1100

±300

±1200

±5

±2

±2

±20

±2

±1

±20

±2

±20

±2

±2

±2

±2

Tuzlata

Autumn

16700

3550

17500

29500

20000

19100

43

51

70

854

5

22

215

22

565

11

29

41

9

2005

±1100

±150

±1000

±1000

±500

±700

±5

±5

±2

±25

±2

±2

±10

±2

±12

±2

±2

±2

±3

 

Table 2:  Element concentration in Enteromorpha intenstinalis.


 

Site

Season

Si

P

S

Cl

K

Ca

Ti

Cr

Mn

Fe

Cu

Zn

Br

Rb

Sr

Sn

I

Ba

Pb

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

[ppm]

Tuzlata

Summer

18600

2550

13200

31700

28400

20000

38

 

256

1280

9

25

150

16

458

 

40

91

5

1992

±1500

±100

±800

±3500

±1200

±2000

±3

 

±10

±10

±1

±2

±10

±2

±15

 

±3

±3

±3

Tuzlata

Summer

13500

2100

15900

31200

28400

17800

32

37

217

1035

15

22

150

12

443

 

33

50

25

1993

±1500

±200

±500

±1000

±500

±600

±3

±3

±5

±20

±2

±2

±6

±2

±15

 

±2

±3

±3

Tuzlata

Spring

14600

3600

15600

27000

27100

17600

40

31

73

1800

7

32

197

15

300

5

40

37

9

1996

±1500

±400

±1000

±800

±250

±1500

±2

±3

±2

±60

±2

±4

±10

±2

±12

±1

±2

±3

±3

Tsarevo

Spring

37800

2670

12800

25600

14000

15300

195

 

290

6680

17

62

400

41

224

12

160

300

6

1996

±2500

±250

±300

±800

±500

±200

±10

 

±15

±330

±2

±5

±20

±3

±10

±2

±5

±20

±2

Tuzlata

Spring

17300

3120

19200

30100

23000

15000

42

27

211

1070

4

23

200

12

230

 

31

20

7

1998

±2000

±320

±500

±1000

±500

±500

±3

±2

±15

±30

±2

±2

±7

±3

±10

 

±2

±2

±2

Ravda

Spring

20600

3000

13400

52750

37300

17500

37

 

315

985

3

29

259

15

165

 

147

65

15

1998

±1500

±300

±500

±2500

±2500

±800

±5

 

±15

±10

±2

±2

±15

±1

±5

 

±5

±5

±3

Sinemoretz

Spring

23400

2650

12600

55400

41800

17700

40

27

280

1070

4

28

244

13

140

5

37

53

8

1998

±1500

±200

±200

±2000

±2500

±800

±2

±3

±30

±70

±2

±3

±15

±2

±10

±2

±2

±5

±2

Maslen

Spring

7200

3300

14200

43800

36900

13400

22

 

205

645

10

31

283

15

61

 

87

16

6

nos

1998

±1000

±400

±400

±600

±500

±300

±2

 

±6

±10

±2

±1

±10

±2

±5

 

±2

±2

±2

Kaliakra

Spring

21000

3020

17850

28700

25400

16200

80

 

56

920

6

20

178

17

161

 

37

14

8

1999

±1000

±300

±1000

±1000

±800

±800

±4

 

±5

±20

±1

±1

±12

±2

±4

 

±3

±2

±2

Tuzlata

Spring

27300

3080

17300

23900

21200

13200

57

 

371

1054

6

16

150

10

197

 

20

9

7

1999

±3000

±400

±500

±500

±350

±200

±3

 

±15

±50

±2

±2

±10

±2

±10

 

±2

±2

±3

Rezovo

Autumn

22500

3000

16100

25300

25400

29300

81

 

171

1290

 

25

180

12

311

8

161

32

15

2001

±2000

±400

±800

±1000

±500

±1500

±3

 

±12

±50

 

±2

±10

±2

±20

±2

±6

±5

±3

Sinemoretz

Autumn

25800

4600

17000

46600

27600

22100

42

34

70

953

 

 

246

8

268

 

188

35

10

2001

±2000

±500

±500

±3000

±1500

±1500

±2

±4

±3

±35

 

 

±10

±2

±10

 

±2

±4

±3

Shabla

Spring

30000

4600

17150

44500

23000

17700

91

 

220

3180

3

27

324

7

156

 

105

248

 

2003

±3000

±450

±500

±700

±300

±800

±9

 

±20

±30

±1

±2

±10

±3

±2

 

±6

±6

 

Kaliakra

Spring

16300

3900

21400

29500

32500

13700

36

 

72

1114

2

24

218

5

133

6

35

20

12

2003

±400

±500

±200

±600

±1500

±400

±2

 

±2

±50

±2

±2

±10

±2

±10

±2

±3

±2

±3

Ahtopol

Spring

55100

3470

16350

32000

24450

14200

45

30

430

954

12

34

321

7

144

7

90

18

7

2005

±2500

±100

±500

±500

±500

±200

±3

±3

±20

±10

±2

±3

±6

±2

±3

±2

±4

±2

±2

Sinemoretz

Spring

28350

2600

15800

30900

27500

17430

86

 

70

2340

5

18

132

16

345

7

106

113

10

2005

±2500

±300

±500

±1500

±2500

±1000

±6

 

±3

±200

±2

±2

±17

±2

±33

±2

±1

±6

±5

Tuzlata

Autumn

45200

3400

14240

35600

36500

22100

104

 

70

2040

3

25

185

17

395

6

143

93

 

2005

±1000

±400

±500

±1200

±1000

±2000

±4

 

±3

±100

±2

±2

±5

±2

±22

±1

±5

±7

 

  

Table 3:  Elemennt concentratioin in Cladophora vagabunda.



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2.                   Forsberg A, Soderlund S, Frank A, Petersson L, Pedersen M, et al. (1988) Studies of metal concentration in the brown seaweed, Fucus vesiculosus from the Archipelago of Stockholm. Environmental Pollution 49: 245-263.

3.                   Rainbow P (1995) Biomonitoring of heavy metal availability in the marine environment. Marine Pollution Bulletin 31: 183-192.

4.                   Rainbow P, Philips D (1993) Cosmopolitian biomonitors of trace metals. Marine Pollution Bulletin. 26 : 593-601.

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7.                   Ho Y (1990) Ulva lactuca as bio indicator of metal contamination intertidal waters in Hong Kong. Hydrobiology 203: 73-81.

8.                   Haritonidis S, Malea P (1995) Seasonal and local variation of Cr, Ni and Co concentration in Ulva rigida, C. agardh and Enteromorpha linza (Linnaeus) from Thermaikos Gulf, Greece. Environmental Pollution 89: 319-327.

9.                   Haritonidis S, Malea P (1999) Bioaccumulation of metals by the green alga Ulva rigida from Thermaikos Gulf, Greece.  Environmental Pollution 104: 365 - 372.

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11.                Locatelli C (1999) Sea water quality criteria by bioindicators. Possible classification based on metal concentrations in Ulva rigida and Tapes philippinarum. Toxicological & Environmental Chemistry 71: 435-446.

12.                Strezov A (2008) Comparison of Some Radionuclides in the Marine Coastal Environment of the Black Sea & the Mediterranean. J Eurasian Analytical Chemistry 3: 170 -182.

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