معرفی تعدادی از گونه های نانوپلانکتون های آهکی هولوسن (مگالاین) از خلیج فارس و بررسی خاصیت بایولومینسانس آنها

نوع مقاله : مقاله پژوهشی

نویسندگان

1 استادیار، دانشکده زمین شناسی، دانشکدگان علوم، دانشگاه تهران، تهران، ایران

2 استاد، دانشکده زیست شناسی، دانشکدگان علوم، دانشگاه تهران، تهران، ایران

3 دانشجوی کارشناسی، دانشکده زمین شناسی، دانشکدگان علوم، دانشگاه تهران، تهران، ایران

10.22034/irqua.2024.713609
چکیده
این مطالعه، بر روی تنوع بیولوژیکی نانوپلانکتون‌های آهکی از آبهای پنج ناحیه خلیج فارس، از غرب و جنوب جزیره هرمز، جنوب جزیره مرجانی کیش، لاوان و سواحل بوشهر دربازه­های زمانی متفاوت، طی چند سال انجام شده­است. در این تحقیق، 29 گونه از 18 جنس از نانوپلانکتون­های آهکی شناسایی شدند که نشان‌دهنده غنا و تنوع بیولوژیکی در این مناطق است. جنس و گونه‌هایی با فراوانی بالا مانند Gephyrocapsa oceanica Helicosphaera carteri, Coccolithus plagicus, Emiliania huxleyi, ، Braarudosphaera bigelowii و  Holococcolithesدر این آبها یافت شدند. مجموعه ای از نانوپلانکون­هایی که در زمان پالئوژن و کرتاسه ظهور پیدا کرده و هم اکنون نیز در دریاها حضور دارند، در آبهای این مناطق یافت شدند. همچنین یکسری آزمایشاتPCR  برای تعیین مقدار باکتریهای حاوی بایولومینسانس نیز در آن انجام شد و کم بودن مقدار باکتریهایPhotorhabdus, Shewanella, Vibrio  و  Aliivibrioکه ساکن آبهای دریایی هستند و تولید کننده آنزیم luciferase می باشند، در این آبها مشخص شد. این مطالعه نشان داد که آبهای مذکور غنی از مواد غذایی و دارای تنوع بالایی ازنانوپلانکتون­ها هستند.

کلیدواژه‌ها

موضوعات


عنوان مقاله English

Introduction of Calcareous Nannoplanktons Holocene (Megaline) Era from the Persian Gulf and investigation of their bioluminescence properties

نویسندگان English

Fariba Foroughi 1
Farideh Siavoushi 2
Mahdi Ataei Tarzangh 3
1 Assistant Professor, Faculty of Geology, Faculty of Sciences, University of Tehran, Tehran, Iran
2 Professor, Faculty of Biology, Faculty of Science, University of Tehran, Tehran, Iran
3 Bachelor student, Faculty of Geology, Faculty of Science, University of Tehran, Tehran, Iran
چکیده English

Calcareous nannoplanktons are present in today's oceans significantly (Young & Bown, 1997, Thibault et al., 2012). As Coccolithophores, they are among the calcareous marine phytoplankton that live in oceanic waters and light seawater. Many have thought that the function of Coccolithus is light for photosynthesis for Coccolithophores (Gartner & Bukry, 1969). Coccolithophores, due to having chlorophyll, make the necessary food by themselves. Coccolithophores are involved in the preparation of biochemical limestones. Calcareous nannoplanktons emerged from the Norian and Rhaetian ages, during the Triassic as very primitive and simple organisms. These organisms spread in all seas and oceans during the Jurassic and Cretaceous periods and reached their development in the Cenozoic. Calcareous nannoplanktons found from the current Triassic period to the recent era and the benefits of their study in the fields of paleontology, paleoecology, and biogeochemistry are of great importance.
Researchers such as Jalili and Hadavi (1399); Hadavi (1387); Martini (1971); Kassler (1971) and Hilbert et al. (1981) conducted studies on the sediments of the Persian Gulf. Bioluminescence properties in seawater from bacteria that live in seawater. These bacteria are Photorhabdus, Shewanella, Vibrio, and Aliivibrio, which produce luciferase enzyme and live in the body of nannoplankton. The accumulation of nannoplankton near the shores at night causes the waters to glow. By presenting detailed studies in the fields of biology, paleontology, and microbiology, this research clarifies the role of nannoplankton in the current and past ecosystems. The purpose of this study is to investigate and understand the spread of calcareous micro-organisms in four strategic regions of the Persian Gulf and the relationship with their bioluminescence characteristics in this region.
Materials and Methods
This study was carried out in the identification of Holocene calcareous nannoplankton (Megaline) in four regions of the Persian Gulf. Eight samples were collected and studied from the surface waters of the western and southern Hormuz Island in Feb. 2018 and Feb. 2023, the beaches of Bushehr in, April 2017; the coral beaches of Kish Feb. 2018, and the west of Lawan Island in August 2021. These studies are carried out based on the determination of the species based on systematics and a series of PCR tests to investigate the bioluminescence characteristics of bacteria in BHI agar and BHI broth to determine the volume of the luciferase enzyme that causes bioluminescence.
Results and discussion
Analysis and samples of eight areas indicate that this nannoplankton can withstand high temperatures (more than 17 degrees Celsius), characteristics that were expected to be achieved due to the special weather conditions and high evaporation in the Persian Gulf.
Studies also show that many species of tropical limestones such as Coccolithus palgicus, Gephyrocapsa oceanica، Helicosphaera carteri ، Reticulofenestra minutula ،Cyclicargolithus abisectus، Syracosphaera pulchra ،Pseudoemiliania ovata، Gephyrocapsa ericsonii ،Retecapsa angustiforata و Emiliania huxleyi are present in these areas. These species help regulate carbon in marine ecosystems and play a significant role in the environmental cycle.
Among the available nannoplankton from Nannoliths, Diatomite, Heterococcoliths, and Holococcolithes, in total, 41 species from 14 genera were identified. You can also see diatoms that live in marine environments.
Microbiology and biology studies on Persian Gulf water samples have shown the presence of a group of light-producing bacteria including Photorhabdus, Shewanella, Vibrio, and Aliivibrio that live in the seas. These bacteria produce luciferase enzyme and thus produce light in the visible range. In this study, only in one of the samples related to the waters of Lawan Island, very little of the optical characteristics of these samples can be seen, and the reason for this is the inappropriate storage of the waters for the test sample.
Conclusions
This study has been conducted on the biological diversity of calcareous nannoplankton from the seawaters of four regions and eight samples of the Persian Gulf, from the western and southern Hormuz Island in February 2018 and February 2023, the beaches of Bushehr in, April 2017; the coral beaches of Kish February 2018, and the west of Lawan Island in August 2021. In this research, 41 species of 14 genera of calcareous nannoplanktons were identified, which shows the richness and biological diversity in these areas.
Species with high abundance such as Gephyrocapsa oceanica, Helicosphaera carteri, Coccolithus plagicus, and Emiliania huxleyi, Holococcolithes were observed. These findings are very important because some of these species that originated from the Paleocene or Cretaceous periods such as Coccolithus plagicus, Retecapsa angustiforata, and Braarudosphaera bigelowii are still present in the seas of the present era. They can provide valuable information on the environmental history of the Persian Gulf. Also, PCR tests were performed to determine the presence of bioluminescence agents in the samples. Despite the evidence of a small presence of light-producing bacteria such as Vibrio and Aliivibrio that produce luciferase enzyme, they exist in seawater. According to the richness of nannoplankton observed, it can be concluded that Persian Gulf waters have the highest level of primary productivity and nutrients are sufficient to support different microbial and planktonic populations

کلیدواژه‌ها English

Bushehr beach
Calcareous nannoplankton
Hormuz Island
Kish Island
Lavan Island
Persian Gulf seawater
bioluminescence
پور­اسماعیل، الف، هادوی، ف.، لک، ر.، (1392). نانوپلانکتون های آهکی در رسوبات هولوسن خلیج فارس  )بندر شهید رجایی(، اقیانوس شناسی، 88/ 22،  11-1.
سنماری، س.، (1385). مطالعات بیوستراتیگرافی فرامینیفرهای پلانکتونیک و نانوفسیل­های آهکی سازند گورپی در شمال گچساران، غرب شیراز، دانشگاه آزاد اسلامی واحد علوم و تحقیقات تهران، 220 ص.
هادوی، ف.، (1390). نانوپلانکتون­های آهکی حوضه خلیج فارس. اقیانوس شناسی، 2/5 ، 41-46.
مجتهدین، الف، هادوی، الف، پوراسماعیل، الف، (1394). بررسی تغییرات شوری رسوبات هولوسن خلیج فارس تا شرق تنگه هرمز با استفاده از گونهBraarudosphaera bigelowii. نشریه کواترنری ایران، 3/1، 181-189 .
Al-Rousan, S., Pätzold, J., Al-Moghrabi, S., Wefer, G., (2004a). Invasion of anthropogenic CO2 recorded in planktonic foraminifera from the northern Gulf of Aqaba. International Journal of Earth Sciences, 93(6), 1066-1076.
Al-Rousan, S., Rasheed, M., Badran, M., (2004b). Nutrient Fluxes from Deep Sediment Support Nutrient Budget in the Oligotrophic Waters of the Gulf of Aqaba. Scientia Marina, 68 (4), 483-490.
Archer, E., Gregor, G., (2013). Validity of U.S. Nutritional Surveillance: National Health and Nutrition Examination Survey Caloric Energy Intake Data, 1971–2010, Polos one.
Auer, G., E. Piller E. W., Harzhauser, M., (2014). High-resolution calcareous nannoplankton palaeoecology as a proxy for small-scale environmental changes in the Early Miocene. Micropaleontolgy, 111: 53–65.doi: 10.1016/j.marmicro.2014.06.005
Bown, P.R., (1998). Calcareous Nannofossil Biostratigraphy.  British Micropaleontology Society Publication Series. Chapman and Hall, London, 328.
Bown, P. R., (2010). Calcareous nannofossils from the Paleogene/Eocene Thermal maximum interval of solution Tanzania (TDP Site 14). Journal of Nannoplankton Research, DOI: 10.58998/Jnr2023
Bown, P. R., Dunkley Jones, T., (2012). Calcareous nannofossils from the Paleogene equatorial Pacific (IODP Expedition 320 Sites U1331-1334). Journal of Nannoplankton Research. 32(2), 3-51.
Bornemann, A., Norris, R. D., Friedrich, O., Beckmann, B., Schouten, S., Damsté, J. S. S., Wagner, T., (2008). Isotopic evidence for glaciation during the Cretaceous super greenhouse. Science, 319(5865), 189-192.
Brownlee, C., Langer, G., Wheeler, G. L., (2020). Coccolithophore calcification: Changing paradigms in changing oceans. Acta Biomater, 120, 4-11. https://doi.org/10.1016/j.actbio.2020.07.050
Daniels, C. J., Brown, C. W., (2020). Ecological implications of ocean acidification in marine food webs. Global Change Biology, 26 (2), 287-299
Freda, M., Young, J., Lino, S., Martins, A., Narciso., A., (2010). A guide to extant Coccolithophores (Calcihaptophycidae, Haptophyta) using light microscopy. Nannoplankton Research, 31/2.
Felis, T., Lohmann, G., Kuhnert, H., Lorenz, S.L., Scholz, D., Pa¨tzold, J., A. Al-Rousan, S., M. Al-Moghrabi, S., (2003). Increased seasonality in Middle East temperatures during the last interglacial period. Nature, doi:10.1038/nature02493.
Gartner, S., Bukry, D., (1969). Tertiary holococcoliths. Journal of Paleontology, 43, 1213-1221.
Geisen, M., Billard, C., Broerse, A.T.C, Cross, L., Probert, I., Young, J.R., (2002). Life-cycle associations involving pairs of holococcolithophorid species: intraspecific variation or cryptic speciation? European Journal of Phycology, 37, 531-550.
Haj Messaoud, J., Thibault, N., Yaich, C., Monkenbusch, J., Omar, H., H.F., Ben Jemai, Watkins, D., K., (2020). The Eocene-Oligocene Transition in the South-Western Neo-Tethys (Tunisia): Astronomical Calibration and Paleoenvironmental Changes. Paleoceanography and Paleoclimatology, 35/8, https://doi.org/10.1029/2020PA003887
Hilbert, D. W., Swift, D. M., Detling, J. K., Dyer, M. I., (1981). Relative growth rates and the grazing optimization hypothesis. Oecologia, 51, 14–18.
Honjo, S., Manganini, J., Cole, J., (1982). Sedimentation of biogenic matter in the deep ocean. Deep Sea Research Part A. Oceanographic Research Papers, 29, 5, 609-625.
Houdan, A., Probert, I., Zatylny, C., Billard, C., (2004). Intraspecific variability in the coccolithophore Emiliania huxleyi. Journal of Phycology, 40 (4), 775-789.
Johnson, V. Y., Smith, R. L., Thompson, M. J., (2015). Paleoceanographic implications of calcareous nannoplankton in global climate change.  Journal of Paleoclimatology, 45(3), 203-214.
Kassler, 1971. The Structural and Geomorphic Evolution of the Persian Gulf. The Persian Gulf, 11–32.
Kiene, R. P., Linn, L. J., Bruton, J. A., (2007). New and important roles for DMSP in marine microbial communities. Journal of Sea Research, 58(2), 139-145.
Martini, E., (1971). Standard Tertiary and Quaternary calcareous nannoplankton. In: A Farinacci (Ed.), Proceedings Planktonic Conference, Romania, 2, 739–85.
Monteiro, D., Curi Estima, S., Gandra, T., P. Silva, A., R, Secchi, E., (2016). Long-term spatial and temporal patterns of sea turtle strandings in southern Brazil. Marine Biology, 6.
Rasheed, M., Al-Rusan, M., Manaseah, R., Al-Horani, F., (2006). The Oceanographic Society of Japan. Nutrient Fluxes from Deep Sediment Support Nutrient Budget in the Oligotrophic Waters of the Gulf of Aqaba. Journal of Oceanography, 62, 83- 89.
Senemari, S., 2014. Diversity changes among calcareous nannofossil assemblages across the Paleocene/Eocene Boundary in the Zagros (Southwest Iran). Journal of Tethys, 2/1, 45–54.
Smith, J., Jones, M., Brown, B., Johnson, J., (2024). The role of haptophytes in the production of dimethyl sulfide. Journal of Climate Regulation, 27(3), 456-469.
Stein, A., Russell, R. B., Aloy, P., (2005). 3did: interacting protein domains of known three-dimensional structure. Nucleic Acids Research, 33, 413–417, https://doi.org/10.1093/nar/gki037
Taylor, B.R., (2019). The impact of ocean acidification on coccolithophore calcification: Current observations and future directions. Marine Ecology Progress Series, 621, 1-15.
Thibault, N., Husson, D., Harlou, R., Gardin, S., Galbrun, B., Huret, E., Minoletti, F., (2012). Astronomical calibration of upper Campanian–Maastrichtian carbon isotope events and calcareous plankton biostratigraphy in the Indian Ocean (ODP Hole 762C): implication for the age of the Campanian–Maastrichtian boundary. Paleogeography, Palaeoclimatology, Palaeoecology, 10.1016/j. palaeo, 27
White, H.J., Marshall, D.J., (2018). Morphological diversity of Coccolithophores: Environmental conditions and evolutionary pathways. Journal of Phycology, 54(6), 703-720.
Winter, A., Henderiks, J., Beaufort, L., Rickaby, R. E. M., Brown, C. W., (2014). Poleward expansion of the coccolithophore Emiliania huxleyi. Journal of Plankton Research, 36 (2), 316-325.
Young, J.R., Bown, P.R., (1997). Proposals for a revised classification system for calcareous nannoplankton. Nannoplankton Research, 19/1.
http://www. International Calcareous Nannoplankton Association (INA website) .