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Journal articles on the topic 'South-east coast'

Author: Grafiati

Published: 4 June 2021

Last updated: 19 February 2022

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1

Leliaert, F. Coppejans. "The marine species of Cladophora (Chlorophyta) from the South African East Coast." Nova Hedwigia 76, no. 1-2 (February 1, 2003): 45–82. http://dx.doi.org/10.1127/0029-5035/2003/0076-0045.

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2

Chakraborty, Rekha Devi, P. Purushothaman P. Purushothaman, G. Kuberan G. Kuberan, Jomon Sebastian, and G. Maheswarudu G. Maheswarudu. "Identification of Oplophorus Gracilirostris from South-East and South-West Coast of India using Mitochondrial Genetic Marker." International Journal of Scientific Research 3, no. 6 (June 1, 2012): 167–69. http://dx.doi.org/10.15373/22778179/june2014/57.

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3

Wood, Aidan D. "The description of Austroglossus pectoralis (Teleostei: Soleidae) larvae from the South-east coast of South Africa." Scientia Marina 64, no. 4 (December 30, 2000): 387–92. http://dx.doi.org/10.3989/scimar.2000.64n4387.

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4

Chakraborty, Kajal, and Deepu Joseph. "Inter-annual and seasonal dynamics of amino acid, mineral and vitamin composition of silver belly Leiognathus splendens." Journal of the Marine Biological Association of the United Kingdom 95, no. 4 (September 3, 2014): 817–28. http://dx.doi.org/10.1017/s0025315414001155.

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Silver bellies, Leiognathus splendens were studied for their spatial (south-west and south-east coasts of India), annual (2008–2011) and seasonal (pre-monsoon, monsoon and post-monsoon) variations of protein, amino acids, vitamins and minerals. The monthly mean Sea Viewing Wide Field-of-view Sensor data for the period from January 2008 to December 2011 were taken into account to indicate the distribution of the photosynthetic pigment chlorophyll-a to test the hypothesis that surface productivity might be related to nutritional biochemistry of this species. The four year average total protein content and chlorophyll-a showed good correlation during monsoon on the south-west coast and monsoon/post-monsoon on the south-east coast, suggesting that the protein content is prejudiced by the chlorophyll-a concentration. Amino acid scores observed monsoon maxima along the south-west and south-east coasts. Significant seasonal variations in vitamin content were observed at the study locations with high content of vitamins D3, E, K1 and C on the south-west coast. Na content was maximal during pre-monsoon on the south-west coast, while post-monsoon maxima of Ca and K content were observed. The Fe, Mn and Zn were abundant in the samples collected from the south-west coast. The concentration of Se exhibited maximum values post-monsoon along the south-west and south-east coasts. The present study demonstrated L. splendens as a valuable source of the protein, amino acids, minerals and vitamins, showing that this low-value species is a good source of well balanced proteins with high biological value to be qualified as a preferred healthy food for human consumption.

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5

de Villiers, Michael. "Roll cloud on the South African east coast." Weather 66, no. 2 (January 25, 2011): 37–39. http://dx.doi.org/10.1002/wea.664.

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6

SAMAAI, TOUFIEK, RUWEN PILLAY, and LIESL JANSON. "Shallow-water Demospongiae (Porifera) from Sodwana Bay, iSimangaliso Wetland Park, South Africa." Zootaxa 4587, no. 1 (April 23, 2019): 1. http://dx.doi.org/10.11646/zootaxa.4587.1.1.

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33 species of shallow-water Demospongiae (Phylum Porifera) are described from Sodwana Bay, iSimangaliso Wetland Park, on the east coast of South Africa. Of the 33 species collected, 18 are redescribed from fresh material and 15 are new to science. Orders Clionaida, Poecilosclerida, Axinellida, Haplosclerida and Dictyoceratida are well represented in the collection with 4 to 6 species each, with the first three groups appearing to have the greatest diversity on the east coast of South Africa. The east coast of South Africa appears to have a high abundance of poecilosclerid and dictyoceratid sponges. The results of this study underscore the importance of poecilosclerid and dictyoceratid sponge fauna of the east coast of South Africa, in terms of the potential for the continued discovery of new species.

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7

Glen, H. F., and R. Boon. "Identifying trees on the East Coast of South Africa." South African Journal of Botany 75, no. 2 (April 2009): 402. http://dx.doi.org/10.1016/j.sajb.2009.02.053.

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8

Thibault-Botha, D., and MJ Gibbons. "Epipelagic siphonophores off the east coast of South Africa." African Journal of Marine Science 27, no. 1 (January 2005): 129–39. http://dx.doi.org/10.2989/18142320509504073.

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9

Sundar, V. "Wave characteristics off the South East Coast of India." Ocean Engineering 13, no. 4 (January 1986): 327–38. http://dx.doi.org/10.1016/0029-8018(86)90009-0.

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10

Kim, Jungsook, and Byung Chul Chun. "Effect of Seawater Temperature Increase on the Occurrence of Coastal Vibrio vulnificus Cases: Korean National Surveillance Data from 2003 to 2016." International Journal of Environmental Research and Public Health 18, no. 9 (April 22, 2021): 4439. http://dx.doi.org/10.3390/ijerph18094439.

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The purpose of this study was to assess the association between seawater temperature and Vibrio vulnificus cases in coastal regions of Korea. All V. vulnificus cases in coastal regions notified to the Korea Disease Control and Prevention Agency between 2003 and 2016 were included in this work. Data for seawater temperature on the south, west, and east coast during the study period were provided by the Korea Oceanographic Data Center of the National Institute of Fisheries Science. We used a generalized additive model and performed a negative binomial regression analysis. In total, 383 notified cases were analyzed (west coast: 196 cases, south coast: 162, and east coast: 25). The maximum seawater temperature was the most significant predictor of V. vulnificus cases on the south and east coasts (relative risk according to the 1 °C increase in seawater temperature (RR) = 1.35 (95% confidence interval (CI): 1.19–1.53) and 1.30 (95% CI: 1.06–1.59), respectively). However, the mean seawater temperature was the most significant predictor for the west coast (RR = 1.34 (95% CI: 1.20–1.51)). These results indicate that continuously monitoring seawater temperature increase in each coastal area is crucial to prevent V. vulnificus infections and protect high-risk groups, such as persons with liver disease.

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11

Tilney, R. L., and T. Hecht. "Early ontogeny of Galeichthys feliceps from the south east coast of South Africa." Journal of Fish Biology 43, no. 2 (August 1993): 183–212. http://dx.doi.org/10.1111/j.1095-8649.1993.tb00422.x.

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12

Dubula, O., and T. A. Lasiak. "Spatial Variability in the MudprawnUpogebia Africanaon the South-east Coast of South Africa." African Journal of Marine Science 25, no. 1 (June 2003): 275–82. http://dx.doi.org/10.2989/18142320309504016.

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13

HADFIELD, KERRY A., NICO J. SMIT, and ANNEMARIÉ AVENANT-OLDEWAGE. "Gnathia pilosus sp. nov. (Crustacea, Isopoda, Gnathiidae) from the East Coast of South Africa." Zootaxa 1894, no. 1 (October 8, 2008): 23–41. http://dx.doi.org/10.11646/zootaxa.1894.1.2.

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The larvae of gnathiid isopods are known to parasitise a large variety of intertidal fish worldwide. In South Africa, the larvae of Gnathia africana Barnard, 1914, have been recorded from various intertidal fish hosts along the cold West and South Coasts. The warmer East Coast, however, has not previously been sampled for gnathiids. From March 2006 to February 2007, intertidal fishes were collected on the East Coast using hand held nets and kept in aerated tanks until the gnathiids completed their feeding. Once fed, the gnathiids were kept alive in 50 ml bottles with fresh sea water till moulting occurred. Results indicated that all the East Coast intertidal gnathiids were from the same species and new to science, and subsequently described as Gnathia pilosus sp. nov. The G. pilosus male and female can be clearly distinguished from other South African species in having numerous tubercles and setae covering the cephalosome and pereon which are not as pronounced in the other species. The G. pilosus larva can also be distinguished from the other South African species by the triangular-shaped cephalosome and numerous sensory pits covering the body.

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14

Schumann, E. H. "THE COASTAL OCEAN OFF THE EAST COAST OF SOUTH AFRICA." Transactions of the Royal Society of South Africa 46, no. 3 (January 1987): 215–29. http://dx.doi.org/10.1080/00359198709520125.

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15

Behera, Pralaya Ranjan, S. S. Raju, M. A. Jishnudev, Shubhadeep Ghosh, and Raju Saravanan. "Emerging jellyfish fisheries along Central South East coast of India." Ocean & Coastal Management 191 (June 2020): 105183. http://dx.doi.org/10.1016/j.ocecoaman.2020.105183.

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16

Rudner, Jalmar, and A. R. Willcox. "Shipwreck and Survival on the South-East Coast of Africa." South African Archaeological Bulletin 40, no. 142 (December 1985): 119. http://dx.doi.org/10.2307/3888470.

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17

Sundar, V. "Wave-power potential off the South-East coast of India." Energy 12, no. 2 (February 1987): 171–75. http://dx.doi.org/10.1016/0360-5442(87)90122-8.

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18

Pandian, P. Kasinatha, S. Ramesh, M. V. Ramana Murthy, S. Ramachandran, and S. Thayumanavan. "Shoreline Changes and Near Shore Processes Along Ennore Coast, East Coast of South India." Journal of Coastal Research 203 (July 2004): 828–45. http://dx.doi.org/10.2112/1551-5036(2004)20[828:scansp]2.0.co;2.

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19

Steyn, E., PJ Fielding, and MH Schleyer. "The artisanal fishery for East Coast rock lobstersPanulirus homarusalong the Wild Coast, South Africa." African Journal of Marine Science 30, no. 3 (December 2008): 497–506. http://dx.doi.org/10.2989/ajms.2008.30.3.5.639.

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20

McSweeney, S. L. "Temporal and spatial variability of the open coast wave climate of Victoria, Australia." Marine and Freshwater Research 71, no. 3 (2020): 394. http://dx.doi.org/10.1071/mf18489.

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The open coast of Victoria, Australia, is one of the highest wave energy coastlines globally. Despite this, a lack of permanently deployed wave buoys has limited prior analysis of wave conditions. In this study, the wave climate of Victoria was analysed using 31 years of directional data hindcast from the National Oceanic and Atmospheric Administration’s WaveWatch-III model (Climate Forecast System Reanalysis hindcasts). An eastward decrease in wave height and period occurs from Portland to Wilson’s Promontory. This trend then reverses on the east coast. Across the west and central coasts, wave direction is dominated by south-west swells as influenced by strong westerly winds and mid-latitude low-pressure systems. On the east coast, wave direction becomes more variable, with added southerly, south-east and easterly components. The Southern Annular Mode influences wave climate variability on the west coast and is negatively correlated with storm frequency and wave direction. On the east coast, the El Niño–Southern Oscillation showed a strong positive correlation with wave height and a negative correlation with direction. This work provides a benchmark to compare to future changes. It will inform a higher-resolution analysis of the spatial correlation of wave conditions with climate processes to predict shoreline response.

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21

Jakobsdóttir, S. S., and H. C. Larsen. "Gravity survey on ice offshore South-East Greenland." Rapport Grønlands Geologiske Undersøgelse 135 (December 31, 1987): 69–72. http://dx.doi.org/10.34194/rapggu.v135.8001.

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In the early spring an effort was made to extend some lines of marine gravity data from the shelf into the coast north of Ammassalik. A net of marine gravity data covers the shelf off East Greenland, reaching from about 59°N to 74°N (fig. 1). South of Scoresby Sund the gravity data are mostly coIlected in regions floored by oceanic crust, though some of the lines cross the ocean-to-continent boundary. Between Ammassalik and Scoresby Sund the oceanto-continent transition zone (OCT) runs dose to the coast (Larsen, 1984), and is probably related to the onshore Tertiary basaltic dyke swarm described by Wager & Deer (1938) and Myers (1980) (fig. 2). An offshore continuation of the dyke swarm was proposed by Larsen (1978). The aim of the gravity project was to obtain three tie-lines connecting the offshore marine gravity data to onshore gravity data to be obtained by the Geodetic Institute during the summer of 1986 (fig. 1). Such tie-lines would provide crucial information on the gravity field over the dyke swarm and might aid in a more precise location ofthe initial line of rifting in this region. The survey area is covered with ice most of the year. Gravity surveys on ice have been carried out both in the Bothnian Bay (Lehmuskoski & Makinen, 1978) and on ice-islands in the polar pack ice (Crary et al., 1952; Kristoffersen, 1982). Thus a helicopter survey with portable gravimeter and readings on the ice was planned for the South-East Greenland survey as this would provide gravity data from the area ofinterest at lowest cost. The ice cover off East Greenland is usually most extensive in April (Larsen, 1985) and the field operation was therefore scheduled for that month.

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22

Hiller, Norton. "The environment, biogeography, and origin of the southern African Recent brachiopod fauna." Journal of Paleontology 68, no. 4 (July 1994): 776–86. http://dx.doi.org/10.1017/s0022336000026214.

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The brachiopod fauna that presently lives in the seas off the coasts of Namibia, South Africa, and southern Moçambique comprises 35 named plus seven unnamed species belonging to 26 genera, making it one of the most diverse in the world. Within the fauna are some species that are confined to the warm waters of the east coast, some that are restricted to the cold west coast waters, and others that enjoy a more widespread distribution. The geographic distribution of species is believed to be controlled by the two major oceanographic systems operating off southern Africa, namely, the Agulhas Current on the east and the Benguela Upwelling System on the west.Among the species that live off the west and south coasts are many that appear to have evolved in situ during times of pronounced environmental stress since the late Miocene. The fauna living off the east coast shows strong similarity with others in the Indian Ocean and it is inferred that many of the species migrated into the South African region by way of the ocean current systems that were established by the mid-Pliocene.Descriptions of Xenobrochus naudei and the previously undescribed Argyrotheca sp. and Amphithyris cf. A. richardsonae are provided.

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23

Kelley, D. F. "Age determination in bass and assessment of growth and year-class strength." Journal of the Marine Biological Association of the United Kingdom 68, no. 1 (February 1988): 179–214. http://dx.doi.org/10.1017/s0025315400050177.

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Scale readings from 6269 bass caught in 1946–86 on various parts of the U.K. coast, with a few from the Channel Islands and France, have been analysed to determine U.K. growth patterns and assess the relative abundance of successive year-classes. In the U.K. growth was fastest on the south-east coast, slowest on the west coast. In the Channel Islands growth was initially slower than on the south-east coast but faster after maturity; though less fast than on the Biscay coast of France. Year-classes of exceptional abundance tended to grow more slowly than classes of normal abundance. There was evidence in each region of a slight long-term fall in growth rate. Best growth occurred in warm summers. The growth period commenced, and annulus formed, at dates ranging from early May for the youngest juveniles to mid July for adults; terminating in each case in October. Males grew rather more slowly than females and appeared less long-lived and less hardy, except on the south-east coast, where, exceptionally, samples were caught well offshore and included large, generally faster growing fish; this suggests a behavioural difference between the sexes rather than consistently slower growth in males. Explanations are offered for occasional fast growing fish, which occur mainly on the south-east coast and mainly with particular year-classes, notably 1966 and 1969. Problems of interpretation are considered and solutions offered.

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24

Vijayanand, P., A. Murugan, K. Saravanaku, S. Ajmal Khan, and S. Rajagopal. "Assessment of Lobster Resources Along Kanyakumari (South East Coast of India)." Journal of Fisheries and Aquatic Science 2, no. 6 (October 15, 2007): 387–94. http://dx.doi.org/10.3923/jfas.2007.387.394.

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25

Cockcroft, V. G., A. C. De Kock, D. A. Lord, and G. J. B. Ross. "Organochlorines in bottlenose dolphinsTursiops truncatusfrom the east coast of South Africa." South African Journal of Marine Science 8, no. 1 (June 1989): 207–17. http://dx.doi.org/10.2989/02577618909504562.

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26

Livingstone, T.-C., JM Harris, AT Lombard, AJ Smit, and DS Schoeman. "Classification of marine bioregions on the east coast of South Africa." African Journal of Marine Science 40, no. 1 (January 2, 2018): 51–65. http://dx.doi.org/10.2989/1814232x.2018.1438316.

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27

Hanchet, Stuart. "Reproductive biology ofSqualus acanthiasfrom the east coast, South Island, New Zealand." New Zealand Journal of Marine and Freshwater Research 22, no. 4 (December 1988): 537–49. http://dx.doi.org/10.1080/00288330.1988.9516324.

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28

Vincent, Jean-Serge. "The Quaternary History of Banks Island, N.W.T., Canada." Géographie physique et Quaternaire 36, no. 1-2 (November 29, 2007): 209–32. http://dx.doi.org/10.7202/032478ar.

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ABSTRACT Banks Island is a polar desert where continental ice sheets, spreading from a dispersal centre to the southeast, reached their maximum extent on at least three occasions. The oldest Banks Glaciation affected all but the northwest. The Pre-Banks Sea preceded glacierization while the Post-Banks Sea formed during déglaciation. Following Morgan Bluffs Interglaciation, characterized by a climate similar to that of today, the south, the east, and the Thomsen River basin were covered during Thomsen Glaciation. The Pre-Thomsen Sea preceded the glacierization, while the Big Sea inundated much of the Island during déglaciation. Following the last or Cape Collinson Interglaciation, characterized by a climate warmer than that of the hypsithermal, Laurentide glacial lobes impinged on the coastal areas, during the M'Clure Stade of Amundsen Glaciation. Prince of Wales and Thesiger lobes, emanating from Amundsen Gulf, respectively advanced in Prince of Wales Strait and Thesiger Bay impinging on the east and southwest coasts. At the same time, Prince Alfred Lobe, originating in Viscount Melville Sound, advanced in M'Clure Strait and impinged on the north coast. The Pre-Amundsen Sea preceded the glacierization of the south coast, while the East Coast Sea submerged the east coast up to 120 m, the Meek Point Sea the west up to 20 m and the Investigator Sea the north up to 30 m, during déglaciation. The late Sand Hills Readvance of Thesiger Lobe built a morainic system on the southwest coast. Later, the northeast was covered, during the Russell Stade of Amundsen Glaciation, by Viscount Melville Lobe, emanating from Viscount Melville Sound, and the east coast was drowned up to 25 m by the Schuyter Point Sea. Limits of extent of Laurentide ice in the southwestern Archipelago are proposed for the two stades of the last or Wisconsinan Glaciation.

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29

Paranathala, W. E. "SUCCESS AND FAILURE OF COAST PROTECTION WORKS IN CEYLON." Coastal Engineering Proceedings 1, no. 6 (January 29, 2011): 47. http://dx.doi.org/10.9753/icce.v6.47.

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The Island of Ceylon, which is often referred to as the Pearl of the Indian Ocean, is 25,481 square miles in extent. It lies between 0 and 10 degrees North Latitude, and between 79 and 82 degrees East Longitude. The Island is mango-shaped. Its length from north to south is 272 miles, and its breadth from east to west is 140 miles. (Fig.1).

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30

Alappat, Linto, Palaniandy Seralathan, Anil Shukla, Kyth Thrivikramji, and Ashok Singhvi. "Chronology of red dune aggradations of South India and its Palaeo-environmental significance." Geochronometria 40, no. 4 (December 1, 2013): 274–82. http://dx.doi.org/10.2478/s13386-013-0118-5.

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Abstract Red sand dunes occur in the coastal plains of south east and west of Tamil Nadu, India between the coordinates of 8°00′ to 9°30′ N; 77°18′ to 79° 00′ E. OSL dating of these sands indicated aggradations between ∼16-9 ka and ∼9-3 ka in the west and east coasts respectively. Dating results from inland red dunes at the foothills of Western Ghats show a break in deposition at ∼6 ka and aggradation since ∼2 ka. The sand aggradations in the west coast occurred during the transition period when SW monsoon in the area was reestablishing. The dunes attained their stability by 9 ka. In the coastal region, the aggradations were controlled by sea level changes and a local recycling of earlier dunes (in the east coast). In the inland areas, the dune building was controlled by sand supply from fluvial sources.

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31

Goschen, WS, EH Schumann, KS Bernard, SE Bailey, and SHP Deyzel. "Upwelling and ocean structures off Algoa Bay and the south-east coast of South Africa." African Journal of Marine Science 34, no. 4 (December 2012): 525–36. http://dx.doi.org/10.2989/1814232x.2012.749810.

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32

Khan, Saeed, Hasley Vincent, and Brent Wilson. "The qualitative and quantitative classification of modern clastic marginal-marine depositional systems, Trinidad." Journal of Sedimentary Research 91, no. 7 (July 15, 2021): 710–34. http://dx.doi.org/10.2110/jsr.2020.119.

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ABSTRACT Trinidad's modern coastal depositional systems are for the first time documented by (traditional) descriptive and (modern) semiquantitative and quantitative classification methods. The processes controlling the morphology and distribution of these systems are also investigated. Google Earth™ satellite images, together with published basinal processes data (e.g., significant wave height, surface littoral currents, and tidal cyclicity) are used to describe system morphology, map depositional elements, and to determine the processes responsible for system distribution, respectively. Coastal depositional systems along Trinidad's east, south, and west coasts comprise deltas, estuaries, tidal-inlet complexes, strandplains, and tidal flats. Their distribution is controlled by the wave regime, although they are also influenced by tidal and fluvial processes. The wave regime changes from wave-dominated along the open east coast, to mixed-energy wave-dominated along the semi-sheltered south coast, and to mixed-energy tide-dominated along the sheltered west coast. Distribution of depositional systems related to this regime are such that the wave-dominated east coast sees the development of wave-dominated estuaries. The south coast has a series of wave-dominated, tide- and river-influenced deltas. The sheltered west coast is the most morphologically diverse with river- and wave-dominated deltas, strandplains, and tidal flats. The application of semiquantitative and quantitative classification methods on modern systems has showed their competence in classifying mixed-influence systems from their morphology and sedimentary record. Quantitative classification using depositional elements lends an appreciation to the morphological signatures of mixed-influence systems. Quantitative classification for sedimentary sections gives an appreciation of the preservation of mixed-influence physical processes. The combination of both allows the correlation of the impact of physical properties on morphology and sedimentary record (i.e., possible disparities between morphology and processes). The combination of semiquantitative and quantitative methods may also hold the key to unlocking the mixed-processes classification of depositional elements.

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33

Morgan, Jess A. T., Wayne D. Sumpton, Andrew T. Jones, Alexander B. Campbell, John Stewart, Paul Hamer, and Jennifer R. Ovenden. "Assessment of genetic structure among Australian east coast populations of snapper Chrysophrys auratus (Sparidae)." Marine and Freshwater Research 70, no. 7 (2019): 964. http://dx.doi.org/10.1071/mf18146.

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Snapper Chrysophrys auratus is a high-value food fish in Australia targeted by both commercial and recreational fisheries. Along the east coast of Australia, fisheries are managed under four state jurisdictions (Queensland, Qld; New South Wales, NSW; Victoria, Vic.; and Tasmania, Tas.), each applying different regulations, although it is thought that the fisheries target the same biological stock. An allozyme-based study in the mid-1990s identified a weak genetic disjunction north of Sydney (NSW) questioning the single-stock hypothesis. This study, focused on east-coast C. auratus, used nine microsatellite markers to assess the validity of the allozyme break and investigated whether genetic structure exists further south. Nine locations were sampled spanning four states and over 2000km, including sites north and south of the proposed allozyme disjunction. Analyses confirmed the presence of two distinct biological stocks along the east coast, with a region of genetic overlap around Eden in southern NSW, ~400km south of the allozyme disjunction. The findings indicate that C. auratus off Vic. and Tas. are distinct from those in Qld and NSW. For the purpose of stock assessment and management, the results indicate that Qld and NSW fisheries are targeting a single biological stock.A

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34

Heath, RA. "Large-scale influence of the New Zealand seafloor topography on western boundary currents of the South Pacific Ocean." Marine and Freshwater Research 36, no. 1 (1985): 1. http://dx.doi.org/10.1071/mf9850001.

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The extensive New Zealand submarine platform lying approximately 1600 km east of Australia has a strong influence on the South Pacific circulation. Together with the Kermadec Ridge, it is the western boundary of the deep South Pacific Ocean with an associated deep western boundary current. Although New Zealand probably influences where the East Australian Current separates from the east Australian coast, at the latitude of northernmost New Zealand, the sloping seafloor on the New Zealand west coast does allow for a meridional flow there. However, the decrease in current speed with depth does decrease the influence of the bottom topography. The net result is that there is both an intensification of the zonal flow across the Tasman Sea at the latitude of northernmost New Zealand, the speed of which is enhanced by the flow over the extensive ridge system, and a general eastwards flow in the Tasman Sea over the latitudinal range of New Zealand, which feeds meridional flows on the New Zealand west coast. It is suggested that the general west to east flow past New Zealand restricts the westward propagation of second- and higher-order baroclinic Rossby waves with the result that, whereas the East Australian Current has rapid near-surface flow which decreases rapidly with depth in the upper 500 m, the surface flow on the east coast of New Zealand is less rapid and decreases more uniformly with depth. One possible consequence of the current speed change with depth is that the flow and eddies on the New Zealand east coast appear to be influenced by the bathymetry whereas the East Australian Current eddies are more a primary component of the current linked to instability in the current system.

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35

Tenjing S, Yambem, and Narasimhaiah N. "Occurrence of Acrosterigma attenuatum (Mollusca: Bivalvia) along South East Coast of India." Journal of Terrestrial and Marine Research 3, no. 2 (April 30, 2019): 33–36. http://dx.doi.org/10.32610/jtmr.2019.v03i02.002.

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36

Czernyadjeva, I. V. "To the moss flora "Coast Chubuka" Reserve (South Kamchatka Peninsula, Far East)." Novosti sistematiki nizshikh rastenii 44 (2010): 357–72. http://dx.doi.org/10.31111/nsnr/2010.44.357.

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The mosses of "Coast Chubuka Reserve" (South Kamchatka, Far East) were studied. Moss flora of reserve includes 141 species, 1 subspecies and 1 variety. 3 taxa — new for Kamchatka Peninsula. Annotated check-list includes species frequency, ecology and phytocoenology. The short analysis of moss flora is provided.

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37

Milmann, Lucas, Salvatore Siciliano, Igor Morais, Andrea Sebastiano Tribulato, Rodrigo Machado, Alexandre N. Zerbini, Julio E. Baumgarten, and Paulo Henrique Ott. "A review of Balaenoptera strandings along the east coast of South America." Regional Studies in Marine Science 37 (May 2020): 101343. http://dx.doi.org/10.1016/j.rsma.2020.101343.

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Wynne, Michael J. "Microcladia exsertasp. nov. (Ceramiaceae, Rhodophyta) from the East coast of South Africa." British Phycological Journal 20, no. 3 (September 1985): 193–200. http://dx.doi.org/10.1080/00071618500650201.

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McGrath, R. J., and D. Bass. "Seed Dispersal by Emus on the New South Wales North-east Coast." Emu - Austral Ornithology 99, no. 4 (December 1999): 248–52. http://dx.doi.org/10.1071/mu99030.

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Kollimalai, Sakthivel, and Antony Fernando S. "Echinoderm diversity in Mudasal Odai and Nagapattinam coast of south east India." International Journal of Biodiversity and Conservation 6, no. 1 (January 31, 2014): 1–7. http://dx.doi.org/10.5897/ijbc2013.0619.

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41

Soundarapa, P., N. John Samue, S. Ravichandr, and T. Kannupandi. "Biodiversity of Crabs in Pichavaram Mangrove Environment, South East Coast of India." International Journal of Zoological Research 4, no. 2 (March 15, 2008): 113–18. http://dx.doi.org/10.3923/ijzr.2008.113.118.

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42

Thomson, Danielle, William Maher, and Simon Foster. "Arsenic and selected elements in marine angiosperms, south-east coast, NSW, Australia." Applied Organometallic Chemistry 21, no. 6 (2007): 381–95. http://dx.doi.org/10.1002/aoc.1229.

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43

Abramov, R. V., O. A. Guschin, S. Ye Navrotskaya, and Zh I. Stont. "HYDROMETEOROLOGICAL MONITORING AT THE SOUTH-EAST BALTIC SEA COAST IN 1996–2010." Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya., no. 1 (July 14, 2015): 54. http://dx.doi.org/10.15356/0373-2444-2013-1-54-61.

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Sundararajan, M., and Usha Natesan. "Geochemistry of core sediments from Mullipallam creek, South East coast of India." Environmental Earth Sciences 61, no. 5 (January 13, 2010): 947–61. http://dx.doi.org/10.1007/s12665-009-0414-9.

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Natesan, Usha, P. R. Rajalakshmi, M. V. Ramana Murthy, and Vincent A. Ferrer. "Nearshore Wave Climate and Sediment Dynamics along South East Coast of India." Journal of the Indian Society of Remote Sensing 43, no. 2 (October 17, 2014): 415–27. http://dx.doi.org/10.1007/s12524-014-0407-3.

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46

Ganesan, M., S. Thiruppathi, and Bhavanath Jha. "Mariculture of Hypnea musciformis (Wulfen) Lamouroux in South east coast of India." Aquaculture 256, no. 1-4 (June 2006): 201–11. http://dx.doi.org/10.1016/j.aquaculture.2006.01.039.

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47

Vos, A. de, C. B. Pattiaratchi, and E. M. S. Wijeratne. "Surface circulation and upwelling patterns around Sri Lanka." Biogeosciences Discussions 10, no. 9 (September 11, 2013): 14953–98. http://dx.doi.org/10.5194/bgd-10-14953-2013.

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Abstract. Sri Lanka occupies a unique location within the equatorial belt in the northern Indian Ocean with the Arabian Sea on its western side and the Bay of Bengal on its eastern side. The region is characterised by bi-annually reversing monsoon winds resulting from seasonal differential heating and cooling of the continental land mass and the ocean. This study explored elements of the dynamics of the surface circulation and coastal upwelling in the waters around Sri Lanka using satellite imagery and the Regional Ocean Modelling System (ROMS) configured to the study region and forced with ECMWF interim data. The model was run for 2 yr to examine the seasonal and shorter term (∼10 days) variability. The results confirmed the presence of the reversing current system in response to the changing wind field: the eastward flowing Southwest Monsoon Current (SMC) during the Southwest (SW) monsoon transporting 11.5 Sv and the westward flowing Northeast Monsoon Current (NMC) transporting 9.5 Sv during the Northeast (NE) monsoon, respectively. A recirculation feature located to the east of Sri Lanka during the SW monsoon, the Sri Lanka Dome, is shown to result from the interaction between the SMC and the Island of Sri Lanka. Along the eastern and western coasts, during both monsoon periods, flow is southward converging along the south coast. During the SW monsoon the Island deflects the eastward flowing SMC southward whilst along the east coast the southward flow results from the Sri Lanka Dome recirculation. The major upwelling region, during both monsoon periods, is located along the south coast and is shown to be due to flow convergence and divergence associated with offshore transport of water. Higher surface chlorophyll concentrations were observed during the SW monsoon. The location of the flow convergence and hence the upwelling centre was dependent on the relative strengths of wind driven flow along the east and west coasts: during the SW (NE) monsoon the flow along the western (eastern) coast was stronger and hence the upwelling centre was shifted to the east (west). The presence of upwelling along the south coast during both monsoon periods may explain the blue whale (Balaenoptera musculus) aggregations in this region.

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Simon, C. A., T. M. Worsfold, L. Lange, and J. Sterley. "The genus Boccardia (Polychaeta: Spionidae) associated with mollusc shells on the south coast of South Africa." Journal of the Marine Biological Association of the United Kingdom 90, no. 3 (August 14, 2009): 585–98. http://dx.doi.org/10.1017/s0025315409990452.

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Three species of Boccardia (B. polybranchia, B. pseudonatrix and B. proboscidea) were associated with mollusc shells on the south and south-east coasts of South Africa. Boccardia polybranchia was widely distributed along the coast and falls within the known distribution range of this species. Comparisons with material from other, international, locations showed that some specimens have been misidentified. No characters could be found to characterize distinct species for different regions within the range of B. polybranchia, as currently recognized. Boccardia pseudonatrix was found only at the most eastern site, increasing its known distribution range. Boccardia proboscidea, a non-indigenous species, was found only on abalone farms and was most abundant in the west.

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Payne, A. I. L. "Growth and stock differentiation of kingklip(Genypterus capensis)on the south-east coast of South Africa." South African Journal of Zoology 20, no. 2 (January 1985): 49–56. http://dx.doi.org/10.1080/02541858.1985.11447913.

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Simon, Carol A. "Pseudopolydora species associated with mollusc shells on the south coast of South Africa, with the description of Ps. dayii, sp nov." Journal of the Marine Biological Association of the United Kingdom 89, no. 4 (May 15, 2009): 681–87. http://dx.doi.org/10.1017/s0025315409000034.

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Two species of the genus Pseudopolydora, Ps. dayii, sp. nov. and Ps. antennata, were associated with gastropods on the south and south-east coasts of South Africa. Pseudopolydora dayii is characterized by prominent post-chaetal notopodial lobes on chaetiger 1 with very long chaetae, a prominent occipital tentacle, having hooded hooks that start on chaetiger 9, branchiae that start on chaetiger 6, stout hooks and lobes placed latero-posteriorly to the hooded hooks in posterior chaetigers. It is a surface-fouler and was found on several species of wild gastropods at four of the five sites sampled and from additional material from the south-west coast and on cultured abalone (Haliotis midae) at a farm on the south-west coast. Three individuals of Ps. antennata were found only with oysters at the easternmost site. This was the first record of this species outside of the Western Cape Province and it is possible that their association with the oysters was fortuitous.

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