Artykuły w czasopismach: „Banks Peninsula”

1

Garnock-Jones, PJ. "Plant life on Banks Peninsula". New Zealand Journal of Botany 52, nr 3 (3.07.2014): 386–87. http://dx.doi.org/10.1080/0028825x.2014.885454.

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Slooten, Elisabeth, William Rayment i Steve Dawson. "Offshore distribution of Hector's dolphins at Banks Peninsula, New Zealand: Is the Banks Peninsula Marine Mammal sanctuary large enough?" New Zealand Journal of Marine and Freshwater Research 40, nr 2 (czerwiec 2006): 333–43. http://dx.doi.org/10.1080/00288330.2006.9517425.

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Boren, L. J., C. G. Muller i N. J. Gemmell. "Colony growth and pup condition of the New Zealand fur seal (Arctocephalus forsteri) on the Kaikoura coastline compared with other east coast colonies". Wildlife Research 33, nr 6 (2006): 497. http://dx.doi.org/10.1071/wr05092.

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Abstract.Since its near extermination by sealing, the New Zealand fur seal (Arctocephalus forsteri) has been recolonising areas of its former range throughout New Zealand and Australia. This study examined fur seal population growth over four breeding seasons spanning 2002–05 at the Ohau Point and Lynch’s Reef colonies in Kaikoura and the Horseshoe Bay and Te Oka Bay colonies on Banks Peninsula, on the east coast of New Zealand. Estimates of pup numbers were made using mark–recapture techniques and condition indices were used to assess the body condition of pups in each colony. We found that the Ohau Point and Te Oka Bay colonies are growing exponentially (32% and 47% per annum respectively), reaching nearly 600 pups at Ohau Point and 300 pups at Te Oka Bay, whereas Horseshoe Bay appears stable. Pups born at Ohau Point are consistently heavier and in better condition than their Banks Peninsula counterparts despite the faster rate of growth observed at Te Oka Bay. An El Niño event in 2003 coincided with a drop in mass and condition at the Banks Peninsula colonies, but not at the Kaikoura colony. This discrepancy between colonies in response to environmental conditions suggests that colony-specific variables at Kaikoura may provide more favourable conditions for rearing pups than on Banks Peninsula.

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Khalil-Oliwa, Oliwia. "Review of Risks and Risk Management Systems in the Largest Islamic Banks of the Arabian Peninsula". Annales Universitatis Mariae Curie-Skłodowska, sectio H – Oeconomia 55, nr 1 (11.05.2021): 19. http://dx.doi.org/10.17951/h.2021.55.1.19-29.

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Theoretical background: The specificity of Islamic principles, on the basis of which Islamic banking was created, as well as the nature of its financial instruments, means that Islamic banks may be exposed to greater risks than conventional banks.Purpose of the article: The aim of the article is to define key risks identified by Islamic banks and to define risk management systems in the 13 largest banks of the Arabian Peninsula region. The article analyses the annual reports submitted by the supervisory boards of the largest Islamic banks of the Arabian Peninsula for 2018, so that common elements in their risk management processes can be found.Research methods: Analyses of annual reports of the banks of the Arabian Peninsula region.Main findings: Supervisory boards of Islamic banks identify risks and implement strategies and risk management structures. The most important risks identified by banks are credit risk, liquidity risk, reputational risk, as well as operational risk, understood as the risk of direct or indirect loss, resulting from inadequate or faulty internal processes, errors of employees or systems and external events. Islamic banks may be exposed to increased credit risk, due to the application of the principle of profit and loss sharing (PLS), which is one of the pillars of Islamic finance. An analysis of the fiancial reports of the largest Islamic banks of the Arabian Peninsula shows that all supervisory boards are aware of the importance and role of an effective risk management system in reducing costs and increasing banks’ results. Most of them use the principles described by the Islamic Financial Services Board (IFSB). All banks have implemented appropriate risk management processes and policies, and have units in their structures responsible for the risk management process, which means that they apply the first IFSB principle. The institutions declare that they identify and monitor risks, and implement risk mitigation measures.

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Pharo, Emma, i Bryony H. Macmillan. "Checklist of the Mosses of Banks Peninsula, New Zealand". Bryologist 101, nr 2 (1998): 352. http://dx.doi.org/10.2307/3244213.

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Reynolds‐Fleming, Janelle V., i Jason G. Fleming. "Coastal circulation within the Banks Peninsula region, New Zealand". New Zealand Journal of Marine and Freshwater Research 39, nr 1 (marzec 2005): 217–25. http://dx.doi.org/10.1080/00288330.2005.9517301.

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Perrie, Leon R., Patrick J. Brownsey i John D. Lovis. "Tmesipteris horomaka, a new octoploid species from Banks Peninsula". New Zealand Journal of Botany 48, nr 1 (marzec 2010): 15–29. http://dx.doi.org/10.1080/00288251003640010.

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8

Wilson, Hugh D. "Regeneration of native forest on Hinewai Reserve, Banks Peninsula". New Zealand Journal of Botany 32, nr 3 (lipiec 1994): 373–83. http://dx.doi.org/10.1080/0028825x.1994.10410480.

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9

Griffin, Sammy, Travis W. Horton i Christopher Oze. "Origin of warm springs in Banks Peninsula, New Zealand". Applied Geochemistry 86 (listopad 2017): 1–12. http://dx.doi.org/10.1016/j.apgeochem.2017.09.013.

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10

Cameron, Claire, Richard Barker, David Fletcher, Elisabeth Slooten i Stephen Dawson. "Modelling Survival of Hector's Dolphins around Banks Peninsula, New Zealand". Journal of Agricultural, Biological, and Environmental Statistics 4, nr 2 (czerwiec 1999): 126. http://dx.doi.org/10.2307/1400593.

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11

Clark, John M. "A new hypertrichous larvalErythrites(Erythraeinae) from Banks Peninsula, New Zealand". International Journal of Acarology 39, nr 5 (31.07.2013): 393–99. http://dx.doi.org/10.1080/01647954.2013.804119.

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12

Hodge, S., i J. W. Early. "Hymenoptera associated with marine strandlines at Christchurch and Banks Peninsula". New Zealand Entomologist 39, nr 2 (2.07.2016): 117–28. http://dx.doi.org/10.1080/00779962.2016.1215034.

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13

Zhao, Ye, i Rongquan Li. "14C dating of moss peat banks in Fildes Peninsula, Antarctica". Chinese Science Bulletin 44, nr 19 (październik 1999): 1817–19. http://dx.doi.org/10.1007/bf02886168.

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14

Cooper, Elisabeth J. "Reindeer grazing reduces seed and propagule bank in the High Arctic". Canadian Journal of Botany 84, nr 11 (listopad 2006): 1740–52. http://dx.doi.org/10.1139/b06-127.

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It is commonly assumed that plant establishment in the High Arctic is limited by severe abiotic conditions and by a paucity of propagules and seeds. Heavy reindeer grazing may reduce plant allocation to reproduction and removes significant proportions of flowers and seeds, thus reducing contributions to seed rain and seed bank. In contrast, foraging and trampling may break up existing mature plants, increasing the vegetative propagules in the soil. To determine the effect of grazing on colonization potential in the High Arctic, two studies were carried out: (i) a comparison of seed bank inside and outside three long-term reindeer ( Rangifer tarandus platyrhnchus (Vrolic)) exclosures and (ii) an investigation of the germinable seed and propagule bank of two neighbouring peninsulas with contrasting reindeer grazing history in northwestern Svalbard (79°N, 12°E). Seed banks inside reindeer exclosures germinated significantly more seedlings (596 seedlings·m–2) than those outside (263 seedlings·m–2). Species composition and total plant cover was similar on both peninsulas, but forage-plant cover was lower on the heavily grazed peninsula (Brøggerhalvøya) than on the adjacent lightly grazed peninsula (Sarsøyra). Brøggerhalvøya had significantly lower species richness and density of seed and propagule bank (0.21 ± 0.02 germinating species per sample, 0.15 ± 0.02 propagule species per sample, 416 ± 103 seedlings·m–2, 283 ± 78 propagules·m–2) than did Sarsøyra (0.44 ± 0.40 germinating species per sample, 0.35 ± 0.03 propagule species per sample,1016 ± 188 seedlings·m–2, 782 ± 238 propagules·m–2). These results imply that reindeer depleted both the seed and the propagule banks, thus reducing the potential for colonization of disturbed areas. Grazing may, therefore, have a lasting impact on High Arctic plant communities.

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15

Sewell, R. J. "Late Miocene volcanic stratigraphy of central Banks Peninsula, Canterbury, New Zealand". New Zealand Journal of Geology and Geophysics 31, nr 1 (styczeń 1988): 41–64. http://dx.doi.org/10.1080/00288306.1988.10417809.

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16

Stephenson, Wayne, i James Shulmeister. "A Holocene progradation record from Okains Bay, Banks Peninsula, Canterbury, New Zealand". New Zealand Journal of Geology and Geophysics 42, nr 1 (1.03.1999): 11–19. http://dx.doi.org/10.1080/00288306.1999.9514828.

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17

Brennan, Stephen O., Andrew P. Fellowes i Peter M. George. "Albumin Banks Peninsula: a new termination variant characterised by electrospray mass spectrometry". Biochimica et Biophysica Acta (BBA) - Protein Structure and Molecular Enzymology 1433, nr 1-2 (sierpień 1999): 321–26. http://dx.doi.org/10.1016/s0167-4838(99)00131-4.

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18

Gormley, Andrew M., Stephen M. Dawson, Stephen M. Dawson, Elisabeth Slooten i Stefan Brager. "CAPTURE-RECAPTURE ESTIMATES OF HECTOR'S DOLPHIN ABUNDANCE AT BANKS PENINSULA, NEW ZEALAND". Marine Mammal Science 21, nr 2 (kwiecień 2005): 204–16. http://dx.doi.org/10.1111/j.1748-7692.2005.tb01224.x.

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19

Gorton, Michael J., R. Bruce Chapman i Susan P. Worner. "Distribution and spread ofAdozyphmus couloni(Burmeister) (Coleoptera: Scarabaeidae) on Banks Peninsula, Canterbury". New Zealand Entomologist 21, nr 1 (styczeń 1998): 75–79. http://dx.doi.org/10.1080/00779962.1998.9722040.

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20

Soons, J. M., N. T. Moar, J. Shulmeister, H. D. Wilson i J. A. Carter. "Quaternary vegetation and climate changes on Banks Peninsula, South Island, New Zealand". Global and Planetary Change 33, nr 3-4 (lipiec 2002): 301–14. http://dx.doi.org/10.1016/s0921-8181(02)00084-x.

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21

Kolesnikov, Roman. "Ecological state of water bodies and their water protection zones within the boundaries of settlements of the Yamal Peninsula". E3S Web of Conferences 265 (2021): 02009. http://dx.doi.org/10.1051/e3sconf/202126502009.

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Most of the population of the Yamal Peninsula lives in settlements located on the banks of rivers. The increasing industrial development of the Yamal Peninsula leads to the fact that in these settlements in the water area and on the shores, objects of the fuel and energy complex are being built and functioning. At the same time, the contribution to water pollution of settlements located here, as well as objects of transport and fuel and energy infrastructure, is still unclear. On the other hand, the issues of intensifying the processes of coastal destruction and the related danger to residential and economic infrastructure are increasingly being discussed. However, the degree of activation of these processes on the Yamal Peninsula is also poorly understood. During the study, the state of water bodies and water protection zones was monitored for the period from 2016 to 2020. It was found that at present no significant anthropogenic pollution of water and bottom sediments is recorded. The content of pollutants and heavy metals is mainly determined by natural conditions. At the same time, the water protection zones are littered with scrap metal and household waste. Activation of channel processes and processes of abrasion and thermal abrasion of the banks is observed. The intensity of coastal destruction processes in the erosion zone varies from 0.25 to 0.85 m/year.

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22

Zimmermann, Klaus, Peter L. Turecek i Hans Peter Schwarz. "Determination of the Prevalence of Fibrinogen Banks Peninsula Mutation (γ280Tyr→Cys) by PCR". Pathophysiology of Haemostasis and Thrombosis 29, nr 4 (1999): 225–28. http://dx.doi.org/10.1159/000022506.

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23

Dominy, Michèle D. "Settler Postcolonial Ecologies and Native Species Regeneration on Banks Peninsula, Aotearoa New Zealand". Anthropological Forum 28, nr 1 (2.01.2018): 89–106. http://dx.doi.org/10.1080/00664677.2018.1431203.

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24

Hampton, S. J., i J. W. Cole. "Lyttelton Volcano, Banks Peninsula, New Zealand: Primary volcanic landforms and eruptive centre identification". Geomorphology 104, nr 3-4 (marzec 2009): 284–98. http://dx.doi.org/10.1016/j.geomorph.2008.09.005.

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25

Wood, Vaughan, i Eric Pawson. "The Banks Peninsula Forests and Akaroa Cocksfoot: Explaining a New Zealand Forest Transition". Environment and History 14, nr 4 (1.11.2008): 449–68. http://dx.doi.org/10.3197/096734008x368394.

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26

Neves, Maria Elisabete, Catarina Proença i António Dias. "Bank Profitability and Efficiency in Portugal and Spain: A Non-Linearity Approach". Journal of Risk and Financial Management 13, nr 11 (17.11.2020): 284. http://dx.doi.org/10.3390/jrfm13110284.

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This paper aims to analyze the determinants of profitability and bank efficiency in the Iberian Peninsula. To achieve the proposed objective, a sample of 66 Portuguese and Spanish banks was analyzed. To test the hypotheses formulated according to the proposed literature review, the panel data methodology was used; specifically, the Generalized Method of Moments (GMM) system model proposed by and the Tobit model. The results point out that the banking performance, measured in terms of profitability and efficiency, in the Iberian Peninsula, is influenced by internal management variables, but also by the macroeconomic environment. More interestingly, and new in the Iberian banking sector literature, the results prove a positive and negative non-linear relationship between bank size and their levels of profitability and efficiency, respectively.

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27

Partridge, T. R. "Soil seed banks of secondary vegetation on the Port Hills and Banks Peninsula, Canterbury, New Zealand, and their role in succession". New Zealand Journal of Botany 27, nr 3 (lipiec 1989): 421–35. http://dx.doi.org/10.1080/0028825x.1989.10414123.

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Gorton, M. J., R. B. Chapman i R. J. Townsend. "Australian black beetle Adoryophorus couloni (Burmeister) extends its range on Banks Peninsula". Proceedings of the New Zealand Plant Protection Conference 51 (1.08.1998): 267. http://dx.doi.org/10.30843/nzpp.1998.51.11701.

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29

Carpenter, Edward. "‘GRASS BANKS BETWEEN THE STORAGE TANKS’: 20TH-CENTURY INDUSTRY ON THE HOO PENINSULA, KENT". Industrial Archaeology Review 36, nr 1 (maj 2014): 15–23. http://dx.doi.org/10.1179/0309072814z.00000000026.

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30

Smith, Craig, David DeMaster, Carrie Thomas, Pavica Srsen, Laura Grange, Victor Evrard i Fabio DeLeo. "Pelagic-Benthic Coupling, Food Banks, and Climate Change on the West Antarctic Peninsula Shelf". Oceanography 25, nr 3 (1.09.2012): 188–201. http://dx.doi.org/10.5670/oceanog.2012.94.

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31

Sherwood, Graham J. "Paleomagnetism and magnetostratigraphy of Miocene volcanics in eastern Otago and Banks Peninsula, New Zealand". New Zealand Journal of Geology and Geophysics 31, nr 2 (kwiecień 1988): 207–24. http://dx.doi.org/10.1080/00288306.1988.10417770.

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32

Donnelly, Jai, James Goff i Catherine Chagué-Goff. "A record of local storms and trans-Pacific tsunamis, eastern Banks Peninsula, New Zealand". Holocene 27, nr 4 (20.09.2016): 496–508. http://dx.doi.org/10.1177/0959683616670222.

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This study of five sand units at Lavericks Bay, New Zealand, reports on the sedimentary evidence for three trans-Pacific tsunamis and two local storms. The 1868 Arica, 1877 Iquique and 1960 Valdivia tsunamis from Chile were the largest distantly generated events in New Zealand’s history but have never before been identified at the same location. It is also the first time that the 1877 Iquique tsunami deposit has been found in New Zealand. Two further sand units were identified as local storm deposits laid down in 1869/1870 and 1929. The identification and chronology of these events were established through the use of geochemistry, palynology, diatoms, charcoal abundance and historical documents. Their relative magnitudes were estimated through the use of grain size parameters and lateral extent of the recognisable sand layers. The recognisable sandy tsunami deposits extend about 60% of the inundation distance, while the storm sediments are finer and less extensive. There were two notable geochemical differences between the storm and tsunami deposits. Both storm deposits had lower concentrations of marine proxy elements associated with lower Ca–Ti and Sr–Ba ratios. Other differences were noted between some of the tsunami and storm deposits such as rip-up clasts and sediment characteristics, but these were by no means unequivocal. It is possible that geochemistry may prove to be the only proxy capable of not only differentiating effectively between storm and tsunami sediments but also identifying the maximum inland extent of a deposit and of inundation. It is the ability to better understand the nature and extent of such catastrophic events through these subtle differences in event characteristics that will help improve risk management for coastlines around the world.

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33

Timm, C., K. Hoernle, F. Hauff, Paul van den Bogaard i S. Weaver. "A mantle origin for the enriched signature in basalts from banks Peninsula, New Zealand". Geochimica et Cosmochimica Acta 70, nr 18 (sierpień 2006): A650. http://dx.doi.org/10.1016/j.gca.2006.06.1212.

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34

Ryan, Christine J., G. J. Hickling i Kerry-Jayne Wilson. "Breeding Habitat Preferences of the New Zealand Fur Seal (Arctocephalus forsteri) on Banks Peninsula". Wildlife Research 24, nr 2 (1997): 225. http://dx.doi.org/10.1071/wr95068.

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Colonies of New Zealand fur seals (Arctocephalus forsteri) on Banks Peninsula, New Zealand, were surveyed between March and August 1993 to compare breeding and non-breeding habitat features. Breeding habitat was characterised by large angular boulders, beaches that were steeper than those of non-breeding habitat, and numerous escape zones, crevices and ledges. Non-breeding habitat was less steep, had smaller rounder boulders and was less exposed to the sun. Multivariate analyses confirmed that overall habitat differences were statistically significant (P < 0·05). A linear discriminant function was calculated for the two habitat types. The resulting classification rule suggested that crevices, ledges and slope were particularly useful predictors of breeding status. The rule had 96% success in classifying the original sites as breeding or non-breeding and now requires validation by further field surveys in areas with different climate, geology and latitude. If establishment of breeding colonies at sites currently used only by non- breeding seals can be predicted from habitat features, this could provide useful information for managers of coastal sanctuaries.

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35

Hughey, K. F. D. "An evaluation of a management saga: The Banks Peninsula Marine Mammal Sanctuary, New Zealand". Journal of Environmental Management 58, nr 3 (marzec 2000): 179–97. http://dx.doi.org/10.1006/jema.1999.0309.

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Rolleston, W. B. R. "Conditions for co-existence of genetic modification in a pasture based system - a farmer perspective". Journal of New Zealand Grasslands 78 (1.01.2016): 83–88. http://dx.doi.org/10.33584/jnzg.2016.78.509.

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Blue Cliffs Station in South Canterbury was taken up by Henry Poingdestre in 1856, 5 years after my great-grandfather, George Rhodes and his brother Robert drove a flock of sheep from Banks Peninsula to The Levels Station to establish the first run in South Canterbury. It was from George that McKenzie famously stole 1000 sheep in 1855 and was caught in the now named Mackenzie Pass, only to escape again into the mist the same night.

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37

Sewell, R. J., B. J. Hobden i S. D. Weaver. "Mafic and ultramafic mantle and deep crustal xenoliths from Banks Peninsula, South Island, New Zealand". New Zealand Journal of Geology and Geophysics 36, nr 2 (czerwiec 1993): 223–31. http://dx.doi.org/10.1080/00288306.1993.9514570.

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38

Burrows, C. J. "Seed trapping in Ahuriri Summit Bush Scenic Reserve, Port Hills, western Banks Peninsula, 1985–1986". New Zealand Journal of Botany 32, nr 2 (kwiecień 1994): 183–215. http://dx.doi.org/10.1080/0028825x.1994.10410367.

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Montgomery, B. R., Dave Kelly i Jenny J. Ladley. "Pollinator limitation of seed set inFuchsia perscandens(Onagraceae) on Banks Peninsula, South Island, New Zealand". New Zealand Journal of Botany 39, nr 4 (grudzień 2001): 559–65. http://dx.doi.org/10.1080/0028825x.2001.9512759.

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Rayment, William, Steve Dawson, Elisabeth Slooten, Stefan Bräger, Sam Du Fresne i Trudi Webster. "Kernel density estimates of alongshore home range of Hector's dolphins at Banks Peninsula, New Zealand". Marine Mammal Science 25, nr 3 (lipiec 2009): 537–56. http://dx.doi.org/10.1111/j.1748-7692.2008.00271.x.

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King, L. H., G. B. Fader, W. H. Poole i R. K. Wanless. "Geological setting and age of the Flemish Cap granodiorite, east of the Grand Banks of Newfoundland". Canadian Journal of Earth Sciences 22, nr 9 (1.09.1985): 1286–98. http://dx.doi.org/10.1139/e85-133.

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Flemish Cap, a large isolated submarine knoll 600 km east of Newfoundland, consists of a central core of Hadrynian rocks and an onlapping sequence of undisturbed to disturbed Mesozoic–Cenozoic sediments. The central core of the cap, sampled with an electric rock-core drill, comprises pink, fine- to medium-grained granodiorite, dacite, and volcanic siltstone. The granodiorite samples, collected in six out of eight cores, are remarkably similar lithologically, despite a separation of up to 65 km, and probably represent a single pluton. The aphanitic dacite and laminated cherty volcanic siltstone have been metamorphosed to subgreenschist (prehnite) facies but show no evidence of contact metamorphism.U–Pb analyses of coarse and fine zircon fractions from a granodiorite core yielded upper intercepts of 751 and 833 Ma, respectively. Although not precise, these ages probably represent the age of intrusion sometime in the 750–830 Ma range and are older than those reported for similar Hadrynian granitic rocks of eastern Newfoundland. AK–Ar age of 657 ± 29 Ma on hornblende from the same core and a K–Ar age of 615 ± 20 Ma on biotite from a granodiorite core elsewhere in the body probably represent incomplete degassing during the superimposed subgreenschist metamorphism of uncertain age.Thus the Flemish Cap granodiorite and associated rocks are part of the Avalon Zone and may represent a much older part of the Avalon Terrane than parts toward the west on Avalon Peninsula and Burin Peninsula.

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Sixtus, C. R., R. R. Scott i G. D. Hill. "The phenology of Cydia succedana on gorse in Canterbury". New Zealand Plant Protection 60 (1.08.2007): 146–51. http://dx.doi.org/10.30843/nzpp.2007.60.4673.

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The phenology of Cydia succedana an introduced seedfeeder of Ulex europaeus was investigated Pheromone traps were set out at McLeans Island Christchurch a warm lowland site and Hinewai Reserve Banks Peninsula a cool upland site to observe the phenology of C succedana at two different altitudes and climatic conditions Moth populations were estimated by the mean number of male moths caught in the traps The phenology of C succedana was synchronised with the first U europaeus flowering in springsummer Significantly more male moths were captured at McLeans Island from October 2002 to February 2003

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Somnark, Rungnapa, i Narumon Sangpradub. "New records of the caddisflies Diplectrona erinya Malicky, 2002 and Diplectrona extrema Banks, 1920 (Trichoptera, Hydropsychidae) from Thailand". Check List 19, nr 1 (9.01.2023): 13–20. http://dx.doi.org/10.15560/19.1.13.

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The distributions of Diplectrona erinya Malicky, 2002 and Diplectrona extrema Banks, 1920 are somewhat limited. Diplectrona extrema has been known in some areas of the Indochina Peninsula archipelago and D. erinya only at the type locality in the north of Vietnam. We provide new records of these two species, which bring the number of Thai species of Diplectrona to 10. These two species were collected from a protected area in Thap Lan National Park. It is obvious that these two species occur at low densities and are probably rare in Thailand.

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Ponkratova, Irina Yu. "Middle Neolithic of the Kamchatka Peninsula". Vestnik NSU. Series: History and Philology 19, nr 5 (2020): 86–102. http://dx.doi.org/10.25205/1818-7919-2020-19-5-86-102.

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Purpose. The study of archaeological sites of the Middle Neolithic of Kamchatka should offer a chronology and a set of criteria for identifying the period. Results. The research data is based on the materials of the studied cultural layer, buried dwellings and individual artifacts of 46 archaeological sites. It has been established that the average Neolithic of Kamchatka can be dated back to 4 000–1 500 cal BP. The sites were found on high water-glacial terraces with a height of 4 to 30 meters on the banks of large rivers and lakes, the sea coast of the eastern part of the peninsula. Their number had increased compared to the previous period. Dwellings had become more complex. Perhaps this is due to the need to have more reliable shelters in the conditions of the marine climate and frequent precipitation of volcanic ash. The ground buildings, semi-underground dwellings and workshops for the manufacture of stone tools were found at the sites. Near the dwellings, special fortifications in the form of artificial ditches and ramparts made of stones and soil were also found. These may have been defensive structures. The increased population size, its settlement mainly along the coast in order to develop marine resources, may have caused conflicts between certain groups of the population in the struggle for the best fishing sites. The stone industry is represented by cores (amorphous and prismatic knife-shaped blades) and primary cleavage products (knife-shaped blades of different sizes without retouching, with edge retouching and on both sides). Among the tools there were retouched triangular stone arrowheads without stem and with stem, leaf-shaped, including miniature, arrowheads; knives – narrow and wide-bladed with a dedicated handle, leaf-shaped oval; roughly beaten and polished sharp-edged adzes of different sizes with a sub-triangular and oval cross-section; end scrapers of various geometric shapes; calibrators of arrow shafts. The strategy of life support of society was aimed at hunting for marine mammals, fishing and gathering, including shellfish. In the sphere of spiritual culture, signs of ceremonial activity (labrets) and art (small figurines and ornaments) have also been identified. Conclusion. It is assumed that with an increased population size and changes in the environmental situation, a new way of life of the population developed, associated with a highly specialized and complex appropriating economy which essentially formed its own archaeological culture (Taryinskaya culture).

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Sidorchuk, Aleksey. "The Potential of Gully Erosion on the Yamal Peninsula, West Siberia". Sustainability 12, nr 1 (28.12.2019): 260. http://dx.doi.org/10.3390/su12010260.

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The Yamal Peninsula occupies the northern part of the West Siberian Plain in Russia. This territory has rapidly developed due to the exploitation of several gas fields. At the same time, the Yamal Peninsula is one of the most severely gullied landscapes in the Arctic. The potential risk of damage to the environment or structures and the cost of such damages are very high there. The erosion potential is the cumulative erosion by runoff above critical, calculated for each point at a catchment. Calculations take into account the geomorphic, lithological, and vegetation cover thresholds, realized in the form of critical runoff depth of erosion initiation. It also takes into account action of all flows between the critical and maximum runoff. The calculations for several gullied catchments on the Yamal Peninsula show the uneven distribution of erosion potential level with the maximum of gully erosion on the steep banks of the river valleys and on gully heads with bare soil. The area with potential erosion in these catchments varies within the range of 17–33%. The erosion on the Yamal Peninsula is mainly of natural origin. It occurs on steep slopes and at the heads of gullies. These landforms are not used for exploitation camps and settlements. Nevertheless, the linear structures, such as railways, roads and pipelines, can cross these unstable landforms with the risk of damage. Erosion potential increases at the spots with bare soil, which appear due to both construction work and natural processes, such as slumping.

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Rayment, William, i Trudi Webster. "Observations of Hector's dolphins (Cephalorhynchus hectori) associating with inshore fishing trawlers at Banks Peninsula, New Zealand". New Zealand Journal of Marine and Freshwater Research 43, nr 4 (grudzień 2009): 911–16. http://dx.doi.org/10.1080/00288330909510049.

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Barley, M. E., S. D. Weaver i J. R. de Laeter. "Strontium isotope composition and geochronology of intermediate—silicic volcanics, Mt Somers and Banks Peninsula, New Zealand". New Zealand Journal of Geology and Geophysics 31, nr 2 (kwiecień 1988): 197–206. http://dx.doi.org/10.1080/00288306.1988.10417769.

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Timm, Christian, Kaj Hoernle, Paul Van Den Bogaard, Ilya Bindeman i Steve Weaver. "Geochemical Evolution of Intraplate Volcanism at Banks Peninsula, New Zealand: Interaction Between Asthenospheric and Lithospheric Melts". Journal of Petrology 50, nr 6 (czerwiec 2009): 989–1023. http://dx.doi.org/10.1093/petrology/egp029.

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Shulmeister, James, Jane M. Soons, Glenn W. Berger, Margaret Harper, Sarah Holt, Neville Moar i John A. Carter. "Environmental and sea-level changes on Banks Peninsula (Canterbury, New Zealand) through three glaciation–interglaciation cycles". Palaeogeography, Palaeoclimatology, Palaeoecology 152, nr 1-2 (sierpień 1999): 101–27. http://dx.doi.org/10.1016/s0031-0182(99)00035-8.

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Morgan‐Richards, M., i J. A. Townsend. "Hybridisation of tree weta on Banks Peninsula, New Zealand, and colour polymorphism withinHemideina ricta(Orthoptera: Stenopelmatidae)". New Zealand Journal of Zoology 22, nr 4 (styczeń 1995): 393–99. http://dx.doi.org/10.1080/03014223.1995.9518058.

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