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Journal articles on the topic 'Vertical zonation'

Author: Grafiati

Published: 4 June 2021

Last updated: 6 February 2022

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1

Noda, Takashi, Aiko Iwasaki, and Keiichi Fukaya. "Recovery of rocky intertidal zonation: two years after the 2011 Great East Japan Earthquake." Journal of the Marine Biological Association of the United Kingdom 96, no. 8 (2015): 1549–55. http://dx.doi.org/10.1017/s002531541500212x.

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To assess the course and status of recovery of rocky intertidal zonation after massive subsidence caused by the 2011 Great East Japan Earthquake, from 2011 to 2013 we censused the vertical distribution of 10 dominant macrobenthic species (six sessile and four mobile species) in the mid-shore zone of 23 sites along the Sanriku coastline, 150–160 km north-northwest of the earthquake epicentre, and compared the vertical distributions of each species with their vertical distributions in the pre-earthquake period. The dynamics of rocky intertidal zonation varied substantially among species. Among s

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2

Yezhov, Yu A., and G. P. Lysenin. "VERTICAL ZONATION IN THE DEVELOPMENT OF KARST." International Geology Review 32, no. 5 (1990): 523–31. http://dx.doi.org/10.1080/00206819009465796.

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3

Sherman, S. I., V. Yu Buddo, and A. I. Miroshnichenko. "VERTICAL ZONATION AND FLUID PERMEABILITY OF FAULT ZONES." International Geology Review 33, no. 9 (1991): 889–902. http://dx.doi.org/10.1080/00206819109465732.

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4

Fenchel, T., LD Kristensen, and L. Rasmussen. "Water column anoxia: vertical zonation of planktonic protozoa." Marine Ecology Progress Series 62 (1990): 1–10. http://dx.doi.org/10.3354/meps062001.

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5

Aubele, Jayne C., L. S. Crumpler, and Wolfgang E. Elston. "Vesicle zonation and vertical structure of basalt flows." Journal of Volcanology and Geothermal Research 35, no. 4 (1988): 349–74. http://dx.doi.org/10.1016/0377-0273(88)90028-5.

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6

Lakova, Iskra, and Silviya Petrova. "Towards a standard Tithonian to Valanginian calpionellid zonation of the Tethyan Realm." Acta Geologica Polonica 63, no. 2 (2013): 201–22. http://dx.doi.org/10.2478/agp-2013-0008.

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Abstract Lakova, I. and Petrowa, S. 2013. Towards a standard Tithonian to Valanginian calpionellid zonation of the Tethyan Realm. Acta Geologica Polonica, 63 (2), 201-221. Warszawa. A calpionellid zonal scheme is proposed for the Tithonian through Valanginian pelagic carbonates of the Western Balkan Unit, based on the vertical ranges of 57 chitinoidellid and calpionellid species recognized. This zonal scheme consists of calpionellid zones that are widely accepted in the Mediterranean Realm, such as the zones of Chitinoidella, Praetintinnopsella, Crassicollaria, Calpionella, Calpionellopsis, Ca

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7

Ogureyeva, G. N. "Vertical vegetation zonation in the mountains of Northeast Siberia." Polar Geography 22, no. 3 (1998): 201–10. http://dx.doi.org/10.1080/10889379809377651.

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8

Fenchel, T., and M. Kühl. "Artificial Cyanobacterial Mats: Growth, Structure, and Vertical Zonation Patterns." Microbial Ecology 40, no. 2 (2000): 85–93. http://dx.doi.org/10.1007/s002480000062.

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9

Bongaerts, Pim, Margaux Carmichael, Kyra B. Hay, Linda Tonk, Pedro R. Frade, and Ove Hoegh-Guldberg. "Prevalent endosymbiont zonation shapes the depth distributions of scleractinian coral species." Royal Society Open Science 2, no. 2 (2015): 140297. http://dx.doi.org/10.1098/rsos.140297.

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Bathymetric distributions of photosynthetic marine invertebrate species are relatively well studied, however the importance of symbiont zonation (i.e. hosting of distinct algal endosymbiont communities over depth) in determining these depth distributions still remains unclear. Here, we assess the prevalence of symbiont zonation in tropical scleractinian corals by genotyping the Symbiodinium of the 25 most common species over a large depth range (down to 60 m) on a Caribbean reef. Symbiont depth zonation was found to be common on a reef-wide scale (11 out of 25 coral species), and a dominant fe

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10

Peng, Buzhuo, Fu Chen, and Lijie Pu. "Progress in the study on mountainous vertical zonation in China." Chinese Geographical Science 9, no. 4 (1999): 297–305. http://dx.doi.org/10.1007/s11769-999-0002-7.

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11

McNeill, Myndee. "Vertical Zonation: Studying Ecological Patterns in the Rocky Intertidal Zone." Science Activities: Classroom Projects and Curriculum Ideas 47, no. 1 (2010): 8–14. http://dx.doi.org/10.1080/00368120903280735.

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12

Campbell, Jocelyn, and Darwyn S. Coxson. "Canopy microclimate and arboreal lichen loading in subalpine spruce-fir forest." Canadian Journal of Botany 79, no. 5 (2001): 537–55. http://dx.doi.org/10.1139/b01-025.

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Hair lichen communities in Engelmann spruce (Picea engelmannii) subalpine fir (Abies lasiocarpa) forests of the northern Cariboo Mountains (British Columbia) show distinct vertical zonation. Alectoria sarmentosa reaches peak abundance in the lower canopy (over 35 kg/ha) whereas Bryoria spp. lichens reach peak abundance in the upper canopy (over 250 kg/ha). These distribution patterns are accentuated by stand structure with trees growing in clumps retaining significantly higher lichen loading on a per branch basis compared to solitary trees. The vertical zonation of lichen communities is acco

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13

Liu, Xiangchong, Wenlei Wang, and Dehui Zhang. "The Mechanisms Forming the Five–Floor Zonation of Quartz Veins: A Case Study in the Piaotang Tungsten–Tin Deposit, Southern China." Minerals 11, no. 8 (2021): 883. http://dx.doi.org/10.3390/min11080883.

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It is common among many vein–type tungsten deposits in southern China that the thickness of ore veins increases from <1 cm to >1 m with increasing depth. A five–floor zonation model for the vertical trend of vein morphology was proposed in the 1960s and has been widely applied for predicting ore bodies at deeper levels, but the causative mechanisms for such a zonation remain poorly understood. The Piaotang tungsten–tin deposit, one of the birthplaces of the five–floor zonation model, is chosen as a case study for deciphering the mechanisms forming its morphological zonation of quartz vei

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14

Cui, Tao. "Vertical Zonation in Penecontemporaneous Period of the Bauxite in WZD Area." Advanced Materials Research 989-994 (July 2014): 1380–83. http://dx.doi.org/10.4028/www.scientific.net/amr.989-994.1380.

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Through systematically geologic survey and observation of drills, this paper have a comprehensive research on Vertical zonation in bauxite deposit of Wuchuan-Zheng,an-Daozhen (WZD) area. Environment of WZD bauxite in penecontemporaneous period can be divided into two parts: vadose zone and phreatic zone. Vadose zone is oxidized and acidic environment. Phreatic zone is reduced and alkalescent environment. Vadose zone is favorable to mineralization, but phreatic zone is not favorable to mineralization.

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15

Danovaro, R., and S. Fraschetti. "Meiofaunal vertical zonation on hard-bottoms: comparison with soft-bottom meiofauna." Marine Ecology Progress Series 230 (2002): 159–69. http://dx.doi.org/10.3354/meps230159.

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16

Strachan, K. L., T. R. Hill, J. M. Finch, and R. L. Barnett. "VERTICAL ZONATION OF FORAMINIFERA ASSEMBLAGES IN GALPINS SALT MARSH, SOUTH AFRICA." Journal of Foraminiferal Research 45, no. 1 (2015): 29–41. http://dx.doi.org/10.2113/gsjfr.45.1.29.

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17

MULLER, UTE. "Vertical zonation and production rates of epiphytic algae on Phragmites australis." Freshwater Biology 34, no. 1 (1995): 69–80. http://dx.doi.org/10.1111/j.1365-2427.1995.tb00424.x.

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18

ABBIATI, M., C. N. BIANCHI, and A. CASTELLI. "Polychaete Vertical Zonation along a Littoral Cliff in the Western Méditerranean." Marine Ecology 8, no. 1 (1987): 33–48. http://dx.doi.org/10.1111/j.1439-0485.1987.tb00173.x.

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19

Wang, Yu, Yue Hu, and Tengyuan Zhao. "Cone penetration test (CPT)-based subsurface soil classification and zonation in two-dimensional vertical cross section using Bayesian compressive sampling." Canadian Geotechnical Journal 57, no. 7 (2020): 947–58. http://dx.doi.org/10.1139/cgj-2019-0131.

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A novel method is developed in this study for soil classification and zonation in a two-dimensional (2D) vertical cross section using cone penetration tests (CPTs). A CPT is usually performed vertically and the number of CPT soundings in a site is often limited in geotechnical engineering practice. It is, therefore, difficult to properly interpret CPT results along the horizontal direction or accurately estimate the horizontal correlation length of CPT data. The method proposed in this study bypasses the difficulty in estimating horizontal correlation length and provides proper identification

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20

Tikhlivets, S. V., and O. M. Trunin. "Horizontal and vertical zonation of the weathering rind of the northern part of the Krivy Rig Basin." Journal of Geology, Geography and Geoecology 28, no. 3 (2019): 581–90. http://dx.doi.org/10.15421/111955.

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The ferriferous-siliceous formation of the Kryvyi Rih Basin has been formed as a result of the effect of different geological processes: sedimentation, diagenesis, dynamothermal metamorphism, metasomatosis, orogenesis, hypergenesis. Hypergenic changes are manifested to a different extent within iron ore deposits of the Kryvyi Rih Basin. In the south part of the basin, thickness of the weathering rind in some places reaches 1,000-1,500 m, it is up to 2,500 in the central, and in the northern part this parameter is much lower. Hypergenic processes are observed in the sections of all stratigraphi

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21

Buzhuo, Peng, Pu Lijie, Bao Haosheng, and D. L. Higgitt. "Vertical Zonation of Landscape Characteristics in the Namjagbarwa Massif of Tibet, China." Mountain Research and Development 17, no. 1 (1997): 43. http://dx.doi.org/10.2307/3673912.

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22

Greenwood, A., R. M. O'Riordan, and D. K. A. Barnes. "Seasonality and vertical zonation of zooplankton in a semi-enclosed sea lough." Journal of the Marine Biological Association of the United Kingdom 81, no. 2 (2001): 213–20. http://dx.doi.org/10.1017/s0025315401003666.

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Zooplankton was collected by a diver-towed net close to the substratum at four depths (0, 6, 12 and 18 m) over a 17 month period in three locations in Lough Hyne, Co. Cork, Ireland. Zooplankton was identified to phylum or class levels and mean numbers were calculated for each taxon, site and depth. Seasonality was observed in several meroplanktonic groups (Echinodermata, Nemertea, Mollusca and fish postlarvae), and in gelatinous zooplankton. Depth preference was found to be statistically significant in the polychaetes (larvae and pelagic species), molluscan and ascidian larvae. However, the in

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23

Benson, K. R. "The Study of Vertical Zonation on Rocky Intertidal Shores--A Historical Perspective." Integrative and Comparative Biology 42, no. 4 (2002): 776–79. http://dx.doi.org/10.1093/icb/42.4.776.

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24

., S. H. Mohammad. "Vertical Zonation and Biometric Parameter of the Gastropod Cerithium scabridum in Suez Canal." Research Journal of Environmental Sciences 2, no. 2 (2008): 100–107. http://dx.doi.org/10.3923/rjes.2008.100.107.

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25

Juvik, James O., Sonia P. Juvik, and Lawrence S. Hamilton. "Altitudinal Resource Zonation versus Vertical Control: Land Use Conflict on Two Hawaiian Mountains." Mountain Research and Development 12, no. 3 (1992): 211. http://dx.doi.org/10.2307/3673666.

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26

WANG, Xian-pu, Shun-li YU, and Da-you TANG. "The Heritage Value of Mountain Vertical Zonation in Temperate Desert Region of China." Arid Zone Research 26, no. 5 (2010): 694–700. http://dx.doi.org/10.3724/sp.j.1148.2009.00694.

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27

Ferre, E. C., K. J. Michelsen, W. G. Ernst, J. D. Boyd, and E. Canon-Tapia. "Vertical zonation of the Barcroft granodiorite, White Mountains, California: Implications for magmatic processes." American Mineralogist 97, no. 7 (2012): 1049–59. http://dx.doi.org/10.2138/am.2012.4013.

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28

MÜLLER, UTE. "The vertical zonation of adpressed diatoms and other epiphytic algae on Phragmites australis." European Journal of Phycology 34, no. 5 (1999): 487–96. http://dx.doi.org/10.1017/s0967026299002413.

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29

Müller, Ute. "The vertical zonation of adpressed diatoms and other epiphytic algae on Phragmites australis." European Journal of Phycology 34, no. 5 (1999): 487–96. http://dx.doi.org/10.1080/09541449910001718841.

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30

Fosså, Jan Helge. "Near-bottom vertical zonation during daytime of deep-living hyperbenthic mysids (Crustacea: Mysidacea)." Sarsia 70, no. 4 (1985): 297–307. http://dx.doi.org/10.1080/00364827.1985.10419684.

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31

Job, Suresh D., and David R. Bellwood. "Light sensitivity in larval fishes: Implications for vertical zonation in the pelagic zone." Limnology and Oceanography 45, no. 2 (2000): 362–71. http://dx.doi.org/10.4319/lo.2000.45.2.0362.

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32

Sati, Vishwambhar Prasad. "Vertical zonation of horticultural farming in the Alaknanda basin of Garhwal Himalaya, India." Journal of Mountain Science 2, no. 4 (2005): 319–28. http://dx.doi.org/10.1007/bf02918405.

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33

Paavo, B. L., D. Ham, S. Görlitz, and P. K. Probert. "How does tidal submersion time affect macroinvertebrate community patterns on a temperate sheltered sandflat?" Marine and Freshwater Research 63, no. 1 (2012): 68. http://dx.doi.org/10.1071/mf11147.

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A general model of vertical zonation has been a fruitful foundation of rocky shore ecology, but no analogous model is widely accepted for intertidal soft sediments. Various local proxies have been used for shore height or tidal submersion time, although objective measurements are rare in the literature. In this study, temperature loggers identified submersion period (SP) in a sheltered temperate New Zealand inlet at discrete distances along transect vertical profiles associated with macrofaunal community differences. Our aim was to evaluate this submersion quantification method and determine w

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34

Tao, Zhongping, Bingli Liu, Ke Guo, et al. "3D Primary Geochemical Halo Modeling and Its Application to the Ore Prediction of the Jiama Polymetallic Deposit, Tibet, China." Geofluids 2021 (August 19, 2021): 1–13. http://dx.doi.org/10.1155/2021/6629187.

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The identification of primary geochemical haloes can be used to predict mineral resources in deep-seated orebodies through the delineation of element distributions. The Jiama deposits a typical skarn–porphyry Cu–polymetallic deposit in the Gangdese metallogenic belt of Tibet. The Cu–polymetallic skarn, Cu–Mo hornfels, and Mo ± Cu porphyry mineralization there exhibit superimposed geochemical haloes at depth. Three-dimensional (3D) primary geochemical halo modeling was undertaken for the deposit with the aim of providing geochemical data to describe element distributions in 3D space. An overall

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35

Mendonça-Neto, José P., Carlos E. L. Ferreira, Laís C. T. Chaves, and Renato C. Pereira. "Influence of Palythoa caribaeorum (Anthozoa, Cnidaria) zonation on site-attached reef fishes." Anais da Academia Brasileira de Ciências 80, no. 3 (2008): 495–513. http://dx.doi.org/10.1590/s0001-37652008000300010.

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This work aimed to test the influence of Palythoa caribeorum, a widely distributed zoanthid in the Atlantic, on site-attached reef fish in a subtropical rocky shore. Density, richness and vertical distribution of reef fish inside (ID) and outside (OD) previously chosen P. caribaeorum dominance patches were compared through stationary visual censuses along three different periods. Fishes were grouped in different trophic guilds to evidence differences in resources uses in both treatments. A complexity index was estimated by the chain link method and percentage covering of benthic organisms was

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36

Henry, Lea-Anne. "Intertidal zonation and seasonality of the marine hydroid Dynamena pumila (Cnidaria: Hydrozoa)." Canadian Journal of Zoology 80, no. 9 (2002): 1526–36. http://dx.doi.org/10.1139/z02-146.

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The vertical zonation and temporal dynamics of the marine hydroid Dynamena pumila were assessed across a wave-exposure gradient on five rocky shores in the Bay of Fundy, Atlantic Canada. Hydroid abundance and occupancy (i.e., percentage occurrence in a quadrat) were measured in 0.25-m2 quadrats at eight vertical elevations for each site over four consecutive seasons. Hydroid abundance and occupancy were highly correlated (R2 = 0.877). Estimates of hydroid fertility (percentage of sexually reproductive colonies) and size (stem height and number of branches) were obtained in five quadrats at eve

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37

Jones, Brian, Robin W. Renaut, and Michael R. Rosen. "Vertical Zonation of Biota in Microstromatolites Associated with Hot Springs, North Island, New Zealand." PALAIOS 12, no. 3 (1997): 220. http://dx.doi.org/10.2307/3515424.

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38

MARUYAMA, Hiroaki. "VERTICAL ZONATION OF AGRICULTURAL LAND USE ON THE LOWER SOUTHERN SLOPES OF MT. ASAMA." Geographical Review of Japa,. Ser. A, Chirigaku Hyoron 60, no. 10 (1987): 643–66. http://dx.doi.org/10.4157/grj1984a.60.10_643.

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39

Somero, G. N. "Thermal Physiology and Vertical Zonation of Intertidal Animals: Optima, Limits, and Costs of Living." Integrative and Comparative Biology 42, no. 4 (2002): 780–89. http://dx.doi.org/10.1093/icb/42.4.780.

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40

Nazimova, D. I., N. P. Polikarpov, A. I. Sukhinin, Ye V. Fedotova, and V. I. Kharuk. "SATELLITE IMAGERY AND THE VERTICAL ZONATION OF VEGETATION IN THE MOUNTAINS OF SOUTHERN SIBERIA." Mapping Sciences and Remote Sensing 38, no. 3 (2001): 212–21. http://dx.doi.org/10.1080/07493878.2001.10642177.

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41

Lavitt, N., R. I. Acworth, and J. Jankowski. "Vertical Hydrochemical Zonation in a Coastal Section of the Botany Sands Aquifer, Sydney, Australia." Hydrogeology Journal 5, no. 2 (1997): 64–74. http://dx.doi.org/10.1007/s100400050117.

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42

Janousek, Christopher N., Karen M. Thorne, and John Y. Takekawa. "Vertical Zonation and Niche Breadth of Tidal Marsh Plants Along the Northeast Pacific Coast." Estuaries and Coasts 42, no. 1 (2018): 85–98. http://dx.doi.org/10.1007/s12237-018-0420-9.

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43

Kusbach, Antonín, Tadeáš Štěrba, Jan Šebesta, et al. "Ecological Zonation As A Tool For Restoration Of Degraded Forests In Northern Mongolia." GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 12, no. 3 (2019): 98–116. http://dx.doi.org/10.24057/2071-9388-2019-31.

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We developed a geo-vegetation zonation in the Khaan Khentii massif, northern Mongolia. Our specific objective was to assess and classify the response of the tree vegetation to environmental factors operating at a coarse climatic level. We sampled forest ecosystem vegetation, climate, physiographic features, and soil properties. Our analysis included clustering, ordination, classification, and ANOVA techniques. Based on the complex data set, we identified three geo-vegetation zones: forest-steppe, montane and dark taiga zone. We characterized them based on the regional environmental factors; (1

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44

Su, Xiaosi, Yaoxuan Chen, Hang Lyu, Yakun Shi, Yuyu Wan, and Yiwu Zhang. "Response of redox zonation to recharge in a riverbank filtration system: a case study of the Second Songhua river, NE China." Hydrology Research 51, no. 5 (2020): 1104–19. http://dx.doi.org/10.2166/nh.2020.108.

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Abstract Bank filtration induced by groundwater pumping results in redox zonation along the groundwater flow path. Besides the river water, recharge from other sources can change local redox conditions; therefore, redox zonation is likely to be complex within the riverbank filtration (RBF) system. In this study, hydrodynamics, hydrogeochemistry, and environmental stable isotopes were combined together to identify the redox conditions at an RBF site. The recharge characteristics and redox processes were revealed by monitoring the variations of water level, δ2H and δ18O, and redox indexes along

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45

Haerudin, Nandi, Rustadi Rustadi, Helmy Fitriawan, Deassy Siska, and Muchammad Farid. "Earthquake Disaster Mitigation Mapping By Modeling of Land Layer and Site Effect Zone in The Kota Baru of South Lampung." Jurnal Ilmiah Pendidikan Fisika Al-Biruni 8, no. 1 (2019): 53–67. http://dx.doi.org/10.24042/jipfalbiruni.v8i1.3705.

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Kota Baru is the satellite city of Bandar Lampung. The city is prepared for the expansion of the city of Bandar Lampung. Zonation map of earthquake risk is required for Kota Baru due to its location within the reach of earthquake energy of Semangko subduction fault. In this study, we model the earthquake-prone zone map based on the soil characteristics (site effect) combined with the underground layer model to get a detailed description of the horizontal and vertical soil character. The microtremor method is performed to obtain the zonation effect mapping. Whereas, the ground layer modeling is

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46

CHRISTIANSEN, ERIC H. "Contrasting processes in silicic magma chambers: evidence from very large volume ignimbrites." Geological Magazine 142, no. 6 (2005): 669–81. http://dx.doi.org/10.1017/s0016756805001445.

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Very large volume (>1000 km3 of magma) crystal-rich dacitic ignimbrites that lack pronounced evidence of fractional crystallization or vertical zonation erupt in some continental magmatic arcs (e.g. the Lund Tuff of the Great Basin and the Fish Canyon Tuff of Colorado in western USA). Apparently, their magma chambers were only modestly heterogeneous and not systematically zoned from top to bottom. These ignimbrites have 40 to 50% phenocrysts set in a high-silica rhyolite glass. Mineral assemblages and mineral compositions suggest pre-eruption temperatures were 730 to 820°C and water and oxy

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47

Vedenin, Andrey, Sergey Galkin, Alexander N. Mironov, and Andrey Gebruk. "Vertical zonation of the Siberian Arctic benthos: bathymetric boundaries from coastal shoals to deep-sea Central Arctic." PeerJ 9 (June 29, 2021): e11640. http://dx.doi.org/10.7717/peerj.11640.

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The bathymetric distribution of species of Annelida, Crustacea and Echinodermata from the region including the Kara, Laptev and East Siberian seas and the adjacent region of the deep-sea Central Arctic was analysed. We focused on vertical species ranges revealing zones of crowding of upper and lower species range limits. Using published data and in part the material obtained during the expeditions of the P.P. Shirshov Institute of Oceanology, we evaluated species vertical distribution from 0 m to the maximum depth of the Central Arctic (~4,400 m). The entire depth range was divided into smalle

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48

Gaplaev, M. Sh. "PLASTICITY AND ADAPTABILITY OF RED BEET ACCESSIONS IN VERTICAL ZONATION OF CENTRAL PRE-CAUCASIAN REGION." Vegetable crops of Russia, no. 4 (January 1, 2016): 15–20. http://dx.doi.org/10.18619/2072-9146-2016-4-15-20.

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49

Miura, Osamu, Teeyaporn Keawtawee, Nobuko Sato, and Ken-ichi Onodera. "Vertical zonation of endosymbiotic zooxanthellae within a population of the intertidal sea anemone, Anthopleura uchidai." Marine Biology 161, no. 8 (2014): 1745–54. http://dx.doi.org/10.1007/s00227-014-2456-0.

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50

Calder, Dale R. "Vertical zonation of the hydroid Dynamena crisioides (Hydrozoa, Sertulariidae) in a mangrove ecosystem at Twin Cays, Belize." Canadian Journal of Zoology 69, no. 12 (1991): 2993–99. http://dx.doi.org/10.1139/z91-422.

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Dynamena crisioides is generally restricted to lower intertidal and shallow subtidal habitats along tropical and subtropical coasts. The hydroid was abundant during this study on prop roots of red mangroves (Rhizophora mangle) at Twin Cays, Belize, where it ranged vertically from 1.1 m below mean tide level (MTL) to 2–3 cm above MTL. The estimated percentage cover of the hydroid was maximal in the lower half of the intertidal zone (MTL and 0.1 m below MTL) and declined rapidly above and below that level. Colony height and number of branches per colony were also consistently highest in hydroids

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