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Journal articles on the topic 'Beachrocks'

Author: Grafiati

Published: 4 June 2021

Last updated: 15 February 2022

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1

Omoto, Kunio. "Radiocarbon Ages and Isotope Fractionations of Beachrock Samples Collected from the Nansei Islands, Southwestern Japan." Radiocarbon 46, no. 2 (2004): 539–50. http://dx.doi.org/10.1017/s0033822200035591.

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A total of 294 beachrock samples were collected from 116 sites on 15 islands in the Nansei Islands chain, southwestern Japan, and were radiocarbon dated. The beachrocks began to form at about 6900 BP and some are still under development in the islands. Values of isotope fractionations of different materials making up the beachrocks ranged between +9.4‰ and −5.7‰. Isotope fractionations outside the range of 0 ± 2‰ suggest that these beachrocks were strongly influenced by underground water and running freshwater when they were cemented. The sea level during the late Holocene has remained the sam

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2

Daryono, Lutfian R., Kazunori Nakashima, Satoru Kawasaki, Koichi Suzuki, Imam Suyanto, and Arief Rahmadi. "Investigation of Natural Beachrock and Physical–Mechanical Comparison with Artificial Beachrock Induced by MICP as a Protective Measure against Beach Erosion at Yogyakarta, Indonesia." Geosciences 10, no. 4 (2020): 143. http://dx.doi.org/10.3390/geosciences10040143.

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Typically, the mitigation of coastal erosion is achieved by amending surface conditions using materials, such as concrete. The objective of this study is to evaluate the feasibility of constructing artificial beachrocks using natural materials (e.g., microbes, sand, shell, pieces of coral, and seaweed, etc.) within a short time, and to propose the method as a novel strategy for coastal protection. Initially, a survey on resistivity and a multichannel analysis of seismic waves (MASW) were conducted along the coastal lines to characterize and elucidate the subsurface structure of existing beachr

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3

Karkani, A., N. Evelpidou, H. Maroukian, and S. Kawasaki. "STUDY OF BEACHROCKS IN EAST ATTICA." Bulletin of the Geological Society of Greece 50, no. 1 (2017): 434. http://dx.doi.org/10.12681/bgsg.11744.

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Sea level indicators, such as tidal notches and beachrocks, may provide valuable information for the relative sea level changes of an area. Beachrocks in particular have received various arguments concerning their use as reliable sea level indicators and their formation environment. This work focuses on the coasts of East Attica in order to trace the palaeoshorelines of the Upper Holocene through the study of beachrocks. The coastal zone was surveyed in detail by snorkelling and diving, in order to locate, map and sample beachrocks. The samples were studied under a SEM, which showed that the b

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4

Erginal, Ahmet, Nafiye Kiyak, Muhammed Ozturk, et al. "First note on marine-like cementation of Late Holocene beachrock, Iznik Lake (Turkey)." Geochronometria 39, no. 1 (2012): 76–83. http://dx.doi.org/10.2478/s13386-011-0053-2.

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Abstract Micro-fabric characteristics and optically stimulated luminescence (OSL) dating results are presented to discuss the controlling agents and timing of beachrock cementation on the fresh-water Iznik Lake shoreline. The beachrocks are made up of grain-supported polygenic conglomerate containing 20.42% carbonate with encrusted grains, basically as micrite coatings, isopachous aragonite rims, cryptocrystalline void fills and meniscus bridges. The optical ages of twelve samples yielded ages that range from 4.226±0.569 ka on the lowermost beds to 0.706±0.081 on the uppermost. This is the fir

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5

Guerra, Núbia C., Chang H. Kiang, and Alcides N. Sial. "Carbonate cements in contemporaneous beachrocks, Jaguaribe beach, Itamaracá island, northeastern Brazil: petrographic, geochemical and isotopic aspects." Anais da Academia Brasileira de Ciências 77, no. 2 (2005): 343–52. http://dx.doi.org/10.1590/s0001-37652005000200011.

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Holocene beachrocks of the Jaguaribe beach, State of Pernambuco, northeastern Brazil, consist of horizontal, cemented layers approximately 40 cm thick. The cement shows three textural varieties: (a) calciferous, surrounding siliciclastic grains, (b) micritic, with an acicular fringe; and (c) cryptocrystalline calcite in pores. Early cementation took place at the water table below beach ridges, where geochemical, hydrodynamic and, perhaps, also microbiological conditions favored rapid precipitation of aragonite and/or high-Mg calcite. delta13C values range from -1.8 to +1.5‰ for dissolved carbo

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6

Ferreira Júnior, Antônio Vicente. "Ambientes de Formação, Processos de Cimentação de Arenitos de Praia e Indicadores de Variações do Nível do Mar (Environments of Formation, Processes of Cementation of Beachrocks and Indicators of Sea Level Variations)." Revista Brasileira de Geografia Física 4, no. 5 (2012): 938. http://dx.doi.org/10.26848/rbgf.v4i5.232746.

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O artigo contém revisão bibliográfica sobre origem e ambiente de formação dos arenitos de praia, assunto hoje em discussão no meio científico. Com base em diversos autores, busca-se apresentar os ambientes de formação e respectivos processos de gênese, tanto físico-químicos quanto por atividade microbiana destacando os processos de cimentação e seu papel enquanto indicadores de antigos níveis marinhos.Palavras-chave: Arenitos de praia, diagênese, cimentação, nível do mar. Environments of Formation, Processes of Cementation of Beachrocks and Indicators of Sea Level Variations ABSTRACTThis paper

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7

Danjo, Takashi, and Satoru Kawasaki. "Characteristics of Beachrocks: A Review." Geotechnical and Geological Engineering 32, no. 2 (2013): 215–46. http://dx.doi.org/10.1007/s10706-013-9712-9.

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8

Iturregui, Ane, Nikole Arrieta, Xabier Murelaga, et al. "The relevance of the analytical methodology in the geochemical study of beachrock outcrops: Arrigunaga Beach inside the Nerbioi-Ibaizabal estuary (Getxo, Basque Country)." Anal. Methods 6, no. 20 (2014): 8247–57. http://dx.doi.org/10.1039/c4ay00913d.

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9

Edwards, Taneisha C. P., and Simon F. Mitchell. "Trace Fossils in Clastic Beachrocks at the Yallahs Salt Ponds, Jamaica: Implications for Beachrock Cementation." Journal of Coastal Research 342 (March 2018): 429–33. http://dx.doi.org/10.2112/jcoastres-d-16-00176.1.

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10

Psomiadis, D., E. Dotsika, K. Albanakis, N. Zisi, D. Poutoukis, and A. Lazaridis. "COMPARISON OF SAMPLING TECHNIQUES FOR ISOTOPIC ANALYSIS OF SHALLOW MARINE CARBONATES." Bulletin of the Geological Society of Greece 43, no. 5 (2017): 2383. http://dx.doi.org/10.12681/bgsg.11638.

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Recent studies have widely used beachrock samples for isotopic and dating techniques; however the source matrix of the analyzed samples varied. Bulk rock material, skeletal fragments, allochems and pure cement have been used in different studies. Basic parameters of each technique are crucial for the accuracy and the reliability of the obtained results, affecting each time important agents. This study includes isotopic analyses (δ13C, δ18O) of marine carbonates (beachrocks) from the coasts of N. Greece (Thassos island). The sub-sampling was carried out along beachrock cores, following differen

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11

Petropoulos, A., I. Baziotis, Ch Anagnostou, and N. Evelpidou. "BEACHROCKS CEMENT CHARACTERISTICS AND CONDITIONS OF FORMATION. CASE STUDY PLATANIAS BEACH, CHANIA, GREECE." Bulletin of the Geological Society of Greece 50, no. 1 (2017): 458. http://dx.doi.org/10.12681/bgsg.11747.

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Beachrocks represents a coastal deposition in the intertidal area, and studying their properties may lead to create a model which identifies the conditions of their formation (paleo-environment). This paper focuses most intently on the cement material which is able to recover the paleo-environment conditions during diagenesis of such coastal sediment. We used optical microscopy, secondary electron microscopy and Raman Spectroscopy to characterize the cement texture, mineralogy and chemistry in the beachrocks. The existence of pure calcite primarily controlled by the meteorite water, while Mg-c

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12

Ghandour, Ibrahim, Hamad Al-Washmi, Athar Khan, Ammar Mannaa, Mohammed Aljahdali, and Brian Jones. "Depositional Setting and Cementation Pattern of Al-Mejarma Beachrocks, Saudi Arabia: A Proxy for the Late Quaternary Red Sea Coastal Evolution." Journal of Marine Science and Engineering 9, no. 9 (2021): 1012. http://dx.doi.org/10.3390/jmse9091012.

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This study utilizes lithofacies characteristics, petrographic, XRD, and stable isotope data of Al-Mejarma beachrocks, Red Sea, Saudi Arabia, to interpret its depositional setting, origin of cement, and coastal evolution. The beachrock is 1.15 m thick, medium to very coarse-grained sandstone with scattered granules. It shows massive to graded bedding, horizontal, ripple, and shore parallel to slightly oblique planar cross-laminations, with a remarkable absence of bioturbation. It was deposited by shore-parallel longshore currents in a relatively high-energy beach environment. The framework comp

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13

Friedman, Gerald M. "Beachrocks record Holocene events, including natural disasters." Carbonates and Evaporites 26, no. 2 (2011): 97–109. http://dx.doi.org/10.1007/s13146-011-0056-3.

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14

MICHELLI, MAXIMILIANO, TEREZA ARAÚJO, MAURO MAIDA, and HELENICE VITAL. "Indicatives of ancient conditions of sea level stability on the southern Pernambuco continental shelf." Pesquisas em Geociências 28, no. 2 (2001): 25. http://dx.doi.org/10.22456/1807-9806.20266.

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The continental shelf in southern Pernambuco State (Brazilian Northeast) is characteristically narrow, and breaks around 32km from the actual coastline, in depths of 50 to 60m. The sediments on this shelf are similar in their constitution to the rest of the Brazilian Northeastern shelf, showing a prevailing fraction of coarse carbonatic sands. There is also a significant input of terrigenous material, which may be found mainly up to 20m deep. Regarding it’s geomorphology, Pernambuco’s southern shelf presents a soft slope, with long and smooth surfaces, sometimes crossed by meandering channels

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15

Rollnic, Marcelo, and Carmen Medeiros. "Equilibrium Beach Profile in the Presence of Beachrocks." Journal of Coastal Research 75, sp1 (2016): 452–56. http://dx.doi.org/10.2112/si75-091.1.

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16

DANJO, Takashi, and Satoru KAWASAKI. "Formation Mechanisms of Beachrocks Based on Cement Materials." Journal of MMIJ 129, no. 7 (2013): 520–28. http://dx.doi.org/10.2473/journalofmmij.129.520.

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17

DANJO, Takashi, and Satoru KAWASAKI. "Physical and Mechanical Properties of Beachrocks in Okinawa Island." Journal of the Japan Society of Engineering Geology 53, no. 4 (2012): 191–200. http://dx.doi.org/10.5110/jjseg.53.191.

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18

Karkani, Anna, Niki Evelpidou, Matteo Vacchi, et al. "Tracking shoreline evolution in central Cyclades (Greece) using beachrocks." Marine Geology 388 (June 2017): 25–37. http://dx.doi.org/10.1016/j.margeo.2017.04.009.

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19

Mannaa, Ammar A., Rabea A. Haredy, and Ibrahim M. Ghandour. "Beachrock as a Paleoshoreline Indicator: Example from Wadi Al-Hamd, South Al-Wajh, Saudi Arabia." Journal of Marine Science and Engineering 9, no. 9 (2021): 984. http://dx.doi.org/10.3390/jmse9090984.

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The present study concerns the Holocene inland beachrocks that are exposed in the Red Sea coastal plain at the mouth of Wadi Al-Hamd, South Al-Wajh City, Saudi Arabia, and their utility as an indicator for Holocene climate and sea level changes. In addition, the framework composition, and carbon and oxygen isotopic data, are employed to interpret the origin of their cement. The beachrock consists mainly of gravel and coarse-grained terrigenous sediments dominated by lithic fragments of volcanic rocks, cherts and rare limestones along with quartz, feldspars and traces of amphiboles and heavy mi

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20

Vieira, Marcela Marques, Luiz Fernando De Ros, and Francisco Hilário Rego Bezerra. "Lithofaciology and Palaeoenvironmental Analysis of Holocene Beachrocks in Northeastern Brazil." Journal of Coastal Research 236 (November 2007): 1535–48. http://dx.doi.org/10.2112/05-0562.1.

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21

Calvet, F., M. C. Cabrera, J. C. Carracedo, et al. "Beachrocks from the island of La Palma (Canary Islands, Spain)." Marine Geology 197, no. 1-4 (2003): 75–93. http://dx.doi.org/10.1016/s0025-3227(03)00090-2.

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22

M.I., Vousdoukas, Velegrakis A.F., Paul M., Dimitriadis C., Makrykosta E., and Koutsoubas D. "Field observations and modeling of wave attenuation over colonized beachrocks." Continental Shelf Research 48 (October 2012): 100–109. http://dx.doi.org/10.1016/j.csr.2012.08.015.

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23

Teng, JianBin, and JianWei Shen. "Microbial carbonates in Holocene beachrocks, Shuiweiling, Luhuitou Peninsula, Hainan Island." Science in China Series D: Earth Sciences 51, no. 1 (2008): 30–40. http://dx.doi.org/10.1007/s11430-007-0132-7.

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24

De Souza, Nivaldo Lemos, Maria Fernanda Torres, and Antonio Vicente Ferreira Junior. "Percepção Ambiental e Inventário dos Serviços Ecossistêmicos nas Praias do Pina e Boa Viagem, Recife, Pernambuco (Environmental Perception and Inventory of Ecosystem Services in the Pina and Boa Viagem Beaches, Recife, Pernambuco)." Revista Brasileira de Geografia Física 12, no. 4 (2019): 1238. http://dx.doi.org/10.26848/rbgf.v12.4.p1238-1251.

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Este trabalho se pauta pela crescente urbanização na região costeira da cidade do Recife e como isso afeta a oferta dos serviços ecossistêmicos ao decorrer do litoral recifense. Buscou-se, também, as especificações das diferenças sobre percepção ambiental nas praias do Pina e Boa Viagem, localizadas na cidade de Recife, Pernambuco. Para a caracterização das diferentes percepções que os frequentadores possuem acerca da praia e dos arenitos e para inventariar os serviços ecossistêmicos, foram feitas aplicações de questionários e o preenchimento de ficha de campo. Os entrevistados possuem percepç

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25

CHAVES, NUBIA S. "Mechanism of cementation in beachrocks based on petrographic and geochemical evidence." Anais da Academia Brasileira de Ciências 73, no. 3 (2001): 472. http://dx.doi.org/10.1590/s0001-37652001000300034.

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26

Pinheiro, Lara M., Raqueline C. P. Monteiro, Juliana A. Ivar do Sul, and Monica F. Costa. "Do beachrocks affect microplastic deposition on the strandline of sandy beaches?" Marine Pollution Bulletin 141 (April 2019): 569–72. http://dx.doi.org/10.1016/j.marpolbul.2019.03.010.

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27

Vieira, Marcela Marques, and Luiz Fernando De Ros. "Cementation patterns and genetic implications of Holocene beachrocks from northeastern Brazil." Sedimentary Geology 192, no. 3-4 (2006): 207–30. http://dx.doi.org/10.1016/j.sedgeo.2006.04.011.

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28

Ramachandran, Asha Latha, Pelin Polat, Abhijit Mukherjee, and Navdeep K. Dhami. "Understanding and creating biocementing beachrocks via biostimulation of indigenous microbial communities." Applied Microbiology and Biotechnology 104, no. 8 (2020): 3655–73. http://dx.doi.org/10.1007/s00253-020-10474-6.

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29

AlShuaibi, A. A., F. I. Khalaf, and A. Al-Zamel. "Calcareous thrombolitic crust on Late Quaternary beachrocks in Kuwait, Arabian Gulf." Arabian Journal of Geosciences 8, no. 11 (2015): 9721–32. http://dx.doi.org/10.1007/s12517-015-1869-5.

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30

Daryono, Lutfian R., Kazunori Nakashima, Satoru Kawasaki, et al. "Shoreline mapping based on beachrocks identification in Krakal-Sadranan beach, Yogyakarta, Indonesia." Bulletin of Engineering Geology and the Environment 80, no. 3 (2021): 2825–44. http://dx.doi.org/10.1007/s10064-020-02101-5.

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31

Dalongeville, Rémi. "Arguments en faveur de la prise en compte de la cimentation des beachrocks." Géomorphologie : relief, processus, environnement 7, no. 4 (2001): 296–97. http://dx.doi.org/10.3406/morfo.2001.1114.

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32

Blanco-Zubiaguirre, L., N. Arrieta, A. Iturregui, et al. "Focused ultrasound solid–liquid extraction for the determination of organic biomarkers in beachrocks." Ultrasonics Sonochemistry 27 (November 2015): 430–39. http://dx.doi.org/10.1016/j.ultsonch.2015.06.012.

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33

Vousdoukas, M. I., A. F. Velegrakis, and T. V. Karambas. "Morphology and sedimentology of a microtidal beach with beachrocks: Vatera, Lesbos, NE Mediterranean." Continental Shelf Research 29, no. 16 (2009): 1937–47. http://dx.doi.org/10.1016/j.csr.2009.04.003.

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34

Danjo, Takashi, and Satoru Kawasaki. "Formation Mechanisms of Beachrocks in Okinawa and Ishikawa, Japan, with a Focus on Cements." MATERIALS TRANSACTIONS 55, no. 3 (2014): 493–500. http://dx.doi.org/10.2320/matertrans.m-m2013844.

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35

Vacchi, Matteo. "Assessing the late Quaternary coastal uplift of Lesvos Island using beachrocks distribution and morphology." Quaternary International 279-280 (November 2012): 509. http://dx.doi.org/10.1016/j.quaint.2012.08.1755.

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36

David, Psomiadis, Tsourlos Panagiotis, and Albanakis Konstantinos. "Electrical resistivity tomography mapping of beachrocks: application to the island of Thassos (N. Greece)." Environmental Earth Sciences 59, no. 1 (2009): 233–40. http://dx.doi.org/10.1007/s12665-009-0021-9.

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37

Daryono, L. R., A. D. Titisari, I. W. Warmada, and S. Kawasaki. "Comparative characteristics of cement materials in natural and artificial beachrocks using a petrographic method." Bulletin of Engineering Geology and the Environment 78, no. 6 (2018): 3943–58. http://dx.doi.org/10.1007/s10064-018-1355-x.

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38

Erginal, Ahmet Evren, Nafiye Güneç Kıyak, Muhammed Zeynel Öztürk, Mustafa Avcıoğlu, Mustafa Bozcu, and Erdinç Yiğitbaş. "Cementation characteristics and age of beachrocks in a fresh-water environment, Lake İznik, NW Turkey." Sedimentary Geology 243-244 (January 2012): 148–54. http://dx.doi.org/10.1016/j.sedgeo.2011.10.012.

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39

Ghandour, Ibrahim M., Hamad A. Al-Washmi, Rashad A. Bantan, and Mohamed M. Gadallah. "Petrographical and petrophysical characteristics of asynchronous beachrocks along Al-Shoaiba Coast, Red Sea, Saudi Arabia." Arabian Journal of Geosciences 7, no. 1 (2013): 355–65. http://dx.doi.org/10.1007/s12517-012-0826-9.

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40

MALTA, J. V., and J. W. A. CASTRO. "Petrography, Stable Isotops and Geochronology of Beachrocks from the Coastline of Rio de Janeiro State, SE Brazil." Anuário do Instituto de Geociências - UFRJ 41, no. 1 (2018): 232–44. http://dx.doi.org/10.11137/2018_1_232_244.

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41

Guimarães, Thaís, Gorki Mariano, Alcina Barreto, and Artur A. Sá. "Beachrocks of Southern Coastal Zone of the State of Pernambuco (Northeastern Brazil): Geological Resistance with History." Geoheritage 9, no. 1 (2016): 111–19. http://dx.doi.org/10.1007/s12371-016-0181-4.

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42

ΚΑΡΑΛΗ-ΒΟΥΔΟΥΡΗ, Α., Γ. ΛΕΙΒΑΔΙΤΗΣ, and A. ΜΕΤΤΟΣ. "Study of the coastal sediments of the Loutraki gulf area." Bulletin of the Geological Society of Greece 34, no. 2 (2018): 717. http://dx.doi.org/10.12681/bgsg.17348.

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The study of the sedimentological and mineralogical characteristics of the coastal sediments in the Loutraki gulf, included analyses of a large number of samples, that is granulometry, thin section study and x-ray examination. From these data the granulometry paramètres were assessed such as mean grain size, standard deviation σ, skewness SK, and kurtosis KG of the sediments. The study of the sedimentological parameters based on the mean grain size the offshoreline is covered by coarse grain sand, whereas the tidal zone indicates a high energy environment. The longshoredrift is from Ν to S. Mo

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43

PSOMIADIS, David, Konstantinos ALBANAKIS, Nikoleta ZISI, Matthieu GHILARDI, and Elissavet DOTSIKA. "Clastic sedimentary features of beachrocks and their palaeo-environmental significance: comparison of past and modern coastal regimes." International Journal of Sediment Research 29, no. 2 (2014): 260–68. http://dx.doi.org/10.1016/s1001-6279(14)60041-x.

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44

Chaves, N. S., and A. N. Sial. "Mixed Oceanic and Freshwater Depositional Conditions for Beachrocks of Northeast Brazil: Evidence from Carbon and Oxygen Isotopes." International Geology Review 40, no. 8 (1998): 748–54. http://dx.doi.org/10.1080/00206819809465235.

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45

Ghandour, Ibrahim M., Hamad A. Al-Washmi, Rashad A. Bantan, and Mohamed M. Gadallah. "Erratum to: Petrographical and petrophysical characteristics of asynchronous beachrocks along Al-Shoaiba Coast, Red Sea, Saudi Arabia." Arabian Journal of Geosciences 7, no. 1 (2013): 367. http://dx.doi.org/10.1007/s12517-013-0879-4.

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46

Pirazzoli, Paolo Antonio. "De l'interprétation de la cimentation dans un beachrock. Quelques remarques sur : "Les variations holocènes du niveau marin mises en évidence par les caractères de la diagenèse des beachrocks ; exemple de Damnoni (Crète)"." Géomorphologie : relief, processus, environnement 7, no. 4 (2001): 295. http://dx.doi.org/10.3406/morfo.2001.1113.

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47

Gaki - Papanastassiou, K., E. Karymbalis, H. Maroukian, and K. Tsanakas. "GEOMORPHIC EVOLUTION OF WESTERN (PALIKI) KEPHALONIA ISLAND (GREECE) DURING THE QUATERNARY." Bulletin of the Geological Society of Greece 43, no. 1 (2017): 418. http://dx.doi.org/10.12681/bgsg.11193.

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Kephalonia Island is located in the Ionian Sea (western Greece). The active subduction zone of the African lithosphere submerging beneath the Eurasian plate is placed just west of the island. The evolution of the island is depended mostly on the geodynamic processes derived from this vigorous margin. The geomorphic evolution of the western part of the island (Paliki peninsula) during the Quaternary was studied, by carrying out detailed field geomorphological mapping focusing on both coastal and fluvial landforms, utilizing aerial photos and satellite image interpretation with the use of GIS te

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48

da Silva, André L. C., Maria A. M. da Silva, Rogério S. de Souza, and Márcio L. V. Pinto. "The role of beachrocks on the evolution of the Holocene barrier systems in Rio de Janeiro, southeastern Brazil." Journal of Coastal Research 70 (April 28, 2014): 170–75. http://dx.doi.org/10.2112/si70-029.1.

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49

Al-Ramadan, Khalid. "Diagenesis of Holocene beachrocks: a comparative study between the Arabian Gulf and the Gulf of Aqaba, Saudi Arabia." Arabian Journal of Geosciences 7, no. 11 (2013): 4933–42. http://dx.doi.org/10.1007/s12517-013-1127-7.

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50

Potratz, Guilherme Loriato, Felipe Saliba de Souza e Almeida, João Wagner de Alencar Castro, Maria Virginia Alves Martins, and Mauro Cesar Geraldes. "EVOLUTION AND PALEOENVIRONMENTAL RECONSTITUTION OF THE SOUTHERN ZONE OF THE RIO DE JANEIRO CITY (SE BRAZIL)." Journal of Sedimentary Environments 4, no. 2 (2019): 189–98. http://dx.doi.org/10.12957/jse.2019.43766.

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Paleoenvironmental reconstructions in coastal environments have been carried out using indicators of relative sea level oscillation (RSL), among them, mollusk shells, beachrocks and sedimentary records. Data from eleven geological-geotechnical drilling cores (from 15 m to 30 m long) distributed along the Ipanema - Leblon coastline and on the edge of the Rodrigo de Freitas Lagoon and respective stratigraphic profiles were analyzed in this work. Eleven radiocarbon ages obtained from shell samples calibrated to eliminate the effect of reservoir were used to perform the time evolution of the study

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