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Artículos de revistas sobre el tema "Lacustrine Settlement"

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Publicado: 7 de junio de 2025
Última modificación: 2 de agosto de 2025

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1

Bouchet, F., and S. Bentrad. "Recovery of equine helminth eggs in a medieval lacustrine settlement." Veterinary Record 141, no. 23 (1997): 601–2. http://dx.doi.org/10.1136/vr.141.23.601.

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2

Drobyshev, Igor, P. Charles Goebel, David M. Hix, R. Gregory Corace, and Marie E. Semko-Duncan. "Pre- and post-European settlement fire history of red pine dominated forest ecosystems of Seney National Wildlife Refuge, Upper Michigan." Canadian Journal of Forest Research 38, no. 9 (2008): 2497–514. http://dx.doi.org/10.1139/x08-082.

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To understand the dynamics of fire in red pine ( Pinus resinosa Ait.) forest ecosystems that once dominated areas of the northern Lake States, we dendrochronologically reconstructed the fire regime prior to European settlement (pre-1860), after European settlement (1860–1935), and postrefuge establishment (post-1935) for different portions (wilderness and nonwilderness) and landforms (sand ridges and outwash channels) of the Seney National Wildlife Refuge (SNWR) in eastern Upper Michigan. Using data from 50 sites, we found that the cumulative number of fires showed a slow rate of accumulation
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3

Rosenswig, Robert M. "RENEWING THE BELIZE ARCHAIC PROJECT IN 2019." Research Reports in Belizean Archaeology 18 (2023): 177–84. http://dx.doi.org/10.62064/rrba.18.15.

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The Archaic period in the Maya region represents six millennia (7000-1000 BCE) when non-ceramic-using peoples began to experiment with domesticates and reduce their settlement ranges. The single longest epoch of the Mesoamerican chronology, these early millennia are often overshadowed by the investigation of more recent peoples who built cities and have left evidence of elaborate artistic traditions. The Belize Archaic Project (BAP) began work over 20 years ago after the fortuitous discovery of aceramic deposits containing heavily patinated lithic tools and debitage under Postclassic settlemen
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4

Medioli, Barbara E., Aruna Dixit, John P. Smol, Thane W. Anderson, and Susan M. Burbidge. "Paleolimnological Evidence of Terrestrial and Lacustrine Environmental Change in Response to European Settlement of the Red River Valley, Manitoba and North Dakota*." Paleoenvironments 59, no. 2-3 (2007): 263–75. http://dx.doi.org/10.7202/014756ar.

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Abstract Limnological and terrestrial changes in three floodplain lakes are correlated with settlement of the Red River valley in Manitoba and North Dakota. Distinctive pollen, diatom and thecamoebian assemblages provide proxy evidence of the ecological changes from pre- to post-settlement periods in Horseshoe Lake, Lake Louise and Salt Lake. In the pre-settlement period (Zone I), prior to ~1812, grass and Quercus pollen dominate and are indicative of a tall grass prairie-oak riparian forest ecosystem. Diatom and thecamoebian assemblages suggest oligo- to mesotrophic limnological conditions, a
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5

Dahal, Bhim Kumar, Sandip Regmi, Kalyan Paudyal, Diwash Dahal, and Diwakar KC. "Enhancing Deep Excavation Optimization: Selection of an Appropriate Constitutive Model." CivilEng 5, no. 3 (2024): 785–800. http://dx.doi.org/10.3390/civileng5030041.

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To minimize the impact on nearby structures during deep excavations, choosing an appropriate soil constitutive model for analysis holds significant importance. This study aims to conduct a comparative analysis of various constitutive soil models—namely, the Mohr–Coulomb (MC) model, the hardening soil (HS) model, the hardening soil small strain (HSS) model, and the soft soil (SS) model—to identify the most suitable model for the lacustrine deposit. To implement these models, the soil’s index properties and mechanical behavior were evaluated from undisturbed soil samples. The numerical simulatio
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6

Garel, Sylvain, Françoise Behar, Johann Schnyder, and François Baudin. "Palaeoenvironmental control on primary fluids characteristics of lacustrine source rocks in the Autun Permian Basin (France)." Bulletin de la Société géologique de France 188, no. 5 (2017): 29. http://dx.doi.org/10.1051/bsgf/2017187.

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The Autunian (Late Gzhelian-Sakmarian, ∼295 Ma) of the Autun Basin (Saône-et-Loire, France) is well known for its lacustrine oil-shales and boghead that were exploited during the 19th and 20th centuries. A study of the kerogen geochemistry, palynofacies, hydrocarbon (HC) distribution of pyrolysates and kinetics on these organic-rich sediments gave indications on the control of lacustrine primary fluid characteristics by palaeoenvironmental settings. Palynofacies results have shown a Botryococcus algae dominance in the boghead, whereas the oil-shales were dominated either by a mixing of terrest
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7

Adhikari, Ajay Raj, and Ananta Man Singh Pradhan. "Deformation analysis of foundation: a case study of Bir Hospital Trauma Centre, Kathmandu, Nepal." Journal of Nepal Geological Society 38 (September 25, 2008): 55–60. http://dx.doi.org/10.3126/jngs.v38i0.31481.

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The rapidly increasing population in the Kathmandu valley has demanded for the construction of multi-storeyed buildings. Such structures can be vulnerable to failures as they are constructed on soft fluvio-lacustrine sediments without detailed deformation analysis of their foundation. Hence, the Bir Hospital Trauma Centre is taken here as a case study for the deformation analysis. The settlement calculated by conventional test methods (e.g., oedometer test, compressibility index, etc.) are purely one dimensional and do not represent the actual value where lateral influence s are possible. For
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8

Guillemot, T., V. Bichet, A. Simonneau, et al. "Impact of Holocene climate variability on lacustrine records and human settlements in South Greenland." Climate of the Past Discussions 11, no. 6 (2015): 5401–38. http://dx.doi.org/10.5194/cpd-11-5401-2015.

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Abstract. Due to its sensitivity to climate changes, south Greenland is a particularly suitable area to study past global climate changes and their influence on locale Human settlements. A paleohydrological investigation was therefore carried out on two river-fed lakes: Lake Qallimiut and Little Kangerluluup, both located close to the Labrador Sea in the historic farming center of Greenland. Two sediment cores (QAL-2011 and LKG-2011), spanning the last four millennia, were retrieved and showed similar thin laminae, described by high magnetic susceptibility and density, high titanium and TOC /
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9

Sutton, Mark Q. "Cluster Analysis of Paleofecal Data Sets: A Test of Late Prehistoric Settlement and Subsistence Patterns in the Northern Coachella Valley, California." American Antiquity 63, no. 1 (1998): 86–107. http://dx.doi.org/10.2307/2694778.

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Data from human paleofecal samples can be used to address a variety of questions, primarily the reconstruction of diet, but also the analysis of nutrition, health, technology, and behavior Statistical analyses of constituents can be used to broaden the potential of paleofecal data, as well as to detail cuisine and to address larger issues of settlement/subsistence models. This potential is illustrated with a cluster analysis of paleofecal constituents from three late prehistoric period sites along the northern shore of ancient Lake Cahuilla, located in the Coachella Valley of southern Californ
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10

Brock, Andrea L. "Envisioning Rome’s Prehistoric River Harbor: An Interim Report from the Forum Boarium." Etruscan Studies 19, no. 1 (2016): 1–22. http://dx.doi.org/10.1515/etst-2016-0001.

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AbstractFollowing a brief discussion of the literature and intellectual history of Rome’s river port, this article presents preliminary results from a mechanized coring survey of the Forum Boarium valley. Conducted in 2015, this survey produced empirical evidence on prehistoric human activity Rome’s floodplain and acquired substantial data on the paleolandscape of the region, including the shifting position of the Tiber River and the discovery of lacustrine deposits in the valley. Additionally, consideration is given to the advantages and limitations posed by the natural landscape during the o
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11

Erlandson, Jon M. "The Role of Shellfish in Prehistoric Economies: A Protein Perspective." American Antiquity 53, no. 1 (1988): 102–9. http://dx.doi.org/10.2307/281156.

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In many prehistoric economies where plant foods supplied a majority of caloric requirements, shellfish may have served as a protein staple, at least on a seasonal basis. This hypothesis is supported with an archaeological example from coastal California, experimental data on shellfish protein yields in southeast Alaska, and review of two previous studies of the economics of shellfish exploitation (Osborn 1977; Parmalee and Klippel 1974). Evaluating the dietary role of shellfish from a protein perspective may have a profound effect on the reconstruction of settlement and subsistence strategies
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12

Colorado-Urrea, G., Y. D. Gonzalez, H. Wang, D. Zapata-Medina, and J. Carranza-Argote. "Rigid inclusions performance as ground improvement for lacustrine clays." IOP Conference Series: Earth and Environmental Science 1336, no. 1 (2024): 012008. http://dx.doi.org/10.1088/1755-1315/1336/1/012008.

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Abstract The Bogotá urban railway system involves constructing a rail maintenance yard covering 33 ha near the Bogotá River. It requires the construction of a 4.1 m embankment to overcome flood risks. Approximately 57,000 rigid inclusions (RI) were installed because of poor soil conditions to control excessive settlement. The embankment and RI were placed on a lacustrine deposit comprising layers with high organic matter content and soft clays that extended up to 200 m below ground surface. The effects of RI installation were reviewed using an inclinometer and benchmark data. Proof static load
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13

Wattinne, Aurélia, Emmanuelle Vennin, and Patrick De Wever. "Evolution of carbonated, lacustrine environment, with stromatolites : a paleoecological approach (quarry of Montaigu-le-Blin, Limagne graben, Allier, France)." Bulletin de la Société Géologique de France 174, no. 3 (2003): 243–60. http://dx.doi.org/10.2113/174.3.243.

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Abstract The Aquitanian deposits of the quarry of Montaigu-le-Blin, located in the ≪ Limagne bourbonnaise », are characterized by lacustrine marl and limestone alternations. They display well-developed vegetal and fauna associations. The sedimentary deposits show an environment which allowed settlement of fresh water fauna. The deposits reveal variations of the water level and consequently of the water chemistry. These variations are characterized by alternations of anoxic and oxidizing lacustrine environments, which are due to periodic climatic changes (alternating more or less humid periods)
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14

Vasil'chuk, Yurij Kirillovich, Jessica Yur'evna Vasil'chuk, Anna Dmitrievna Belik, Alexander Pavlovich Ginzburg, Nadine Arkad'evna Budantseva, and Alla Constantinovna Vasil'chuk. "Cryogenic soils near the Yeletsky settlement, northeast of the Komi Republic." Арктика и Антарктика, no. 4 (April 2020): 51–79. http://dx.doi.org/10.7256/2453-8922.2020.4.34011.

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The subject of this research is the soils and soil-geochemical catenae in the area of Yeletsky settlement, located in the northeast of the Komi Republic. Catena were deposited on the mound covered with moss-shrub tundra transect from the interfluve of Usa and Yelets Rivers to a lacustrine depression, complicated by arching permafrost mounds. Within the district of research, the authors laid five soil incisions (EL20-P1, EL20-P2, EL20-P3, EL20-P4 and EL20-P5) that formed a soil-geochemical catena along the slope. Complex land cover found at the periphery. The explored soils were formed on silty
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15

Mountjoy, Joshu J., Xiaoming Wang, Susi Woelz, et al. "Tsunami hazard from lacustrine mass wasting in Lake Tekapo, New Zealand." Geological Society, London, Special Publications 477, no. 1 (2018): 413–26. http://dx.doi.org/10.1144/sp477.21.

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AbstractLacustrine-tsunami risk from landslides can be significant yet for most locations globally the hazard remains unquantified. Lake Tekapo, in the tectonically active mountain belt of New Zealand's South Island, has been chosen to develop surveying and modelling techniques to assess the hazard from landslide tsunamis. Lake Tekapo is ideal for this study due to the high sedimentation rates, steep surrounds and the proximity to active faulting that indicate a high landslide potential. The shoreline tourist settlement and hydropower infrastructure mean the impact of any tsunami could be sign
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16

Grimley, David A., Ashley S. Lynn, Colby W. Brown, and Neal E. Blair. "Magnetic Fly Ash as a Chronological Marker in Post-Settlement Alluvial and Lacustrine Sediment: Examples from North Carolina and Illinois." Minerals 11, no. 5 (2021): 476. http://dx.doi.org/10.3390/min11050476.

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Fly ash consists of mainly silt-size spherules that form during high-temperature coal combustion, such as in steam locomotives and coal-burning power plants. In the eastern USA, fly ash was distributed across the landscape atmospherically beginning in the late 19th century, peaking in the mid-20th century, and decreasing sharply with implementation of late 20th century particulate pollution controls. Although atmospheric deposition is limited today, fly ash particles continue to be resedimented into alluvial and lacustrine deposits from upland soil erosion and failure of fly ash storage ponds.
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17

Толстобров, Дмитрий Сергеевич, Алена Николаевна Толстоброва, Василий Васильевич Колька, et al. "PUTATIVE RECORDS OF THE HOLOCENE TSUNAMI IN LACUSTRINE BOTTOM SEDIMENTS NEAR THE TERIBERKA SETTLEMENT (KOLA PENINSULA, RUSSIA)." Proceedings of the Karelian Research Centre of the Russian Academy of Sciences, no. 9 (September 27, 2018): 92. http://dx.doi.org/10.17076/lim865.

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18

Harzhauser, M., O. Mandic, A. K. Kern, et al. "Explosive demographic expansion by dreissenid bivalves as a possible result of astronomical forcing." Biogeosciences 10, no. 12 (2013): 8423–31. http://dx.doi.org/10.5194/bg-10-8423-2013.

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Abstract. Human induced range expansions of invasive dreissenid bivalves are of great concern. However, the underlying biological processes are only poorly understood, partly due to the lack of information on natural expansion events. Here we use the extinct bivalve species Sinucongeria primiformis as a model organism for testing natural (i.e. pre-Anthropocene) blooms of dreissenid species in a lacustrine system of Lake Pannon during the Tortonian (~ 10.5 Myr; late Miocene). A total of 600 samples from a consecutive core were evaluated for the relative abundance of this pavement-forming mollus
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19

Harzhauser, M., O. Mandic, A. K. Kern, et al. "Explosive demographic expansion by dreissenid bivalves as a possible result of astronomical forcing." Biogeosciences Discussions 10, no. 7 (2013): 12009–27. http://dx.doi.org/10.5194/bgd-10-12009-2013.

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Abstract. Human induced range expansions of invasive dreissenid bivalves are of great concern. However, the underlying biological processes are only poorly understood, partly due to the lack of information on natural expansion events. Here we use the extinct bivalve species Sinucongeria primiformis as a model organism for testing natural (i.e. non-Anthropocene) blooms of dreissenid species in a lacustrine system of Lake Pannon during the Tortonian (~10.5 Myr; Late Miocene). 600 samples from a consecutive core were evaluated for the relative abundance of this pavement-forming mollusc, which cov
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20

Précieux, Christian Behanzin, Agbandji Lucien, and Kouami Takpe Auguste. "Solid Waste Valorization and the Challenge of Social Representations in Ganvié, Benin." International Journal of Social Science and Human Research 08, no. 05 (2025): 2894–902. https://doi.org/10.5281/zenodo.15377946.

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Ganvié, a historic lacustrine settlement in southern Benin, faces growing environmental and public health challenges due to inadequate solid waste management. This article explores how local social representations of waste influence both the practices of disposal and emerging valorization strategies within this aquatic urban space. Drawing on qualitative fieldwork including interviews, participant observation, and discourse analysis this study highlights the ambivalent perceptions of waste among residents, shaped by historical, symbolic, and material factors. While plastic and synthetic
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21

Labarca, Rafael, Matías Frugone-Álvarez, Liz Vilches, et al. "Taguatagua 3: A new late Pleistocene settlement in a highly suitable lacustrine habitat in central Chile (34°S)." PLOS ONE 19, no. 5 (2024): e0302465. http://dx.doi.org/10.1371/journal.pone.0302465.

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We present the results of the excavations and analyses of the diverse and exceptional archaeological assemblage of Taguatagua 3, a new late Pleistocene site located in the ancient Tagua Tagua lake in Central Chile (34°S). The anthropogenic context is constrained in a coherently dated stratigraphic deposit which adds new information about the mobility, subsistence strategies, and settlement of the early hunter-gatherers of southern South America. The age model constructed, as well as radiocarbon dates obtained directly from a combustion structure, indicate that the human occupation occurred ove
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22

Labarca, Rafael, Matías Frugone-Álvarez, Liz Vilches, et al. "Correction: Taguatagua 3: A new late Pleistocene settlement in a highly suitable lacustrine habitat in central Chile (34°S)." PLOS ONE 19, no. 7 (2024): e0306861. http://dx.doi.org/10.1371/journal.pone.0306861.

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23

Gauthier, Emilie, Andrés Currás, Charly Massa, Typhaine Guillemot, Hervé Richard, and Vincent Bichet. "Late Holocene Environmental History and Norse Settlement in Outer Fjords from South Greenland: A Case Study at Lake Qallimiut." Geosciences 13, no. 4 (2023): 123. http://dx.doi.org/10.3390/geosciences13040123.

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To complement discussions about vegetation history and climate variations in south Greenland, especially during the Norse settlement, we developed a sedimentological multiproxy approach to study a 4300-year-old lacustrine core comprising pollen analysis, NPPs analysis, physical measurements (magnetic susceptibility, density, and grain size), and geochemical analyses (X-ray fluorescence, X-ray diffraction, and elemental analyses). Sediment archives were retrieved from a river-fed lake, Lake Qallimiut, located in the outer fjords of the Vatnahverfi area. The pollen analysis indicated a transitio
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24

Golovneva, L. B., and S. V. Shczepetov. "The late cretaceous flora from volcanogenic deposits of Northern Priokhotie (The Okhotsk-Chukotka volcanogenic belt)." Palaeobotany 2 (2011): 100–113. http://dx.doi.org/10.31111/palaeobotany/2011.2.100.

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The Karamken floristic assemblage occurs from basal layers of the Kholchan Formation of the Okchotsk-Chukotka volcanogenic belt (OCVB). The locality is situated at Khasyn River near Karamken settlement. The Karamken assemblage is composed of 6 taxa: Heilungia sp., Phoenicopsis ex gr. angustifolia Heer, Sphenobaiera sp., Metasequoia sp., Taxodium amguemensis (Efimova) Golovn., Trochodendroides sp. This flora is distinct from more ancient Arman flora and younger Ola flora. According to systematic composition the Karamken floristic assemblage is similar to the Chaun flora of Central Chukotka (the
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25

Erlandson, Jon M., and Madonna L. Moss. "The Systematic Use of Radiocarbon Dating in Archaeological Surveys in Coastal and Other Erosional Environments." American Antiquity 64, no. 3 (1999): 431–43. http://dx.doi.org/10.2307/2694143.

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Traditionally, archaeologists have used l4C dating primarily as a postexcavation analytical tool to establish the age of features, strata, or assemblages. In coastal zones and other environments around the world, however, thousands of archaeological sites are rapidly eroding or endangered by other destructive processes. We believe archaeologists should expand their use of l4C dating, systematically incorporating it into surveys in coastal, lacustrine, riverine, and other environments where erosional exposures often provide access to extensive stratigraphic profiles. With examples from the Paci
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26

Agatova, A. R., R. K. Nepop, L. B. Khazin, et al. "New chronological (14C, OSL), paleontological and geochemical data on developing of ice-dammed lakes in Kurai basin (south-eastern part of the Russian Altai) during the MIS-2." Доклады Академии наук 488, no. 3 (2019): 319–22. http://dx.doi.org/10.31857/s0869-56524883319-322.

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One of the highly debatable issue of the Altai Pleistocene paleogeography is the chronology and extension of the last ice-dammed lakes. For the first time paleontological, mineralogical characteristics, and optically stimulated luminescence (OSL) ages for lacustrine deposits confirm accumulation of ice-dammed lake with depth at least 170 m in Kurai basin at the end of the Late Pleistocene - 16-19 ka. New data provide information about the ecology and evolution of this Sartan reservoir. Draining of this lake less affected the topography in comparison with earlier cataclysmic glacier-lakes outbu
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27

Yoko, Sugiura, Zepeda Elizabeth, Pérez Carmen, and Kabata Shigeru. "El desarrollo de un asentamiento lacustre en la cuenca alta del río Lerma: el caso de Santa Cruz Atizapán, México central." Arqueologia Iberoamericana 5 (March 31, 2010): 5–22. https://doi.org/10.5281/zenodo.1308896.

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El valle de Toluca se localiza en la cuenca hidrológica Lerma-Chapala-Santiago, la más extensa de la República Mexicana. A lo largo de su milenaria historia, ha sido reconocido por ser una región donde se encuentran tres ciénagas (Chignahuapan, Chimaliapan y Chicnahuapan), circundadas por volcanes y densos bosques además del río Lerma. La riqueza ambiental de este frío valle favoreció la temprana ocupación de la región, cuyas evidencias arqueológicas se remontan, por lo menos, hasta hace más de 3000 a&nt
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28

Roffet-Salque, Mélanie, Arkadiusz Marciniak, Paul J. Valdes, et al. "Evidence for the impact of the 8.2-kyBP climate event on Near Eastern early farmers." Proceedings of the National Academy of Sciences 115, no. 35 (2018): 8705–9. http://dx.doi.org/10.1073/pnas.1803607115.

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The 8.2-thousand years B.P. event is evident in multiple proxy records across the globe, showing generally dry and cold conditions for ca. 160 years. Environmental changes around the event are mainly detected using geochemical or palynological analyses of ice cores, lacustrine, marine, and other sediments often distant from human settlements. The Late Neolithic excavated area of the archaeological site of Çatalhöyük East [Team Poznań (TP) area] was occupied for four centuries in the ninth and eighth millennia B.P., thus encompassing the 8.2-thousand years B.P. climatic event. A Bayesian analys
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29

Guo, Wei, Shiguang Xu, Tuo Hong, Shaolei Hao, and Gang Chen. "Study of Structural and Compression Properties of Soft Soils in Kunming at Different Moisture Contents." Shock and Vibration 2023 (September 26, 2023): 1–10. http://dx.doi.org/10.1155/2023/8618546.

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The structure of soil refers to the properties and arrangement of soil particles and pores, as well as their interactions, which have a significant impact on the mechanical behavior of soil. Clarifying the strengths and weaknesses of soil structure can effectively ensure engineering safety during designing. In this study, the structural soft soil in the Wujiaba area of Kunming City was studied. A comprehensive structural parameter γ was proposed by analyzing one-dimensional consolidation test data, which consider both the moisture content and yield stress. Due to its high moisture content and
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30

Belyakov, Vladimir, and Alexsandra Kuporova. "On Peat Production Capacity in Verkhoyansky District, Sakha (Yakutia) Republic." E3S Web of Conferences 41 (2018): 01047. http://dx.doi.org/10.1051/e3sconf/20184101047.

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The article analyzes the possible substitution of long-range coal with peat fuel in boilerhouses of Batagai settlement, the Sakha (Yakutia) Republic, and technical and ecological problems that arise. Potential in-situ resources for permafrost production of moulded solid fuel with peat are examined. The study introduces two options of peat fuel production for boilerhouses: peat milling and sod peat moulding. Experimental work on sod peat drying shows that sod peat can be cut and dried to the conditioned moisture content in northern Yakutia but it is inexpedient both technologically and ecologic
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31

Tolmie, Clare, and John M. Lambert. "The Lake Effect: Lake Michigan, Landscape Evolution, and the Archaeological Record of the Chicago Region." Midcontinental Journal of Archaeology 49, no. 1 (2024): 3–24. http://dx.doi.org/10.5406/23274271.49.1.02.

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Abstract Lake Michigan continues to have a major impact on the environment in the Chicago region, and changes in lake levels were a major driver of landscape evolution throughout the late Pleistocene and Holocene. Fluctuating lake levels reduced or increased the extent and character of terrestrial resources. The landscape has also been altered by erosional and aggradational processes from near-shore currents and wave action. Interpretation of archaeological site and settlement patterns in this region requires an understanding of the factors that have shaped and continue to shape this landscape
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32

Yang, Jiangqiang, Wei Zhang, Zhijiu Cui, Chaolu Yi, Yixin Chen, and Xiangke Xu. "Climate change since 11.5 ka on the Diancang Massif on the southeastern margin of the Tibetan Plateau." Quaternary Research 73, no. 2 (2010): 304–12. http://dx.doi.org/10.1016/j.yqres.2009.11.004.

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The Diancang Massif is located in a region linking the Tibetan and Yungui Plateaus. Climatically, it is in a transition belt between the south and middle subtropical zones, controlled by Indian monsoon and westerlies. Thus, this study provides more evidences on the evolution of Indian monsoon since the Holocene. We reconstruct the history of climate on the Diancang Massif since 11.5 ka, using integrated correlation of glacial activities, early human settlement sites, and climate proxies abstracted from variations in grain size, magnetic susceptibility, geochemical composition, and pollen in la
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33

Quintana Krupinski, Nadine B., Jennifer R. Marlon, Ami Nishri, Joseph H. Street, and Adina Paytan. "Climatic and human controls on the late Holocene fire history of northern Israel." Quaternary Research 80, no. 3 (2013): 396–405. http://dx.doi.org/10.1016/j.yqres.2013.06.012.

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Long-term fire histories provide insight into the effects of climate, ecology and humans on fire activity; they can be generated using accumulation rates of charcoal and soot black carbon in lacustrine sediments. This study uses both charcoal and black carbon, and other paleoclimate indicators from Lake Kinneret (Sea of Galilee), Israel, to reconstruct late Holocene variations in biomass burning and aridity. We compare the fire history data with a regional biomass-burning reconstruction from 18 different charcoal records and with pollen, climate, and population data to decipher the relative im
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34

Sten, Erik, Hans Thybo, and Nanna Noe Nygaard. "Resistivity and georadar mapping of lacustrine and glaciofluvial sediments in the late-glacial to postglacial Store Amose basin, Denmark." Bulletin of the Geological Society of Denmark 43 (July 14, 1996): 87–98. http://dx.doi.org/10.37570/bgsd-1996-43-10.

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Resistivity profiling, resistivity sounding, georadar profiling and analyses of borings are used in a sedimentological and geomorphological study of shallow subsurface deposits in the proximal (southeastern) part of the Store Amose lacustrine basin in eastern Denmark. Areas of low, intermediate and high resistivities are located by resistivity profiling. Low-resistivity areas (type I) correspond to a thick unit of water-saturated lake sediments (fine detritus gyttja and siltlclay) which were deposited in a large lake system from the late Weichselian to the late Holocene. In intermediate-resist
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35

Harning, David J., Christopher R. Florian, Áslaug Geirsdóttir, et al. "High-resolution Holocene record based on detailed tephrochronology from Torfdalsvatn, north Iceland, reveals natural and anthropogenic impacts on terrestrial and aquatic environments." Climate of the Past 21, no. 4 (2025): 795–815. https://doi.org/10.5194/cp-21-795-2025.

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Abstract. Open questions remain around the Holocene variability of climate in Iceland, including the relative impacts of natural and anthropogenic factors on Late Holocene vegetation change and soil erosion. The lacustrine sediment record from Torfdalsvatn, north Iceland, is the longest known in Iceland (∼ 12 000 cal yr BP), and along with its high sedimentation rate, it provides an opportunity to develop high-resolution quantitative records that address these challenges. In this study, we use two sediment cores from Torfdalsvatn to construct a detailed age model derived from marker tephra lay
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36

Gibaja, Juan F., Bogdana Milić, Angeliki Kita, Tasos Bekiaris, Niccolò Mazzucco, and Kostas Kotsakis. "The lacustrine settlement of Dispilio (Lake Kastoria, Northern Greece): An approach to economic and craft activities through a functional study of lithic tools." Journal of Archaeological Science: Reports 63 (May 2025): 105091. https://doi.org/10.1016/j.jasrep.2025.105091.

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37

Tolstobrova, A., O. Korsakova, and D. Tolstobrov. "The late-glacial — Holocene stratigraphy of bottom sediments from small isolated lakes in the Barents Sea coast (Kola region)." Vestnik of geosciences, no. 6 (August 12, 2022): 26–37. http://dx.doi.org/10.19110/geov.2022.6.3.

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Lithological study and diatom analysis of the bottom sediments from small lakes belonging to the category of isolated basins located on the Barents Sea coast of the Kola region was carried out. Stratigraphic subdivision of depositional sequences was performed based on the new data obtained from the Settlement Teriberka area, as well as on the published data from other areas; lithostratigraphic units (LSU), which are stratogens, were identified in them. We found out that the proglacial reservoir was marine during deglaciation on the Barents Sea coast, freshwater (LSU 1) sediments of the ice-mar
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38

Lespez, Laurent, Arthur Glais, José-Antonio Lopez-Saez, et al. "Middle Holocene rapid environmental changes and human adaptation in Greece." Quaternary Research 85, no. 2 (2016): 227–44. http://dx.doi.org/10.1016/j.yqres.2016.02.002.

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Numerous researchers discuss of the collapse of civilizations in response to abrupt climate change in the Mediterranean region. The period between 6500 and 5000 cal yr BP is one of the least studied episodes of rapid climate change at the end of the Late Neolithic. This period is characterized by a dramatic decline in settlement and a cultural break in the Balkans. High-resolution paleoenvironmental proxy data obtained in the Lower Angitis Valley enables an examination of the societal responses to rapid climatic change in Greece. Development of a lasting fluvio-lacustrine environment followed
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Сорокин, А. Н., А. В. Панин, А. Л. Смирнов, В. Н. Карманов, В. В. Морозов, and Н. Н. Солодков. "INITIAL DEVELOPMENT OF THE ZABOLOTYE REGION BASED ON THE RECENT GEOARCHAEOLOGICAL STUDIES." Краткие сообщения Института археологии (КСИА), no. 265 (March 12, 2021): 45–60. http://dx.doi.org/10.25681/iaras.0130-2620.265.45-60.

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В 2018 г. были возобновлены геоархеологические исследования в котловине Заболотского палеоозера (Московская область) - одного из реликтов территории Дубнинской низменности. В процессе трехлетних работ был выполнен значительный объем изысканий, приведших к радикальному пересмотру представлений о развитии геоморфологической обстановки изучаемого региона. Было установлено, что в течение последней (валдайской) ледниковой эпохи на этой территории господствовали не озерные, как считалось ранее, а аллювиальные условия рельефогенеза. Обстановка речных пойм с обилием возвышенных, редко затапливаемых ме
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40

Bazarova, B. B., A. P. Kuklin, I. E. Mikheev, et al. "Biodiversity of a small water body during the initial filling phase (the Amazar River of the Amur River Basin, Russia)." IOP Conference Series: Earth and Environmental Science 895, no. 1 (2021): 012008. http://dx.doi.org/10.1088/1755-1315/895/1/012008.

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Abstract In 2017, for the purposes of the Pulp and Saw Mill (PSM) “Polyarnaya”, the spillover dam was constructed on the Amazar River, a left tributary of the Amur River. Upon completion of the dam construction, the waters of the river formed a small river reservoir PSM “Polyarnaya”. This work covers findings on components and quantities of the newly formed reservoir at its initial stage and the data on biodiversity of its feeding flows. At this stage, the species composition of the flora and fauna in the reservoir falls in between the lacustrine and the riverine ones. The riverine conditions
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41

Krueger, Andrea M., and Francine M. G. McCarthy. "Great Canadian Lagerstätten 5. Crawford Lake – A Canadian Holocene Lacustrine Konservat-Lagerstätte with Two-Century-Old Viable Dinoflagellate Cysts." Geoscience Canada 43, no. 2 (2016): 123. http://dx.doi.org/10.12789/geocanj.2016.43.086.

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In addition to commonly preserved microfossils like pollen and diatoms, the varved sediments of Crawford Lake, Ontario, contain the fossilized remains of otherwise rare microfossils. Bottom water anoxia resulted from the physiography of this small, deep lake and enhanced biochemical oxygen demand (BOD) during two distinct phases of human settlement: prehistoric Iroquoian (approximately 1268–1486 CE) and historic Euro-Canadians (since 1822 CE). The exceptional preservation of delicate organic-walled microfossils like rotifer loricae and cellulosic dinoflagellate thecae provides unparalleled ins
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42

Unkelbach, Julia, Kaoru Kashima, Gaadan Punsalpaamuu, Lyudmila Shumilovskikh, and Hermann Behling. "Decadal high-resolution multi-proxy analysis to reconstruct natural and human-induced environmental changes over the last 1350 cal. yr BP in the Altai Tavan Bogd National Park, western Mongolia." Holocene 30, no. 7 (2020): 1016–28. http://dx.doi.org/10.1177/0959683620908662.

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The ‘Altai Tavan Bogd’ National Park in the north-western part of the Mongolian Altai, Central Asia, is located in a forest-steppe ecosystem. It occurs under the influence of extreme continental and montane climate and is sensitive to natural and anthropogenic impacts. High-resolution (<20 years per sample) multi-proxy data of pollen, non-pollen palynomorphs (NPPs), macro-charcoal, diatoms, and XRF scanning from radiocarbon-dated lacustrine sediments reveal various environmental changes and the impact of different settlement periods for the late-Holocene. From 1350 to 820 cal. yr BP (AD 600
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43

Platzman, ES, and SP Lund. "High-resolution environmental magnetic study of a Holocene sedimentary record from Zaca Lake, California." Holocene 29, no. 1 (2018): 17–25. http://dx.doi.org/10.1177/0959683618804636.

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Mineral magnetic studies of Holocene lake sediments recovered from Zaca Lake, in coastal southern California have yielded a 3000-year high-resolution record of terrestrial hydrologic variability and paleolimnology. Samples for magnetic analysis were obtained from an 8.73 m core recovered from the central region of Zaca Lake. Ages, constrained using a combined paleomagnetic and radiocarbon chronostratigraphy, yield sedimentation rates of 2–10 mm/yr with an average rate of 3 mm/yr over the 3000-year interval. Parameters reflecting decadal-scale variability in magnetic concentration (susceptibili
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44

Kramkowski, Mateusz. "Paleośrodowiskowe znaczenie zmian tempa i charakteru sedymentacji osadów jeziora Jelonek w Borach Tucholskich = Paleoenvironmental significance of changes in the rate and type of sedimentation in Lake Jelonek within Poland’s Tuchola Pine Forest (Bory Tucholskie)." Przegląd Geograficzny 92, no. 3 (2020): 409–22. http://dx.doi.org/10.7163/przg.2020.3.6.

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This paper presents the matter of the environmental reconstruction of laminated lacustrine sediments from the Younger Dryas through to the present day, in particular in respect of microlithofacial analysis and sedimentation rate. Lake Jelonek is located within the Tuchola Pine Forest of northern Poland (at 53°45’58N, 18°23’30E). It occupies a subglacial channel immediately adjacent to the Wda Valley. The lake covers 19.9 ha and has a maximum depth of 13.8 m. In 2014, overlapping sediment cores JEL14 (14.23 m) were collected from that deepest part, in order for a full sediment profile including
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45

Кренке, Н. А., Е. Г. Ершова, И. Н. Ершов, et al. "RADIOCARBON DATING OF ARCHAEOLOGICAL SITES AND NATURAL FEATURES IN THE SMOLENSK REGION IN 2014-2021." Краткие сообщения Института археологии (КСИА), no. 267 (October 4, 2022): 320–44. http://dx.doi.org/10.25681/iaras.0130-2620.267.320-344.

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В статье приведены результаты радиоуглеродного датирования археологических памятников и природных объектов (озерных и болотных отложений, погребенных почв), где производился антракологический и спорово-пыльцевой анализы. В качестве наиболее существенных результатов отмечаются следующие: 1) на Соборной горе в Смоленске выявлены остатки поселения культуры шнуровой керамики бронзового века, которому соответствует дата, указывающая на втор. пол. III тыс. до н. э.; 2) здесь же выявлен культурный слой поселения VII-IX вв. (видимо, древнейшего Смоленска русской летописи), датированного по серии образ
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46

Dembele, N'dji dit Jacques. "Quaternary fluvio-lacustrine environments and human settlements in West Africa." Past Global Change Magazine 23, no. 2 (2015): 76. http://dx.doi.org/10.22498/pages.23.2.76.

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47

Мазуркевич, А. Н., Е. В. Долбунова, В. В. Цыбрий, et al. "RESULTS OF NEW STUDIES OF EARLY NEOLITHIC LAYERS AT RAKUSHECHNYY YAR (ROSTOV REGION)." Краткие сообщения Института археологии (КСИА), no. 262 (November 15, 2021): 27–43. http://dx.doi.org/10.25681/iaras.0130-2620.262.27-43.

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Ракушечный Яр - уникальный стратифицированный памятник VII/VI тыс. до н. э. - раннего Средневековья - характеризуется сложной стратиграфией и палеорельефом, наличием погребенных почв и культурных слоев. Планомерные раскопки памятника проводились в 1960-1970 гг. и возобновлены в 2008 г. В результате комплексных археологических и геологических исследований выявлены особенности культурных слоев, позволившие выстроить микрохронологию этого памятника, где отдельные слои формировались за очень короткое время. Ракушечный Яр представляет свидетельства разновременного и последовательного заселения чело
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48

Pineda-Jaimes, Jorge Arturo, Cesar Augusto García-Ubaque, and Rodrigo Elías Esquivel-Ramírez. "Assessment of Geotechnical Hazard due to Deep Excavations in Bogota Clays: A Contribution for Sustainability in Urban Environments." Revista Facultad de Ingeniería 29, no. 54 (2020): e11373. http://dx.doi.org/10.19053/01211129.v29.n54.2020.11373.

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The development of resilient and sustainable cities considers the construction of infrastructure projects that involve deep excavations. During excavations, surface displacements frequently occur that may be inadmissible for previously constructed elements of the urban environment, threatening the sustainability of already consolidated sectors. In this article, we present an approximation to the estimation of the geotechnical hazard by deep excavations in soft lacustrine soils of Bogotá, DC, using parametric numerical simulations that sought to establish the probability of occurrence of base b
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49

Malnik, Valerii V., Masumi Yamamuro, Irina V. Tomberg, Elena V. Molozhnikova, Yuri S. Bukin, and Oleg A. Timoshkin. "Lacustrine, wastewater, interstitial and fluvial water quality in the Southern Lake Baikal region." Journal of Water and Health 20, no. 1 (2021): 23–40. http://dx.doi.org/10.2166/wh.2021.064.

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Abstract The coastal area of the southern Lake Baikal with the population over 35,000 people remains an attractive spot for both tourists and local residents. Despite high anthropogenic impact, a detailed assessment of water quality in this area has not been performed so far. Here, we performed a comprehensive evaluation of the quality of the surface, bottom and interstitial water in rivers, lacustrine water and wastewater in the southern Lake Baikal region. We analyzed 37 samples for the presence of fecal enterococci, Escherichia coli and assessed their hydrochemical parameters: concentration
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50

Billaud, Yves. "Sur les rives du lac du Bourget à la fin de l’âge du Bronze." Collection EDYTEM. Cahiers de géographie 20, no. 1 (2018): 317–31. http://dx.doi.org/10.3406/edyte.2018.1433.

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The archeological knowledge of the lake Le Bourget has long been limited to the lot of objects dredged with little regard for the context on the Late Bronze Age lakeside settlements during the second half of the 19th century. Underwater surveys over the past two decades have resulted in a review of the observations of precursors of underwater archeology and allow to clarify the area and the conservation status of the sites. On several of them, and contrary to what was conventionally accepted, thick sedimentary sequences are present. Stratigraphic excavations and tree-ring dating are used to de
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