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Journal articles on the topic 'Karstic infilling'

Author: Grafiati
Published: 7 June 2025
Last updated: 2 August 2025

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1

Fagoaga, Ana, Francisco Javier Molina, Vicente D. Crespo, César Laplana, Rafael Marquina, and Francisco J. Ruíz-Sánchez. "Geological context and micromammal fauna characterisation from the karstic infilling of La Pedrera (Albaida, Valencia, E Spain)." Spanish Journal of Palaeontology 32, no. 2 (2020): 241. http://dx.doi.org/10.7203/sjp.32.2.17042.

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2

Conrad, Georges, and Gérard Onoratini. "Le remplissage karstique de la grotte de l'Adaouste et sa genèse (Jouques, B.D.R) [The karstic infilling of Adaouste cave.]." Quaternaire 8, no. 2 (1997): 159–74. http://dx.doi.org/10.3406/quate.1997.1570.

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3

Sebe, Krisztina, Mihály Gasparik, Zoltán Szentesi, Gergely Surányi, Ágnes Novothny, and Luca Pandolfi. "New Pleistocene vertebrate assemblages from the Villány Hills (SW Hungary): Siklós and Palkonya." Fragmenta Palaeontologica Hungarica 38 (2023): 75–94. http://dx.doi.org/10.17111/fragmpalhung.2023.38.75.

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The Villány Hills in SW Hungary have the richest archive of Pliocene–Quaternary vertebrate faunas in the Pannonian Basin, mostly in karstic cavities. Here we present three new sites that extend the list of Pleistocene vertebrate locations for the area and add information to the evolution history of the region. In the northern part of the Siklós quarry, bone breccia was found coming from fissures in Jurassic or Cretaceous limestones. Its lithofacies and fossil content are similar to those of other well-known Plio-Pleistocene karst infills of the region. As it contained mostly snake vertebrae, i
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4

Camus, Hubert. "Caractérisation morphokarstique de l'Igue du Gral." Revue de Paléobiologie 43, no. 2 (2024): 107–49. https://doi.org/10.5281/zenodo.13860476.

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The Igue du Gral, as a largely vertical cavity, has functioned as a natural trap during several periods, and the distribution of the filling is linked to the opening and to the closing of entrance vents over time. The prolonged periods when it was closed allowed the good conservation of paleontological material, while the episodic karst functioning of the cavity was determined by the morpho-dynamic and climatic factors, both on the surface of the plateau and underground. The alternation of overture and closure controls the conditions of deposition, alteration, or degradation, particularly when
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5

Hodnett, John-Paul M., and David K. Elliott. "Carboniferous chondrichthyan assemblages from the Surprise Canyon and Watahomigi formations (latest Mississippian–Early Pennsylvanian) of the western Grand Canyon, Northern Arizona." Journal of Paleontology 92, S77 (2018): 1–33. http://dx.doi.org/10.1017/jpa.2018.72.

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AbstractTwo chondrichthyan assemblages of Late Mississippian/Early Pennsylvanian age are now recognized from the western Grand Canyon of northern Arizona. The latest Serpukhovian Surprise Canyon Formation has yielded thirty-one taxa from teeth and dermal elements, which include members of the Phoebodontiformes, Symmoriiformes, Bransonelliformes, Ctenacanthiformes, Protacrodontoidea, Hybodontiformes, Neoselachii (Anachronistidae), Paraselachii (Gregoriidae, Deeberiidae, Orodontiformes, and Eugeneodontiformes), Petalodontiformes, and Holocephali. The euselachian grade taxa are remarkably diverse
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Baqués, Vinyet, Estibalitz Ukar, Stephen E. Laubach, Stephanie R. Forstner, and András Fall. "Fracture, Dissolution, and Cementation Events in Ordovician Carbonate Reservoirs, Tarim Basin, NW China." Geofluids 2020 (April 18, 2020): 1–28. http://dx.doi.org/10.1155/2020/9037429.

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Ordovician carbonate rocks of the Yijianfang Formation in the Tabei Uplift, Tarim Basin, contain deeply buried (>6000 m), highly productive oil and gas reservoirs associated with large cavities (>10 m). Previous workers inferred that large cavities are paleocaves (paleokarst) formed near the surface and subsequently buried. Alternately, caves may have formed by dissolution at depth along faults. Using 227 samples from 16 cores, we document textures and cement compositions bearing on cavity histories with petrographic, high-resolution scanning electron microscopy (SEM), isotopic, and flui
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Mocochain, Ludovic, Philippe Audra, and Jean-Yves Bigot. "Base level rise and per ascensum model of speleogenesis (PAMS). Interpretation of deep phreatic karsts, vauclusian springs and chimney-shafts." Bulletin de la Société Géologique de France 182, no. 2 (2011): 87–93. http://dx.doi.org/10.2113/gssgfbull.182.2.87.

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Abstract In Mediterranean karsts, the Messinian salinity crisis induced first a deepening of the karst systems, then a flooding after the Pliocene transgression, and finally a reorganization of the drains after this base level rise. This reorganization mainly corresponds to the development of phreatic lifts: the chimney-shafts and the vauclusian springs. Such a per ascensum speleogenesis appears with a base level rise, which is caused by eustatism, by fluvial aggradation or valley infilling, or by continental subsidence. Consequently, we explain the origin of most of the deep phreatic cave sys
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8

Veress, Márton. "Postglacial evolution of paleodepressions in glaciokarst areas of the Alps and Dinarides." Zeitschrift für Geomorphologie 60, no. 4 (2016): 343–58. http://dx.doi.org/10.1127/zfg/2016/0331.

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The karstification of the paleodolines of glaciokarst is studied. Our methods included topographical mapping, geomorphological mapping and analysis, vertical electrical sounding (VES) measurements, areal imaging, investigation of the material of the superficial deposit. On glaciokarst, the paleodolines without cover are the bare karst patches, while paleodolines with cover belong to allogenic karst (if the cover is impermeable) or covered karst (if the cover is permeable). The covered karst also occur in patches, their pattern depends on the distribution of paleodolines, the size of glacier va
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9

Dobrowolski, Radosław, Marta Ziółek, Krystyna Bałaga, Jerzy Melke, and Andrij Bogucki. "Radiocarbon Age and Geochemistry of the Infillings of Small Closed Depressions from Western Polesie (Poland Se, Ukraine Nw)." Geochronometria 36, no. -1 (2010): 39–46. http://dx.doi.org/10.2478/v10003-010-0010-8.

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Radiocarbon Age and Geochemistry of the Infillings of Small Closed Depressions from Western Polesie (Poland Se, Ukraine Nw)In this paper we report the results of interdisciplinary investigations of deposits filling small closed depressions in the Western Polesie region. There were reconstructed the environmental changes and the main evolution phases of four morphometrically similar forms (=research sites) situated in the Lublin and Volhynia parts of the Polesie region. The gathered sedimentological, chronostratigraphical, palynological and geochemical data evidence great lithological (peats, g
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10

Jabrane, Oussama, Pedro Martínez-Pagán, Marcos A. Martínez-Segura, et al. "Integration of Electrical Resistivity Tomography and Seismic Refraction Tomography to Investigate Subsiding Sinkholes in Karst Areas." Water 15, no. 12 (2023): 2192. http://dx.doi.org/10.3390/w15122192.

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Operational and safety issues associated with subsiding sinkholes in karst areas start with the definition of fractures and joints, causing ground weakness. Conventional geotechnical boreholes and geological mapping must be complemented with indirect subsurface exploration techniques to detail those structures. This work aims to use electrical resistivity tomography (ERT) and seismic refraction tomography (SRT) near-surface geophysical techniques to infer the 2D and 3D geometry of sediment-infilled sinkholes formed by the conjunction of fractures and joints in karst areas. Geophysical surveys
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11

Bjørnerud, M. "Evidence for extensive post-Caledonian karst development in southwestern Spitsbergen." Geological Magazine 129, no. 4 (1992): 465–69. http://dx.doi.org/10.1017/s0016756800019543.

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AbstractProterozoic limestones at several localities in southwestern Spitsbergen contain karst-related features (layered clastic infillings, collapse breccias, deeply weathered depressions) which overprint the Caledonian deformational fabric in the rocks. These features apparently developedbetween middle Devonian and mid-Carboniferous time when the Precambrian basement complex stood high above sea level. Recognition of these karst features may shed light on depositional and tectonic events in post-Caledonian Spitsbergen.
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12

Dobrowolski, Radosław, and Stanisław Fedorowicz. "Glacial and Periglacial Transformation of Palaeokarst in the Lublin-Volhynia Region (Se Poland, NW Ukraine) on the Base of TL Dating." Geochronometria 27, no. -1 (2007): 41–46. http://dx.doi.org/10.2478/v10003-007-0012-3.

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Glacial and Periglacial Transformation of Palaeokarst in the Lublin-Volhynia Region (Se Poland, NW Ukraine) on the Base of TL Dating Distinctly diverse results of TL dating are obtained for the deposits with similar lithofacial features but filling morphologically differentiated karst palaeoforms (dolines, pipes, pockets). The infillings of dolines and pipes are mostly of the Saalian age. Based on sedimentological analysis, their formation conditions are related to sub- or/and terminoglacial environment. The age obtained for all infillings of pockets is underestimated in comparison with lithos
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13

Quinif, Yves, and Marc Legros. "Stratigraphy of the Lorette Cave (Rochefort, Belgium): Study of the “gours suspendus” section." Geologica Belgica 24, no. 3-4 (2021): 169–79. http://dx.doi.org/10.20341/gb.2021.005.

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The Lorette Cave contains a wide variety of deposits within various stratigraphical contexts. This cave is a part of the complex underground meander cut-off of the Wamme and Lomme rivers, between some swallow-holes along their two talwegs near On, Jemelle and Rochefort, and the general resurgence at Eprave. The Lorette Cave is embedded within the Givetian limestone formations of the Calestienne. This cave displays the first part with a labyrinthic structure. Some parts of the karstic network are affected by recent tectonic activity, which dislocates some galleries and provokes collapses. The s
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14

Kumarapeli, P. Stephen, Lao Kheang, Larry Hoy, and H. Pintson. "Chalcopyrite–bornite and chalcopyrite–bornite–barite in the Acton Vale Limestone, southeastern Quebec: mineralized shelf-margin slivers in a Taconian nappe." Canadian Journal of Earth Sciences 27, no. 1 (1990): 27–39. http://dx.doi.org/10.1139/e90-003.

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The Acton Vale limestone units of probable Early Ordovician age in the external nappe zone of the Appalachian foldbelt in southeastern Quebec host numerous occurrences of vein- and breccia-type copper deposits. Associated with these are two significant occurrences of barite: one at Upton consisting of a stratiform mass of probable economic potential; and the other at Lord Aylmer consisting of thin, tabular, karstic infillings of barite. Studies of the mineral occurrences at Acton Vale, Upton, and Lord Aylmer show that the mineralization is epigenetic and formed largely by open-space filling at
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15

James, J. M. "Burial and infilling of a karst in Papua New Guinea by road erosion sediments." Environmental Geology 21, no. 3 (1993): 144–51. http://dx.doi.org/10.1007/bf00775298.

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16

Husson, Eglantine, Michel Séranne, Pierre-Jean Combes, et al. "Marine karstic infillings: evidence of extreme base level changes and geodynamic consequences (Paleocene of Languedoc, south of France)." Bulletin de la Société Géologique de France 183, no. 5 (2012): 425–41. http://dx.doi.org/10.2113/gssgfbull.183.5.425.

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Abstract Late Jurassic platform carbonates of Languedoc (southern France) are deeply incised by Late Miocene canyons, allowing the observation of karst systems filled with sediments containing evidences of marine origin. Field and structural relationships as well as new biostratigraphic data (planktonic foraminifera and calcareous nannofossils) provide a Latest Cretaceous-Earliest Paleocene age for the major karstification and a Paleocene (Danian-Selandian) age for the sedimentary filling. The ≥ 350 m vertical extent of this karst system and its subsequent marine filling gives a minimum amplit
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17

North, Leslie A., Beynen Philip E. Van, and Mario Parise. "Interregional comparison of karst disturbance: West-central Florida and southeast Italy." Journal of Environmental Management 90, no. 5 (2009): 1770–81. https://doi.org/10.5281/zenodo.13511695.

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(Uploaded by Plazi for the Bat Literature Project) The karst disturbance index (KDI) consists of 31 environmental indicators contained within the five broad categories: geomorphology, hydrology, atmosphere, biota, and cultural. The purpose of this research is to apply the KDI to two distinct karst areas, west Florida, USA, and Apulia, Italy. Through its application, the utility of the index can be validated and other important comparisons can be made, such as differences in the karst legislations implemented in each region and the effect of time exposure to human occupation to each karst terra
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18

North, Leslie A., Beynen Philip E. Van, and Mario Parise. "Interregional comparison of karst disturbance: West-central Florida and southeast Italy." Journal of Environmental Management 90, no. 5 (2009): 1770–81. https://doi.org/10.5281/zenodo.13511695.

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(Uploaded by Plazi for the Bat Literature Project) The karst disturbance index (KDI) consists of 31 environmental indicators contained within the five broad categories: geomorphology, hydrology, atmosphere, biota, and cultural. The purpose of this research is to apply the KDI to two distinct karst areas, west Florida, USA, and Apulia, Italy. Through its application, the utility of the index can be validated and other important comparisons can be made, such as differences in the karst legislations implemented in each region and the effect of time exposure to human occupation to each karst terra
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19

North, Leslie A., Beynen Philip E. Van, and Mario Parise. "Interregional comparison of karst disturbance: West-central Florida and southeast Italy." Journal of Environmental Management 90, no. 5 (2009): 1770–81. https://doi.org/10.5281/zenodo.13511695.

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(Uploaded by Plazi for the Bat Literature Project) The karst disturbance index (KDI) consists of 31 environmental indicators contained within the five broad categories: geomorphology, hydrology, atmosphere, biota, and cultural. The purpose of this research is to apply the KDI to two distinct karst areas, west Florida, USA, and Apulia, Italy. Through its application, the utility of the index can be validated and other important comparisons can be made, such as differences in the karst legislations implemented in each region and the effect of time exposure to human occupation to each karst terra
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20

North, Leslie A., Beynen Philip E. Van, and Mario Parise. "Interregional comparison of karst disturbance: West-central Florida and southeast Italy." Journal of Environmental Management 90, no. 5 (2009): 1770–81. https://doi.org/10.5281/zenodo.13511695.

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(Uploaded by Plazi for the Bat Literature Project) The karst disturbance index (KDI) consists of 31 environmental indicators contained within the five broad categories: geomorphology, hydrology, atmosphere, biota, and cultural. The purpose of this research is to apply the KDI to two distinct karst areas, west Florida, USA, and Apulia, Italy. Through its application, the utility of the index can be validated and other important comparisons can be made, such as differences in the karst legislations implemented in each region and the effect of time exposure to human occupation to each karst terra
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21

Muhammad, Ros Fatihah, Tze Tshen Lim, Norliza Ibrahim, et al. "First discovery of Stegodon (Proboscidea) in Malaysia." Warta Geologi 46, no. 3 (2020): 196–98. http://dx.doi.org/10.7186/wg463202004.

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A cheek tooth of Stegodon, an extinct genus of Proboscidea, had been discovered in a cave in Gopeng, Perak. The discovery represents the first fossil of Stegodon ever found in Malaysia. Embedded in lithified cave infillings are the associated dental remains from at least three or four other different taxa of fossil mammals commonly found among Southeast Asian Pleistocene-Holocene faunas. The finding provides a unique chance for investigations into the evolution dynamics of Stegodon in this part of Southeast Asia and the species diversity of Proboscidea in prehistoric Peninsular Malaysia. Fossi
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Debard, Evelyne. "Les remplissages karstiques du Bas-Vivarais : karstogénèse, sédimentogénèse et archéologie [Karstic infillings of the Bas-Vivarais: kartogenesis, sedimentogenesis and archeology.]." Quaternaire 8, no. 2 (1997): 305–17. http://dx.doi.org/10.3406/quate.1997.1582.

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23

Turk, Janez. "Identification of depositional hiatuses in karst infillings – Example from Divje babe I cave (Slovenia)." Geologija 54, no. 1 (2011): 121–28. http://dx.doi.org/10.5474/geologija.2011.009.

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24

Matton, Guillaume, Michel Jébrak, and James K. W. Lee. "Resolving the Richat enigma: Doming and hydrothermal karstification above an alkaline complex." Geology 33, no. 8 (2005): 665–68. http://dx.doi.org/10.1130/g21542ar.1.

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Abstract The Richat structure (Sahara, Mauritania) appears as a large dome at least 40 km in diameter within a Late Proterozoic to Ordovician sequence. Erosion has created circular cuestas represented by three nested rings dipping outward from the structure. The center of the structure consists of a limestone-dolomite shelf that encloses a kilometer-scale siliceous breccia and is intruded by basaltic ring dikes, kimberlitic intrusions, and alkaline volcanic rocks. Several hypotheses have been presented to explain the spectacular Richat structure and breccia, but their origin remains enigmatic.
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25

Bassil, Joseph, Aude Naveau, Maïté Bueno, Moumtaz Razack, and Véronique Kazpard. "Leaching behavior of selenium from the karst infillings of the Hydrogeological Experimental Site of Poitiers." Chemical Geology 483 (April 2018): 141–50. http://dx.doi.org/10.1016/j.chemgeo.2018.02.032.

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26

Combes, Pierre-Jean, Bernard Peybernès, Marie-José Fondecave-Wallez, Michel Séranne, Jean-Luc Lesage, and Hubert Camus. "Latest-Cretaceous/Paleocene karsts with marine infillings from Languedoc (South of France); paleogeographic, hydrogeologic and geodynamic implications." Geodinamica Acta 20, no. 5 (2007): 301–26. http://dx.doi.org/10.3166/ga.20.301-326.

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27

Campy, Michel, Pierre Bintz, Jacques Evin, Henri Laville, and Jean Chaline. "Sedimentary record in french karstic infillings during the last climatic cycle [ Enregistrement sédimentaire dans les remplissages karstiques français au cours du dernier cycle climatique. ]." Quaternaire 5, no. 3 (1994): 157–63. http://dx.doi.org/10.3406/quate.1994.2027.

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28

Viehofen, Agnes, Christoph Hartkopf‐Fröder, and Else Marie Friis. "Inflorescences and Flowers ofMauldinia angustilobasp. nov. (Lauraceae) from Middle Cretaceous Karst Infillings in the Rhenish Massif, Germany." International Journal of Plant Sciences 169, no. 7 (2008): 871–89. http://dx.doi.org/10.1086/589975.

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29

Minwer-Bararat, Raef, Antonio García-Alix, Jordi Agustí, Elvira Martín Suárez, and Matthijs Freudenthal. "The micromammal fauna from Negratín-1 (Guadix Basin, southern Spain): new evidence of African-Iberian mammal exchanges during the Late Miocene." Journal of Paleontology 83, no. 6 (2009): 854–79. http://dx.doi.org/10.1666/09-009.1.

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A rich and diverse micromammal fauna from the late Turolian (MN13) locality of Negratín-1 (Guadix Basin, southern Spain) is described. The faunal list of this site includes Apodemus gudrunae, Occitanomys alcalai, Stephanomys dubari, Paraethomys meini, Myocricetodon jaegeri, Debruijnimys almenarensis, Apocricetus alberti, Ruscinomys sp., Eliomys sp., Atlantoxerus sp., Parasorex ibericus, and Soricidae indet. This is the most nearly complete mammal fauna from the Miocene of the Guadix Basin and allows precise correlations with localities from other Iberian areas. In addition, some of the taxa id
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Crégut-Bonnoure, Evelyne, Nicolas Boulbes, Emmanuel Desclaux, and Adrian Marciszak. "New Insights into the LGM and LG in Southern France (Vaucluse): The Mustelids, Micromammals and Horses from Coulet des Roches." Quaternary 1, no. 3 (2018): 19. http://dx.doi.org/10.3390/quat1030019.

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Coulet des Roches is a natural karst trap in Southern France. Its infilling dates back to the end of the Pleniglacial (Last Glacial Maximum, LGM) and the end of the Tardiglacial (Last Glacial, LG). Three mustelid species have been identified in this infilling: the common polecat (Mustela putorius, minimum number of individuals (MNI) = 4), the stoat (Mustela erminea, MNI = 14) and the weasel (Mustela nivalis, MNI = 48). The common polecat remains are metrically and morphologically indistinguishable from recent European specimens. The smallest mustelids are mainly represented by average-sized sp
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Peybernès, Bernard, Marie-José Fondecave-Wallez, Pierre-Jean Combes, and Michel Seranne. "Successive Paleocene and Eocene infillings of polyphase paleokarsts within the Cretaceous limestones of the Empordà thrust sheets (Catalan Pyrenees, Spain) : relationships between tectonics and karstification." Bulletin de la Société Géologique de France 178, no. 1 (2007): 15–24. http://dx.doi.org/10.2113/gssgfbull.178.1.15.

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Abstract The Mesozoic series of the southern units of the Pyrenean Empordà thrust sheets (Montgrí and Figueres nappes, Catalonia, Spain) were finally emplaced over the autochthonous basement and its Cenozoic cover during Eocene times. However, they have originally been folded by the “Laramian” compressional event (Late Cretaceous/Early Paleocene), while they were still in their root zone more than 50 km to the N-NE. Postdating the Santonian, the emersion of the Cretaceous tectorogen induced karst formation at the expense of Berriasian to Santonian limestone sequences. Karst cavities of this
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Combes, Pierre-Jean, Bernard Peybernès, Marie-José Fondecave-Wallez, Michel Séranne, Jean-Luc Lesage, and Hubert Camus. "Reply to comment on Latest-Cretaceous/Paleocene karsts with marine infillings from Languedoc (South of France) ; paleogeographic, hydrogeologic and geodynamic implications." Geodinamica Acta 21, no. 3 (2008): 139–43. http://dx.doi.org/10.3166/ga.21.139-143.

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Riggs, Alan C., W. J. Carr, Peter T. Kolesar, and Ray J. Hoffman. "Tectonic Speleogenesis of Devils Hole, Nevada, and Implications for Hydrogeology and the Development of Long, Continuous Paleoenvironmental Records." Quaternary Research 42, no. 3 (1994): 241–54. http://dx.doi.org/10.1006/qres.1994.1075.

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AbstractDevils Hole, in southern Nevada, is a surface collapse into a deep, planar, steeply dipping fault-controlled fissure in Cambrian limestone and dolostone. The collapse intersects the water table about 15 m below land surface and the fissure extends at least 130 m deeper. Below water, most of the fissure is lined with a >30-cm-thick layer of dense maxillary calcite that precipitated continuously from groundwater for >500,000 yr. The thick mammillary calcite coat implies a long history of calcite-supersaturated groundwaters, which, combined with the absence of dissolutional morpholo
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Gonzato, Guido, Enrico Borghi, Roberto Chignola, Nereo Preto, and Guido Rossi. "Paleokarst coastal caves at Torricelle Hills (Lessini Mountains, Venetian Prealps, Italy)." International Journal of Speleology 52, no. 2 (2023): 123–38. http://dx.doi.org/10.5038/1827-806x.52.2.2462.

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This paper describes a set of paleokarst caves at Torricelle Hills near Verona (Southern Alps, Italy.) At this locality, erosional surfaces and paleokarst cavities show that sedimentation of late Paleogene neritic limestones was interrupted by subaerial exposure. Karst features developed during a phase of marine regression that started after the early Oligocene and ended in the mid Miocene. These caves were originally completely filled by iron oxides- and hydrated oxides-rich paleosol sediments (ochre) that, for centuries, have been mined for pigments. Mining activity emptied the caves, leavin
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Mhanna, R., A. Naveau, M. Bueno, et al. "Concomitant behavior of arsenic and selenium from the karst infillings materials of the fractured carbonate Dogger Aquifer (Hydrogeological Experimental Site, Poitiers, France)." Chemosphere 275 (July 2021): 129935. http://dx.doi.org/10.1016/j.chemosphere.2021.129935.

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36

Kah, Linda C., Julie K. Bartley, Tracy D. Frank, and Timothy W. Lyons. "Reconstructing sea-level change from the internal architecture of stromatolite reefs: an example from the Mesoproterozoic Sulky Formation, Dismal Lakes Group, arctic Canada." Canadian Journal of Earth Sciences 43, no. 6 (2006): 653–69. http://dx.doi.org/10.1139/e06-013.

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The Mesoproterozoic Dismal Lakes Group, arctic Canada, contains a relatively thin, yet regionally extensive stromatolitic reef complex that developed subtidally during a major transgression, shoaled to sea level, and was overlain by intertidal to supratidal carbonate and evaporite strata. The September Lake reef complex exhibits a complex internal architecture that records the interaction between stromatolite growth and changes in accommodation space derived from both higher order (4th- or 5th-order, parasequence-scale) changes in sea level and the variable bathymetry of the sea floor. Reef gr
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Bilotte, Michel, Laurent Bruxelles, Joseph Canérot, Bernard Laumonier, and Régine Simon Coinçon. "Comment to “Latest-Cretaceous/Paleocene karsts with marine infillings from Languedoc (South of France); paleogeographic, hydrogeologic and geodynamic implications by P. J. Combes et al.”." Geodinamica Acta 20, no. 6 (2007): 403–13. http://dx.doi.org/10.3166/ga.20.403-413.

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Angelone, Chiara, Stanislav Čermák, Blanca Moncunill-Solé, et al. "Systematics and paleobiogeography of Sardolagus obscurus n. gen. n. sp. (Leporidae, Lagomorpha) from the early Pleistocene of Sardinia." Journal of Paleontology 92, no. 3 (2018): 506–22. http://dx.doi.org/10.1017/jpa.2017.144.

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AbstractThe extreme rareness of Sardinian fossil sites older than Middle and Late Pleistocene makes the Monte Tuttavista karst complex (E Sardinia, Italy) very important. Remarkable lagomorph material, recovered from several fissure infillings of Monte Tuttavista referable to the Capo Figari/Orosei 1 and Orosei 2 faunal sub-complexes (early Pleistocene, ~2.1/1.9–1.1 Ma), allowed us to describe a new endemic insular leporid, Sardolagus obscurus n. gen. n. sp. The new taxon is characterized by a peculiar combination of an advanced p3 (Lepus-type) and a primitive P2 lacking deep flexa. The origin
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Cílek, Václav. "Pískovcové převisy středních a severních Čech: jejich vznik, sedimenty a paleoantropologický význam." Lidé města 6, no. 1/13 (2004): 98–105. https://doi.org/10.14712/12128112.4356.

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The most important findings of the study of sandstone rockshelter and their infillings can be summarised as follows: 1. Genesis of rockshelters: The race of rockshelter formation under Holocene climatic conditions is low, because Mesolithic artefacts are often found in undisturbed layer 2-15 cm from the sandstone wall, thus che shape of many rockshelters has not changed much during last at least 9000 radiocarbon years. The destructive action of frost during ice ages seems to be responsible for the origin of majority rockshelters. The reservoir of capillary water is located either in more perme
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Angelucci, Diego E., Mariana Nabais, and João Zilhão. "Formation processes, fire use, and patterns of human occupation across the Middle Palaeolithic (MIS 5a-5b) of Gruta da Oliveira (Almonda karst system, Torres Novas, Portugal)." PLOS ONE 18, no. 10 (2023): e0292075. http://dx.doi.org/10.1371/journal.pone.0292075.

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Gruta da Oliveira features a c. 13 m-thick infilling that includes a c. 6.5 m-thick archaeological deposit (the “Middle Palaeolithic sequence” complex), which Bayesian modelling of available dating results places in MIS 5a (layers 7–14) and MIS 5b (layers 15–25), c. 71,000–93,000 years ago. The accumulation primarily consists of sediment washed in from the slope through gravitational processes and surface dynamics. The coarse fraction derives from weathering of the cave’s limestone bedrock. Tectonic activity and structural instability caused the erosional retreat of the scarp face, explaining
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Abdulsamad, E. O., and Mansour M. Elbabour. "Juliana Lake: A Wetland in an Urban Environment1." Libyan Journal of Science &Technology 7, no. 2 (2022): 65–72. http://dx.doi.org/10.37376/ljst.v7i2.2241.

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Of all the remaining natural habitats of Benghazi’s urban area (NE Libya), perhaps the most threatened are its karst lakes and coastal salt marshes (locally known as Sebkha). Juliana Lake stands out as one example of a fragile ecosystem that is steadily shrinking and exposed to dredging, infilling and, consequently, possible damage to its aquatic organisms, and the inevitable loss of its renowned biodiversity. Several 19th & 20th–century traveller’s sketches and maps, soil maps, photographs and satellite images provide the bases for change in the size and magnitude of the lake and its adja
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Pomel, Simon, and Richard Maire. "Exemple d'enregistrement des changements climatiques et de l'anthropisation dans les remplissages endokarstiques de Chine centrale (Hubei) [Climatic changes and human impact recorded in the karst infillings of central China (Hubei)]." Quaternaire 8, no. 2 (1997): 119–28. http://dx.doi.org/10.3406/quate.1997.1566.

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Pérez-Cano, Jordi, Alejandro Gil-Delgado, Oriol Oms, and Ramon Mercedes-Martín. "Paleoenvironmental constraints influencing charophyte communities in an Early Cretaceous Karstic Lake, La Pedrera de Meià Konservat-Lagerstätte (Southern Pyrenees): combining geochemical and palaeoecological analyses." Facies 71, no. 1 (2025). https://doi.org/10.1007/s10347-024-00696-9.

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AbstractThe combined sedimentological and palaeoecological analysis of charophyte-rich carbonate microfacies is proven to be a useful methodology for the palaeoenvironmental reconstruction of continental settings. However, the integration of these charophyte assemblages with geochemical proxies has not been explored, yet. In the present work, the charophyte-rich muddy carbonates of the Barremian La Pedrera de Meià Konservat-Lagerstätte (Southern Pyrenees, Spain) were studied from a taxonomic, taphonomic, and palaeoecological viewpoint, and the results were later integrated with previously publ
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Carter, Terry R., Stéphanie Larmagnat, Shuo Sun, Philippe Letellier, and Hazen A. J. Russell. "Caractérisation de la porosité avec la technique d’imagerie médicale CT-scan de deux aquifères paléokarstiques profondément enfouis situés dans les carbonates du Silurien, sud Ontario, Canada." Hydrogeology Journal, September 5, 2023. http://dx.doi.org/10.1007/s10040-023-02668-9.

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AbstractPaleokarst and paleokarst aquifers are not as well-documented as shallow karst, and studies of pores and pore networks are rare. Paleokarst lacks the open conduits typical of karst due to compaction, infilling, and diagenetic recrystallization by deep burial, so groundwater movement is through matrix porosity. In this case study, porosity networks in two saline aquifers in carbonate paleokarst of the Silurian Guelph Formation and Salina A-1 Carbonate Unit in southern Ontario (Canada) have been studied in drill cores at microscopic to macroscopic scales, utilizing medical computed tomog
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Baldermann, Andre, Florian Mittermayr, Stefano M. Bernasconi, et al. "Fracture dolomite as an archive of continental palaeo-environmental conditions." Communications Earth & Environment 1, no. 1 (2020). http://dx.doi.org/10.1038/s43247-020-00040-3.

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Abstract The origin of Quaternary dolomites in continental environments (e.g. karst and lakes) is barely constrained compared to marine dolomites in sedimentary records. Here we present a study of dolomite and aragonite formations infilling young fractures of the ‘Erzberg’ iron ore deposit, Austria, under continental-meteoric and low temperature conditions. Two dolomite generations formed shortly after the Last Glacial Maximum (~20 kyr BP): dolomite spheroids and matrix dolomite. Clumped isotope measurements and U/Th disequilibrium ages reveal formation temperatures of 0–3 °C (±6 °C) and 3–20
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Simoneit, Bernd R. T., Daniel R. Oros, Angelika Otto, Christoph Hartkopf-Fröder, and Volker Wilde. "Terpenoids in resinites from middle Cretaceous karst infillings in the Rhenish Massif (Rhineland, Germany): botanical source and preservation." International Journal of Earth Sciences, September 27, 2023. http://dx.doi.org/10.1007/s00531-023-02351-0.

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Simoneit, Bernd R. T., Daniel R. Oros, Angelika Otto, Christoph Hartkopf-Fröder, and Volker Wilde. "Correction: Terpenoids in resinites from middle Cretaceous karst infillings in the Rhenish Massif (Rhineland, Germany): botanical source and preservation." International Journal of Earth Sciences, November 29, 2023. http://dx.doi.org/10.1007/s00531-023-02358-7.

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48

Stratford, Dominic, Laurent Bruxelles, J. Francis Thackeray, Travis R. Pickering, and Sophie Verheyden. "Comments on ‘U-Pb dated flowstones restrict South African early hominin record to dry climate phases’ (Pickering et al. Nature 2018;565:226–229)." South African Journal of Science 116, no. 3/4 (2020). http://dx.doi.org/10.17159/sajs.2020/7094.

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Pickering et al. (Nature 2018;565:226–229) utilised calcium carbonate flowstone deposits (i.e. speleothems) from eight Pliocene and Pleistocene South African Cradle of Humankind cave sites to propose that biases were created within the fossil record due to absent clastic sedimentation phases during wet periods, when caves were closed and only speleothems accumulated. Such a scenario has significant implications for our understanding of variability in hominin mobility, resource exploitation, functional repertoires and interactions with competitors in changing environmental and ecological contex
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Yang, Mengying, Xiucheng Tan, Fang Xu, et al. "Controlling factors and evolution of reservoirs in continental rift lacustrine carbonate factory: insight from the cretaceous ITP-BVE formation in Brazil’s Santos Basin." Frontiers in Earth Science 13 (March 27, 2025). https://doi.org/10.3389/feart.2025.1551406.

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The Cretaceous Itapema and Barra Velha Formations in Brazil’s Santos Basin represent a rare giant rift lacustrine carbonate factory with considerable potential for oil and gas exploration. Through a comprehensive petrological and petrophysical analysis of field A in Santos Basin, this study clarifies the reservoir properties and distribution of this lacustrine carbonate facies and further investigates the controlling factors and differential evolution of lacustrine carbonate reservoirs. The main research results are as follows: (1) The Itapema Formation is characterized by bioclastic limestone
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