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Journal articles on the topic 'Palaeoecological reconstruction'

Author: Grafiati

Published: 24 April 2022

Last updated: 30 July 2025

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1

Fortelius, Mikael, Peter Myrdal, and Indre Zliobaite. "The best of all possible coexistence." Palaeobiodiversity and Palaeoenvironments 101, no. 1 (2021): 259–65. http://dx.doi.org/10.1007/s12549-020-00468-7.

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AbstractThe writings of Gottfried Wilhelm Leibniz (1646–1716) provide a window on early evolutionary thinking of a kind interestingly different from the roots of modern evolutionary theory as it emerged in the years following the French Revolution. Here we relate aspects of Leibniz’s thinking to methods of modern palaeoecology and show that, despite a different terminology and a different hierarchic focus, Leibniz emerges as a strikingly modern theoretician, who viewed the living world as dynamic and capable of adaptive change. The coexistence approach of palaeoecological reconstruction, devel

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2

Qader, Waseem, Showkat Hamid Mir, Julia Meister, Reyaz Ahmad Dar, Marco Madella, and Irfan Rashid. "Sedimentological perspective on phytolith analysis in palaeoecological reconstruction." Earth-Science Reviews 244 (September 2023): 104549. http://dx.doi.org/10.1016/j.earscirev.2023.104549.

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3

FERGUSON, Crystal, and Florin PENDEA. "Identifying glacio–isostatic rebound processes using testate amoeba as palaeohydrological proxies; a case study from subarctic Québec, Canada." Revista de Geomorfologie 20, no. 1 (2018): 5–16. http://dx.doi.org/10.21094/rg.2018.008.

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Glacio–isostatic rebound is one of the most important landscape processes affecting the northern and northeastern coast of Canada and, therefore, reconstruction of postglacial rebound rates is critical for a better understanding of landscape evolution in this region. Yet, studies reconstructing coastal palaeogeography in Northern Canadaare constrained by the limitation of shell–based radiocarbon chronologies used in dating shoreline displacementand palaeo–sea levels. This study proposes an alternative methodology for the reconstruction and dating of palaeo–sea levels, which uses testate amoeba

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Schaal, Caroline, and Henri-Georges Naton. "Contribution of archaeobotany to understand taphonomic phenomena. The case of a Preboreal palaeochannel of Autrecourt-et-Pourron (Ardennes, France)." BSGF - Earth Sciences Bulletin 192 (2021): 6. http://dx.doi.org/10.1051/bsgf/2021003.

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Palaeoecology, through the analysis of the interactions between environmental factors and ecosystems, refines the knowledge of the structuring process of plant communities and helps to understand the complexity of past environments. However, it is necessary to analyse the taphonomic phenomena (deposition, conservation, degradation) affecting plant macrofossil assemblages in order to perform relevant palaeoecological analyses. Indeed, plant macrofossils may be under or over-represented in carpological assemblages, depending on the resistance of their cell membranes and the sedimentary condition

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Chevalier, Manuel. "<i>crestr</i>: an R package to perform probabilistic climate reconstructions from palaeoecological datasets." Climate of the Past 18, no. 4 (2022): 821–44. http://dx.doi.org/10.5194/cp-18-821-2022.

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Abstract. Statistical climate reconstruction techniques are fundamental tools to study past climate variability from fossil proxy data. In particular, the methods based on probability density functions (or PDFs) can be used in various environments and with different climate proxies because they rely on elementary calibration data (i.e. modern geolocalised presence data). However, the difficulty of accessing and curating these calibration data and the complexity of interpreting probabilistic results have often limited their use in palaeoclimatological studies. Here, I introduce a new R package

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Krolopp, Endre, and P�l S�megi. "Palaeoecological reconstruction of the late pleistocene, based on loess malacofauna in Hungary." GeoJournal 36, no. 2-3 (1995): 213–22. http://dx.doi.org/10.1007/bf00813173.

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7

Feurdean, Angelica, and Ole Bennike. "Late Quaternary palaeoecological and palaeoclimatological reconstruction in the Gutaiului Mountains, northwest Romania." Journal of Quaternary Science 19, no. 8 (2004): 809–27. http://dx.doi.org/10.1002/jqs.872.

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8

Patnaik, Rajeev. "Micromammal-Based Palaeoenvironment of Upper Siwaliks Exposed Near Village Saketi, H. P." Journal Geological Society of India 46, no. 4 (1995): 429–37. http://dx.doi.org/10.17491/jgsi/1995/460414.

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Abstract Two sections, namely Kanthro and Moginand exposing Upper Siwalik rocks near village Saketi (H.P., India) have yielded a diverse fossil assemblage and evidence for pedogenic modifications. Palaeoecological reconstruction indicates the presence of atleast four palaeocommunities (pond, pondbank, bushland and grassland). Studies concerning taphonomy reveals that there was a gradual accumulation of micro and megafossil remains in shallow seasonal ponds of broad flood plains. It is also noticed that the concentration of some small mammal remains were due to biogenic processes.

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9

Richer, Suzi, and Benjamin Gearey. "The Medicine Tree: Unsettling palaeoecological perceptions of past environments and human activity." Journal of Social Archaeology 17, no. 3 (2017): 239–62. http://dx.doi.org/10.1177/1469605317731013.

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In this paper, we consider palaeoecological approaches to past landscapes and reflect upon how these are relevant to archaeological themes concerning concepts of environmental change and the role of past and present human communities in these processes. In particular, we highlight the importance of local context in the perception and understanding of landscape. Utilising a case study from Nepal, we look to ‘unsettle’ a conventional palaeoecological interpretation of a pollen record, originally constructed on western ecological principles, and instead draw on an interpretative perspective roote

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Tapody, Réka Orsolya, Pál Sümegi, Dávid Molnár, et al. "Sedimentological-Geochemical Data Based Reconstruction of Climate Changes and Human Impacts from the Peat Sequence of Round Lake in the Western Foothill Area of the Eastern Carpathians, Romania." Quaternary 4, no. 2 (2021): 18. http://dx.doi.org/10.3390/quat4020018.

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This paper presents the results of comparative sedimentological and geochemical analysis of the mire at Sânpaul, Round Lake (Kerek-tó). The palaeoecological site is situated in the western foothill area of the Eastern Carpathians in Romania. The primary objective of this study was to analyse the accumulation of major and trace elements in a 7500 year-long peat and lake deposition. The concentrations of 13 elements were determined by using handheld XRF. This paper presents the results of a multidisciplinary study, for which the principal aims were to examine the long-term relationship between l

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Grenaderova, A. V., and R. A. Sharafutdinov. "RECONSTRUCTION OF PALAEOECOLOGICAL CONDITIONS IN THE VALLEY OF OYA RIVER IN LATE HOLOCENE." Proceedings of the Tigirek State Natural Reserve, no. 1 (2005): 141–46. http://dx.doi.org/10.53005/20767390_2005_1_141.

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12

Olchev, A. V., E. R. Getmanova, and E. Yu Novenko. "A modeling approach for reconstruction of annual land surface evapotranspiration using palaeoecological data." IOP Conference Series: Earth and Environmental Science 438 (February 4, 2020): 012021. http://dx.doi.org/10.1088/1755-1315/438/1/012021.

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13

Nikolaou, K., A. Alysandratou, K. Karanika, et al. "SEDIMENTOLOGY AND PALAEOENVIRONMENTAL RECONSTRUCTION OF AG-1 CORE OF AYVALIK REGION, NW TURKEY." Bulletin of the Geological Society of Greece 50, no. 1 (2017): 354. http://dx.doi.org/10.12681/bgsg.11736.

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This study presents sedimentological and palaeontological data retrieved from a coastal lagoon near Ayvalik in NW Turkey. The objective of this study is to interpret the depositional environments and reconstruct the evolution of the study area during the late Holocene. 42 sediment samples have been retrieved from a 13m core. Sedimentological analyses such as grain size analysis, moment measures of mean, sorting, skewness and kurtosis, definition of total organic carbon (T.O.C.), total nitrogen (T.N.), colour and CaCO3 (%) were employed. Moreover, macro and microfossils were collected to recons

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Deforce, Koen, Annelies Storme, Jan Bastiaens, et al. "Middle-Holocene alluvial forests and associated fluvial environments: A multi-proxy reconstruction from the lower Scheldt, N Belgium." Holocene 24, no. 11 (2014): 1550–64. http://dx.doi.org/10.1177/0959683614544059.

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Analyses of pollen, plant macrofossils (seeds, fruits, wood and mosses), molluscs, diatoms and vertebrate (mainly fish) remains allowed a detailed reconstruction of a middle-Holocene alluvial forest and its associated hydrological conditions. The use of multiple proxies resulted in a taxonomically more detailed and environmentally more comprehensive understanding of terrestrial as well as aquatic habitats. The results demonstrate possible biases in palaeoecological reconstructions of alluvial and estuarine environments drawn from single proxies. Many locally occurring woody taxa were underrepr

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15

Rybníček, Kamil, and Eliška Rybníčková. "A palaeoecological reconstruction of precultural vegetation in the intermontane basins of the Western Carpathians." Ecologia mediterranea 11, no. 1 (1985): 27–31. http://dx.doi.org/10.3406/ecmed.1985.1067.

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16

Socha, Paweł. "Rodent palaeofaunas from Biśnik Cave (Kraków-Częstochowa Upland, Poland): Palaeoecological, palaeoclimatic and biostratigraphic reconstruction." Quaternary International 326-327 (April 2014): 64–81. http://dx.doi.org/10.1016/j.quaint.2013.12.027.

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17

Thorn, Vanessa C. "New Zealand sub-Antarctic phytoliths and their potential for past vegetation reconstruction." Antarctic Science 20, no. 1 (2007): 21–32. http://dx.doi.org/10.1017/s0954102007000727.

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AbstractPhytoliths in the modern vegetation of sub-Antarctic Campbell Island are compared with those in the soil beneath to assess the accuracy of vegetation reconstructions made from dispersed phytolith assemblages. The soil phytoliths alone suggest the source vegetation is a grassland association for all study sites, which reflects none of the herb, fern or shrub component of the overlying vegetation. It is concluded that at this locality dispersed phytoliths on their own are not reliable indicators of source vegetation and should be used with caution in this context for palaeoecological stu

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18

Eastwood, W. J., N. Roberts, and H. F. Lamb. "Palaeoecological and archaeological evidence for human occupance in southwest Turkey: the Beyşehir occupation phase." Anatolian Studies 48 (December 1998): 69–86. http://dx.doi.org/10.2307/3643048.

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The mountains of the Eastern Mediterranean have a long history of human occupation and exploitation of the natural environment (Grenon, Batisse 1989; McNeil 1992). Whilst the reconstruction of vegetation and human-induced landscape change is primarily based upon pollen analysis and other palaeoecological methods, the history of human occupation relies heavily upon archaeology, including field survey information and excavation reports. Both palaeoecology and archaeology are supplemented by historical accounts, especially for later periods, and when these data sources are combined they have the

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Hristova, Raina, and Preslav Peev. "About the stratigraphic correlation of events in Holocene geoarchaeology." Review of the Bulgarian Geological Society 84, no. 3 (2023): 355–58. http://dx.doi.org/10.52215/rev.bgs.2023.84.3.355.

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Many researchers work in the field of the newly emerging discipline – marine geoarchaeology during the Holocene. One of the most current scientific studies, which combined the efforts of archaeologists and geologists, are the interdisciplinary ones, the purpose of which is to make a palaeogeographical reconstruction of the natural environment in the period from Prehistory to the Late Antiquity. Based on a broad methodological basis, geological, geomorphological, biostratigraphic, archaeological and historical data are simultaneously interpreted. This type of modern geoarchaeological research p

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20

Downey, Clare, and Manuel Domínguez-Rodrigo. "Palaeoecological reconstruction and hominid land use of the Lake Natron basin during the Early Pleistocene." Before Farming 2002, no. 3-4 (2002): 1–36. http://dx.doi.org/10.3828/bfarm.2002.3-4.5.

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21

Beaulieu-Audy, Véronique, Michelle Garneau, Pierre J. H. Richard, and Hans Asnong. "Holocene palaeoecological reconstruction of three boreal peatlands in the La Grande Rivière region, Québec, Canada." Holocene 19, no. 3 (2009): 459–76. http://dx.doi.org/10.1177/0959683608101395.

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22

Barczi, Attila, and Katalin Joó. "The role of kurgans in the Palaeopedological and Palaeoecological reconstruction of the Hungarian Great Plain." Zeitschrift für Geomorphologie, Supplementary Issues 53, no. 1 (2009): 131–37. http://dx.doi.org/10.1127/0372-8854/2009/0053s1-0131.

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23

Ayyad, S., and P. D. Moore. "Surface pollen rain studies in the Nile Delta, Egypt, and their use in palaeoecological reconstruction." Review of Palaeobotany and Palynology 82, no. 1-2 (1994): 191. http://dx.doi.org/10.1016/0034-6667(94)90030-2.

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24

Marquer, L., S. Pomel, A. Abichou, E. Schulz, D. Kaniewski, and E. Van Campo. "Late Holocene high resolution palaeoclimatic reconstruction inferred from Sebkha Mhabeul, southeast Tunisia." Quaternary Research 70, no. 2 (2008): 240–50. http://dx.doi.org/10.1016/j.yqres.2008.06.002.

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AbstractRelations between climate change and landscape evolution during the last two millennia in southeastern coastal Tunisia have been documented using high-resolution reconstruction of flood history and fire activity in the Sebkha Mhabeul core. The age model, based on tephrochronology, indicates that the core extends from Roman to modern times and encompasses the well-defined climatic periods of the last two millennia. This record provides a first palaeoecological/palaeoclimatic high resolution reconstruction in North Africa using a cross-disciplinary approach with both physical (grey-scale

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25

DRINIA, H. "Palaeoenvironmental significance of a late Miocene benthic foraminifera fauna from Apostoli Formation, Central West Crete, Greece." Bulletin of the Geological Society of Greece 34, no. 2 (2018): 627. http://dx.doi.org/10.12681/bgsg.17113.

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The palaeoenvironmental and palaeoecological reconstruction of the Apostoli Basin (Crete, Rethymnon Region) during early Late Miocene by means of benthic foraminifers is given. Biologically important factors, such as oxygen and nutrient content of sea-water, played a great role in the evolution of the palaeoecosystem. A gradual deepening took place during the deposition of the Apostoli Formation. The sediments of the lower part of the formation document a shallow-marine environment with vegetation in the neighborhood. In the middle part of the formation sediments are characterized by intermedi

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Tan, Zhen-Zhen, Yi-Ming Cui, Lwin Mar Saing, Chun-Xiang Li, and Ya Li. "Systematics and Palaeoecology of Three New Acrocarpous Mosses from the Mid-Cretaceous of Kachin, Myanmar." Plants 14, no. 14 (2025): 2124. https://doi.org/10.3390/plants14142124.

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The mid-Cretaceous Kachin amber deposit from northern Myanmar is currently a promising locality for reconstructing Cretaceous bryophyte floras. However, the vast majority of bryophyte fossils reported from Kachin amber are epiphytic leafy liverworts of Porellales and pleurocarpous mosses of Hypnodendrales, while acrocarpous mosses are rarely discovered. In addition, terrestrial-to-lithophytic bryophytes have never been reported from Kachin amber. In this study, we describe three new species of acrocarpous mosses, Calymperites proboscideus sp. nov., Calymperites chenianus sp. nov., and Ditrichi

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27

Ferrón, Humberto G., Carlos Martínez-Pérez, and Héctor Botella. "Ecomorphological inferences in early vertebrates: reconstructing Dunkleosteus terrelli (Arthrodira, Placodermi) caudal fin from palaeoecological data." PeerJ 5 (December 6, 2017): e4081. http://dx.doi.org/10.7717/peerj.4081.

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Our knowledge about the body morphology of many extinct early vertebrates is very limited, especially in regard to their post-thoracic region. The prompt disarticulation of the dermo-skeletal elements due to taphonomic processes and the lack of a well-ossified endoskeleton in a large number of groups hinder the preservation of complete specimens. Previous reconstructions of most early vertebrates known from partial remains have been wholly based on phylogenetically closely related taxa. However, body design of fishes is determined, to a large extent, by their swimming mode and feeding niche, m

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Tichá, Anna, Krisztina Buczkó, and Václav Houk. "Notes to the use of Aulacoseira taxa in the palaeoecological reconstruction of the Bohemian Forest lakes." Studia botanica hungarica 48, no. 2 (2017): 173–88. http://dx.doi.org/10.17110/studbot.2017.48.2.173.

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29

Herrmann, Mark. "Palaeoecological reconstruction of the late Oligocene Maar Lake of Enspel, Germany using lacustrine organic walled algae." Palaeobiodiversity and Palaeoenvironments 90, no. 1 (2010): 29–37. http://dx.doi.org/10.1007/s12549-009-0016-2.

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30

O'connell, Michael, Frazer J. G. Mitchell, Peter W. Readman, Terence J. Doherty, and Declan A. Murray. "Palaeoecological investigations towards the reconstruction of the post-glacial environment at Lough Doo, County Mayo, Ireland." Journal of Quaternary Science 2, no. 2 (1987): 149–64. http://dx.doi.org/10.1002/jqs.3390020208.

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31

Roberts, M. B., M. R. Bates, C. Bergman, et al. "Excavation of the Lower Palaeolithic Site at Amey's Eartham Pit, Boxgrove, West Sussex: A Preliminary Report." Proceedings of the Prehistoric Society 52 (1986): 215–45. http://dx.doi.org/10.1017/s0079497x00006666.

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The acheulian site at Boxgrove contains one of the most extensive areas of in situ fauna and flintwork yet discovered in Britain. This material is found in a complex sequence of sediments which represent depositional conditions from a 42 m sea level rise to the onset of a full periglacial climate. Excavation of the archaeological horizon has been accompanied by a programme of multidisciplinary research examining site formation processes, palaeolandscape and palaeoecological development, using sedimentological and environmental reconstruction techniques. Dating of the site is tentative as no ab

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Vári, Tamás Zsolt, Elemér Pál-Molnár, and Pál Sümegi. "Reconstructing the Paleoenvironmental Evolution of Lake Kolon (Hungary) through Palaeoecological, Statistical and Historical Analyses." Diversity 15, no. 10 (2023): 1095. http://dx.doi.org/10.3390/d15101095.

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The research utilizes an interdisciplinary approach, combining geological, ecological, and historical methods. It delves into the environmental evolution of Lake Kolon over a span of 17,700 years, shedding light on the intricate interplay between geological processes and ecological changes. The historical, statistical (PCA, DCA), and palaeoecological analyses centers on a core sequence situated in the heart of the lake, building upon previous research endeavors (pollen, malacological, macrobotanical and sedimentological analyses with radiocarbon dating). Forest fires occurred at the end of the

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Pidek, Irena Agnieszka. "Pollen-based vegetation and climate reconstruction of the Ferdynandovian sequence from Łuków (eastern Poland)." Acta Palaeobotanica 53, no. 1 (2013): 115–38. http://dx.doi.org/10.2478/acpa-2013-0009.

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ABSTRACT Early middle Pleistocene deposits from Łukow, correlated with the Cromerian complex, represent rare bi-partite Ferdynandovian pollen sequence encompassing two interglacial warmings (F1 and F2) separated by F1/2 cooling/glaciation and related to MIS 15-13. The paper presents pollen-based palaeoecological and palaeoclimate investigations in which plant climate indicators were applied. Additionally modern pollen dataset from the Roztocze region was used to evaluate vegetation history in terms of forest communities and presence and abundance of tree taxa sensitive to air temperature and h

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Carboni, M. Gabriella, Luisa Bergamin, Letizia Di Bella, et al. "Palaeoenvironmental reconstruction of late Quaternary foraminifera and molluscs from the ENEA borehole (Versilian plain, Tuscany, Italy)." Quaternary Research 74, no. 2 (2010): 265–76. http://dx.doi.org/10.1016/j.yqres.2010.07.006.

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AbstractForaminifera and molluscs from the 90 m deep ENEA borehole (Versilian plain, central Italy) were studied for paleoenvironmental purposes. Palaeontological analyses, integrated with U/Th and radiocarbon data, helped to recognize late Quaternary sea-level changes and supplied results on tectonic mobility of the area. The study highlighted four sedimentary phases. The first phase consists of a shore environment attributed to MIS 7.1. A hiatus corresponding to MIS 6 is hypothesized at the top of this interval. Recognition of the paleo-shoreline of MIS 7.1 at − 72.8 m signifies a vertical d

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Burgess, Roger, David Jolley, and Adrian Hartley. "Palaeoenvironmental reconstruction of Triassic floras from the Central North Sea." Journal of the Geological Society 179, no. 3 (2021): jgs2021–071. http://dx.doi.org/10.1144/jgs2021-071.

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The Triassic sediments of the Central North Sea (CNS) are considered to have been deposited in a continental environment under a semi-arid climate. The Skagerrak Formation in particular comprises an alternation of sandstone and mudstone members, the development of which is considered to be climatically driven. However, conflicting models exist as to how climate influences member deposition. Here we analyse the climatic signal using a multivariate statistical approach in which detrended correspondence analysis (DCA) is applied to palynological observations to quantify environmental reconstructi

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Barabach, Jan. "The history of Lake Rzecin and its surroundings drawn on maps as a background to palaeoecological reconstruction." Limnological Review 12, no. 3 (2012): 103–14. http://dx.doi.org/10.2478/v10194-011-0050-0.

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AbstractThe article presents the results of landscape analysis of the surroundings of Lake Rzecin in Noteć Forest depicted on cartographic materials. Morphometrical analysis and analysis of changes in the water conditions of Lake Rzecin were conducted. Thanks to many cartographic data, changes in lake geometry could be observed during almost the whole of the last two centuries. The results show that the major impact on the rate of lake level decrease in the last two hundred years was due to melioration works. Two periods of rapid decrease in the lake surface can be observed during this time. T

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Molloy, Karen, and Michael O'Connell. "Palaeoecological investigations towards the reconstruction of woodland and land-use history at Lough Sheeauns, Connemara, western Ireland." Review of Palaeobotany and Palynology 67, no. 1-2 (1991): 75–113. http://dx.doi.org/10.1016/0034-6667(91)90017-w.

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Staszak-Piekarska, Agata, and Monika Rzodkiewicz. "Reconstruction of palaeoecological changes in Lake Łebsko on the basis diatom analysis (the southern Baltic coast, Poland)." Landform Analysis 29 (December 31, 2015): 81–90. http://dx.doi.org/10.12657/landfana.029.010.

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39

Blaus, Ansis, Triin Reitalu, Leeli Amon, Jüri Vassiljev, Tiiu Alliksaar, and Siim Veski. "From bog to fen: palaeoecological reconstruction of the development of a calcareous spring fen on Saaremaa, Estonia." Vegetation History and Archaeobotany 29, no. 3 (2019): 373–91. http://dx.doi.org/10.1007/s00334-019-00748-z.

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40

Dobrowolski, Radosław, Irena Pidek, Witold Alexandrowicz, et al. "Interdisciplinary studies of spring mire deposits from Radzików (South Podlasie Lowland, East Poland) and their significance for palaeoenvironmental reconstructions." Geochronometria 39, no. 1 (2012): 10–29. http://dx.doi.org/10.2478/s13386-011-0052-3.

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Abstract The paper presents the results of interdisciplinary (multiproxy) palaeoenvironmental studies of peat — calcareous tufa depositional sequences of spring mire from Radzików site (east Poland). Analyses of three biotic proxies (plant macrofossils, pollen, molluscs) were supplemented with sedimentological, geochemical, oxygen and carbon stable isotopes analyses and radiocarbon dating and used for reconstruction of environmental changes in Late Glacial and Holocene. The obtained results enable us to (1) reconstruct main phases of mire development and (2) determine environmental factors inf

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Sarkar, Suman. "Diverse geniculate coralline algae in Cenozoic fossil records: knowledge gaps and applications in palaeoecology." Journal of Palaeosciences 73, no. 2 (2024): 157–64. https://doi.org/10.54991/jop.2024.1895.

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Coralline red algae (Corallinophycideae) are marine calcifying primary producers documented in euphotic habitats globally. Cenozoic carbonate sediments of India put forward an excellent opportunity for the analysis of coralline algae, their contribution in reconstruction of benthic palaeoenvironments and response to climate change. Compared to the common integrated analysis of non-geniculate coralline morphotypes with benthic groups like corals and larger benthic foraminifera, application of geniculate coralline algae is relatively very poor in palaeoecological studies. In order to understand

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Ponomarenko, Ekaterina, Tatiana Pugacheva, and Liubov Kuleshova. "Palaeoecological Conditions in the South-Eastern and Western Baltic Sea during the Last Millennium." Quaternary 7, no. 4 (2024): 44. http://dx.doi.org/10.3390/quat7040044.

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We present the reconstruction of palaeoenvironmental conditions in the Gdansk, Bornholm, and Arkona Basins of the Baltic Sea over the last millennium. A multiproxy study (including geochemical, XRF, grain size, AMS, and micropalaeontological analyses) of five short sediment cores was performed. The relative age of the sediments was determined based on the Pb distribution along the sediment sequences, as radiocarbon dating has resulted in an excessively old age. The retrieved cores cover two comparable warm periods, the Medieval Climate Anomaly and the Modern Warm Period, for which the increase

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Lyubas, AA, MB Kabakov, VV Kriauciunas, TF Obada, IN Nicoara, and AA Tomilova. "Freshwater mollusks from Neogene-Quaternary Dniester and Prut riverine deposits as indicator paleoenvironments: chemical composition of shells and its palaeoecological interpretation." Arctic Environmental Research 19, no. 1 (2019): 35–42. http://dx.doi.org/10.3897/issn2541-8416.2019.19.1.35.

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The respective environments in two ancient rivers were studied using geochemical methods with paleogeographic reconstructions of fossil material represented by shells of freshwater bivalve mollusks. The studied outcrops are located in the basins of the Dniester and Prut rivers. Materials were collected from two Pliocene (Brînza, Giurgiuleşti) outcrops and the ages of the second group of localities (Sucleia, Slobozia Mare, Gura Bîcului) are from Middle to Late Pleistocene. The determination of the taxonomic position was carried out using standard malacological methods. Geochemical data were use

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Lyubas, AA, MB Kabakov, VV Kriauciunas, TF Obada, IN Nicoara, and AA Tomilova. "Freshwater mollusks from Neogene-Quaternary Dniester and Prut riverine deposits as indicator paleoenvironments: chemical composition of shells and its palaeoecological interpretation." Arctic Environmental Research 19, no. (1) (2019): 35–42. https://doi.org/10.3897/issn2541-8416.2019.19.1.35.

Full text

Abstract:

The respective environments in two ancient rivers were studied using geochemical methods with paleogeographic reconstructions of fossil material represented by shells of freshwater bivalve mollusks. The studied outcrops are located in the basins of the Dniester and Prut rivers. Materials were collected from two Pliocene (Brînza, Giurgiuleşti) outcrops and the ages of the second group of localities (Sucleia, Slobozia Mare, Gura Bîcului) are from Middle to Late Pleistocene. The determination of the taxonomic position was carried out using standard malacological methods. Geochemical data were use

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45

Sanz-Pérez, Dánae, Manuel Hérnandez Fernández, María Belén Muñoz-García, Patricia Pérez-Dios, Jorge Morales, and Laura Domingo. "Palaeoecological and palaeoenviromental reconstruction of the upper Miocene vertebrate karstic site of Corral de Lobato, central-eastern Spain." Palaeogeography, Palaeoclimatology, Palaeoecology 556 (October 2020): 109877. http://dx.doi.org/10.1016/j.palaeo.2020.109877.

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Ren, Xiaolin, Duowen Mo, Michael Storozum, et al. "Early urban impact on vegetation dynamics: Palaeoecological reconstruction from pollen records at the Dongzhao site, Henan Province, China." Quaternary International 521 (June 2019): 66–74. http://dx.doi.org/10.1016/j.quaint.2019.07.012.

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Golyeva, Alexandra, and Maja Andrič. "Palaeoecological reconstruction of wetlands and Eneolithic land use in Ljubljansko barje (Slovenia) based on biomorphic and pollen analysis." CATENA 112 (January 2014): 38–47. http://dx.doi.org/10.1016/j.catena.2012.12.009.

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Pr�sch-Danielsen, Lisbeth, and Asbj�rn Simonsen. "Palaeoecological investigations towards the reconstruction of the history of forest clearances and coastal heathlands in south-western Norway." Vegetation History and Archaeobotany 9, no. 4 (2000): 189–204. http://dx.doi.org/10.1007/bf01294634.

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Rybníček, K., and E. Rybníčková. "Palaeoecological and phytosociological reconstruction of precultural vegetation in the Bílý Kříž area, the Moravskoslezské Beskydy Mts, Slovak Republic." Vegetation History and Archaeobotany 4, no. 3 (1995): 161–70. http://dx.doi.org/10.1007/bf00203934.

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Vári, Tamás Zsolt, Elemér Pál-Molnár, and Pál Sümegi. "Palaeoenvironmental Analysis of the Southern Part of the Danube–Tisza Interfluve (Hungary): The Northern Loess Wall of Katymár and the Hay Meadows and Loess Banks of Hajós." Diversity 16, no. 10 (2024): 619. http://dx.doi.org/10.3390/d16100619.

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This study presents a comprehensive palaeoenvironmental reconstruction of the southern part of the Danube–Tisza interfluve in the Carpathian Basin from the Late Pleistocene to Early Holocene, addressing the region’s response to global climate forcings and local environmental factors based on multi-proxy analyses of two key protected areas: the Katymár brickyard and the hay meadows and loess banks of Hajós. By integrating radiocarbon-dated malacological, macrobotanical, pollen, phytolith, geochemical, and sedimentological analyses, it was possible to provide a picture of past climate–ecosystem

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