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Relevant bibliographies by topics / Holocène – Tunisie

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Journal articles

Academic literature on the topic 'Holocène – Tunisie'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Holocène – Tunisie"

1

Ballais, Jean-Louis. "Évolution holocène de la Tunisie saharienne et présaharienne." Méditerranée 74, no. 4 (1991): 31–38. http://dx.doi.org/10.3406/medit.1991.2735.

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2

Boujelben, Abdelkarim, Vincent Lebreton, and Mohamed Raouf Karray. "Dynamique lacustre Holocène dans la sebkha al Kalbiyya(Tunisie centre orientale)." Quaternaire, no. 28/2 (May 29, 2017): 239–45. http://dx.doi.org/10.4000/quaternaire.8138.

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3

Morzadec-Kerfourn, Marie Thérèse. "L'évolution des Sebkhas du golf de Gabès (Tunisie) à la transition Pléistocène supérieur-Holocène." Quaternaire 13, no. 2 (2002): 111–23. http://dx.doi.org/10.3406/quate.2002.2185.

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4

ZAIBI, CHAHIRA, BURKHARD SCHARF, FINN ANDREAS VIEHBERG, DIETMAR KEYSER, and FEKRI KAMOUN. "Preliminary report on the living non-marine Ostracoda (Crustacea) from Tunisia with the description of a new Psychrodromus species." Zootaxa 3626, no. 4 (2013): 499–516. http://dx.doi.org/10.11646/zootaxa.3626.4.5.

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Since 1928, Henri Gauthier has been the only zoologist to describe the extant non-marine ostracod fauna of Tunisia. In 2010, new samples of living non-marine ostracods were collected from central and southern Tunisia. A complete list of the 41 non-marine ostracods of Tunisiais presented, including the species of Gauthier’s work, published Holocene records, and new results from our field study. Historical faunal variations (El Melah Lagoon, Lac de Tunis, Sebkhas El- Guettiate and Dreîaa, and Lac Ichkeul) are briefly discussed and related to recent environmental changes. In 2006, El Melah Lagoon contained a freshwater, brackish, and a marine ostracod assemblage. In the future, this lagoon will probably dry up and become a sebkha. Lac de Tunis has developed from a marine bay over a lagoon connected to the Mediterranean Seato a brackish/freshwater environment. Sebkhas El-Guettiate and Dreîaa have developed from marine bays to dry salt flats. Lac Ichkeul is eutrophied and has become brackish since the time of Gauthier. We also describe a new species, Psychrodromus tunisicus n. sp., and present a determination key for the genus. The finding of a species of the genus Psychrodromus is the first report of this genus inNorth Africa.

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5

Zielhofer, Christoph, and Dominik Faust. "Mid- and Late Holocene fluvial chronology of Tunisia." Quaternary Science Reviews 27, no. 5-6 (2008): 580–88. http://dx.doi.org/10.1016/j.quascirev.2007.11.019.

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6

Morhange, Christophe, and Paolo Antonio Pirazzoli. "Mid-Holocene emergence of southern Tunisian coasts." Marine Geology 220, no. 1-4 (2005): 205–13. http://dx.doi.org/10.1016/j.margeo.2005.06.031.

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7

Kolstrup, Else. "Late Holocene pollen records from the Segermes valley, Ne Tunisia." Historical Biology 9, no. 1-2 (1994): 131–36. http://dx.doi.org/10.1080/10292389409380494.

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8

Frébourg, Gregory, Claude-Alain Hasler, and Eric Davaud. "Catastrophic event recorded among Holocene eolianites (Sidi Salem Formation, SE Tunisia)." Sedimentary Geology 224, no. 1-4 (2010): 38–48. http://dx.doi.org/10.1016/j.sedgeo.2009.12.006.

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9

Zerai, Kamel. "Chronostratigraphy of Holocene alluvial archives in the Wadi Sbeïtla basin (central Tunisia)." Géomorphologie : relief, processus, environnement 15, no. 4 (2009): 271–86. http://dx.doi.org/10.4000/geomorphologie.7737.

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10

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 intensity, quartz particles) and biological (charcoal and pollen) indicators. The flood history shows four wet/dry cycles (ca. AD 550–950, 950–1300, 1300–1570 and 1570–1870) of different duration. Major hydrological instabilities are concentrated during the Medieval Climate Anomalies and the early Little Ice Age, between AD 1000 and 1550. Direct correlation between climate and fire cannot be established suggesting that the fire history of the Sebkha environment is mainly influenced by human activity. This study demonstrates the great value of sebkhas as palaeoenvironmental archives.

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