Late Holocene water level fluctuations of Lake Afourgagh (Middle-Atlas Mountains, Morocco) inferred from charophyte remains

• Published in: Palaeogeography, Palaeoclimatology, Palaeoecology
• Main Authors: Détriché, Sébastien, Bréhéret, Jean-Gabriel, Soulié-Märsche, I., Karrat, L., Macaire, Jean-Jacques
• Other Authors: Transferts continentaux : forçages anthropiques, climatiques et géodynamiques, Institut des Sciences de la Terre d'Orléans (ISTO), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS), Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement IRD : UR226-Centre National de la Recherche Scientifique (CNRS), Université Sidi Mohamed Ben Abdellah (USMBA), This work was supported by the "Action Intégrée" MA 01/10 programme (François Rabelais University, Tours, France/Sidi Mohamed Ben Abdellah University, Fez, Morocco) and the CNRS-ECLIPSE project: "Impact anthropique sur l'érosion des sols et la sédimentation dans les zones humides associées durant l'Holocène" in 2005 and 2006-2007
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2009
• Subjects: Palaeolimnology; Late Holocene; Charophytes; Chara aspera; Chara hispida; Gyrogonites; Karstic lake; Middle-Atlas Mountains; Morocco; [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces; environment; [SDE.MCG]Environmental Sciences/Global Changes; Low Lake
• Online Access: https://hal-insu.archives-ouvertes.fr/insu-00426196; https://hal-insu.archives-ouvertes.fr/insu-00426196/document; https://hal-insu.archives-ouvertes.fr/insu-00426196/file/DA_trichA_.pdf; https://doi.org/10.1016/j.palaeo.2009.09.012

International audience Water level fluctuations of Lake Afourgagh (Middle-Atlas Mountains, Morocco) over the last 2500 years (Late Holocene) have been reconstructed using charophyte remains in the lake sediment archives. The study involved 22 pits (1-3 m deep) dug along a transect across the lake shore terrace. Biogenic activity appears to be a dominant contributor to the accumulation of the lake sediments, as the thickest deposits are tufas composed of charophyte-encrusted stems with numerous gyrogonites (termed "charophyte tufas"). The gyrogonites were identified as Chara aspera and Chara hispida remains. The spatial distribution of these two species, measured vertically within a single core and horizontally along the shore terrace, varies according to bathymetry. Shallow proximal environments are characterized by the development of C. aspera, whereas C. hispida remains are mostly observed in distal sediments. Moreover, according to their ecological characteristics, the C. hispida belt migrated proximally when the water level rose, whereas the C. aspera belt migrated distally when the water level fell. These trends were observed successively in a single charophyte tufa layer which records the rise, highstand, and fall of lake level in a single depositional sequence. The late Holocene palaeobathymetry of Lake Afourgagh was inferred by comparing data on charophyte remains and deposit geometry. Data provide evidence for four major low lake level phases (estimated in terms of amplitude) which induced the development of palaeosols in proximal settings at 2191 cal. BP, 1769 BP, 1515 cal. BP and 1062 cal. BP. These results confirm the accuracy of charophyte-based palaeobathymetry studies.