Foraminiferal record and environmental changes during the deposition of the Early-Middle Pleistocene sapropels in southern Italy

被引:39
|
作者
Stefanelli, S
Capotondi, L
Ciaranfi, N
机构
[1] Univ Bari, Dipartimento Geol & Geofis, I-70125 Bari, Italy
[2] CNR, ISMAR, Marine Geol Sect, I-40129 Bologna, Italy
关键词
benthic and planktonic foraminifera; sapropel; i-Cycle; 90; Mediterranean; Early-Middle Pleistocene;
D O I
10.1016/j.palaeo.2004.10.001
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
A foraminiferal investigation documents the palacoenvironmental changes across the sapropel units associated with insolation-cycles 90 and 86 in the Early-Middle Pleistocene IM/Fosso 5 Agosto section (Basilicata, southern Italy). Three benthic foraminiferal fossil associations (Associations A, B and C), identified by performing Hierarchical Cluster Analysis on the quantitative data, can be considered diagnostic of the palaeoenvironmental conditions before, during and after the sapropel intervals. They indicate a gradual decrease of bottom water oxygenation prior to the onset of sapropel deposition and a rapid return to stable environmental conditions at the end of the sapropel events. The constant presence of benthic foraminifera throughout the sapropels implies that the bottom environment was not totally anoxic. The high-resolution distributional pattern of planktonic and benthic foraminifera within the sapropel associated with i-cycle 90 documents a surface water cooling with consequent rapid re-oxygenation of bottom waters that subdivides this interval in two phases. Both of them are characterized by an early subphase with warm climate conditions, a decrease of salinity in surficial water layers and dominated by the low oxygen tolerant benthic species Globobulimina affinis. The late subphase shows thermal stratification during summer and a relatively deep and oxygenated mixed layer during winter. In this subphase, the contemporaneous replacement of G. affinis, the "less opportunistic, but more resistant to low oxygen conditions" species with Bolivina alata, Bolivina dilatata and Brizalina spathulata, the "less resistant to low oxygen conditions" species, indicates the relative oxygen improvement in sediment pore water. The frequent changes detected in the sapropel-associated faunal composition underline the unstable nature of bottom water oxygen content. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:27 / 52
页数:26
相关论文
共 50 条
  • [1] Cyclic changes in oxygenation based on foraminiferal microhabitats: Early-middle Pleistocene, Lucania Basin (Southern Italy)
    Stefanelli, S
    JOURNAL OF MICROPALAEONTOLOGY, 2004, 23 : 81 - 95
  • [2] Hominin responses to environmental changes during the Middle Pleistocene in central and southern Italy
    Orain, R.
    Lebreton, V.
    Ermolli, E. Russo
    Semah, A. -M.
    Nomade, S.
    Shao, Q.
    Bahain, J-J
    Hohenstein, U. Thun
    Peretto, C.
    CLIMATE OF THE PAST, 2013, 9 (02) : 687 - 697
  • [3] Early-Middle Pleistocene environmental changes and human evolution in the Italian peninsula
    Manzi, Giorgio
    Magri, Donatella
    Palombo, Maria Rita
    QUATERNARY SCIENCE REVIEWS, 2011, 30 (11-12) : 1420 - 1438
  • [4] ENVIRONMENTAL CHANGES AND HUMAN SETTLEMENT IN THE CENTRAL MARCHES (ITALY) DURING THE EARLY-MIDDLE HOLOCENE
    Calderoni, Gilberto
    Cilla, Giuseppe
    Dramis, Francesco
    Gobbi, Cecilia
    PHYSIO-GEO, 2007, 1 : 21 - 32
  • [5] Vegetation and climate across the Early-Middle Pleistocene transition at Montalbano Jonico, southern Italy
    Bertini, Adele
    Toti, Francesco
    Marino, Maria
    Ciaranfi, Neri
    QUATERNARY INTERNATIONAL, 2015, 383 : 74 - 88
  • [6] Climate and vegetation changes during the Lateglacial and early-middle Holocene at Lake Ledro (southern Alps, Italy)
    Joannin, S.
    Vanniere, B.
    Galop, D.
    Peyron, O.
    Haas, J. N.
    Gilli, A.
    Chapron, E.
    Wirth, S. B.
    Anselmetti, F.
    Desmet, M.
    Magny, M.
    CLIMATE OF THE PAST, 2013, 9 (02) : 913 - 933
  • [7] Environmental changes during early-middle Holocene from the sediment record of the Chaohu Lake,Anhui Province
    WANG XinYuan 1
    2Work Station for Remote Sensing Archaeology
    3 College of Geography and Marine Science
    4Department of Management Information Systems
    5Nanjing Institute of Geography and Limnology
    Science Bulletin, 2008, 53 (S1) : 153 - 160
  • [8] Environmental changes during early-middle Holocene from the sediment record of the Chaohu Lake, Anhui Province
    Wang XinYuan
    Zhang GuangSheng
    Wu Li
    Zhang XiHui
    Zhang EnLou
    Xiao XiaYun
    Jiang QingFeng
    CHINESE SCIENCE BULLETIN, 2008, 53 : 153 - 160
  • [9] Early-Middle Pleistocene environmental and biotic transition in north-western Armenia, southern Caucasus
    Tesakov, Alexey S.
    Simakova, Alexandra N.
    Frolov, Pavel D.
    Sytchevskaya, Eugenia K.
    Syromyatnikova, Elena, V
    Foronova, Irina, V
    Shalaeva, Eugenia A.
    Trifonov, Vladimir G.
    PALAEONTOLOGIA ELECTRONICA, 2019, 22 (02) : 2 - 39
  • [10] The Early Pleistocene in Latium (Central Italy): palaeoecology from benthic foraminiferal record
    Di Bella, L
    Carboni, MG
    Bergamin, L
    Iamundo, F
    QUATERNARY INTERNATIONAL, 2005, 131 : 23 - 34