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100 _aSevink, Jan
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245 _aHolocene vegetation record of upland northern Calabria, Italy: Environmental change and human impact/
260 _bSage,
_c2019.
300 _aVol 29, issue 4, 2019 : (633-647 p.).
520 _aEarlier studies on Holocene fills of upland lakes (Lago Forano and Fontana Manca) in northern Calabria, Italy, showed that these hold important palaeoecological archives, which however remained poorly dated. Their time frame is improved by new 14C dates on plant remains from new cores. Existing pollen data are reinterpreted, using this new time frame. Two early forest decline phases are distinguished. The earliest is linked to the 4.2 kyr BP climatic event, when climate became distinctly drier, other than at Lago Trifoglietti on the wetter Tyrrhenian side, where this event is less prominent. The second is attributed to human impacts and is linked to middle-Bronze Age mobile pastoralism. At Fontana Manca (c. 1000 m a.s.l.), it started around 1700 BC, in the higher uplands a few centuries later (Lago Forano, c. 1500 m a.s.l.). In the Fontana Manca fill, a thin tephra layer occurs, which appears to result from the AP2 event (Vesuvius, c. 1700 BC). A third, major degradation phase dates from the Roman period. Land use and its impacts, as inferred from the regional archaeological record for the Raganello catchment, are confronted with the impacts deduced from the palaeoarchives.
650 _a4.2 ka BP climate event,
_951751
650 _a archaeology,
_950689
650 _alake fills,
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650 _apollen records,
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650 _atephrochronology
_951754
700 _a Bakels, Corrie C
_951755
700 _aAttema, Peter AJ
_951756
700 _aVito, Mauro A Di
_951757
700 _aArienzo, Ilenia
_951758
773 0 _012756
_916504
_dLondon: Sage Publication Ltd, 2019.
_tHolocene/
_x09596836
856 _uhttps://doi.org/10.1177/0959683618824695
942 _2ddc
_cART
999 _c12814
_d12814