A quantitative understanding of climatic variations in the Levant during the last glacial cycle is needed to support archaeologists in assessing the drivers behind hominin migrations and cultural developments in this key region at the intersection betwee
The sedimentary sections that were deposited from the Holocene Dead Sea and its Pleistocene precurso...
of late glacial Lake Lisan and fan delta surfaces between 280 and 365m bmsl (meters below mean sea l...
These datasets provide sedimentological data partly at annual resolution and an age model for the la...
A quantitative understanding of climatic variations in the Levant during the last glacial cycle is n...
Changes in the level of closed lakes such as the glacial Lake Lisan/Near East, that occupied the Jor...
Lake Lisan, the late Pleistocene precursor of the Dead Sea, existed from ∼70,000 to 15,000 yr B.P. I...
The Dead Sea is a terminal lake of one of the largest hydrological systems in the Levant and may thu...
Documentation of short-term climate variability during the glacial period has been limited by the av...
In this paper we describe the stratigraphy and sediments deposited in Lake Samra that occupied the D...
The lake level of the Dead Sea, Southern Levant, has fluctuated with an amplitude of ∼250 m in respo...
The rain regime of the Levant during the late Quaternary was controlled primarily by Mediterranean c...
Based on geomorphic observations, we discuss lake-level fluctuations, alluvial deposition and river ...
Calcite speleothems are a hitherto hardly documented occurrence in the nowadays arid to hyper-arid r...
The Dead Sea is located on the boundary between the Sahara and the Mediterranean climatic zones. Its...
The southern Levant is a key region for studying vegetation developments in relation to climate dyna...
The sedimentary sections that were deposited from the Holocene Dead Sea and its Pleistocene precurso...
of late glacial Lake Lisan and fan delta surfaces between 280 and 365m bmsl (meters below mean sea l...
These datasets provide sedimentological data partly at annual resolution and an age model for the la...
A quantitative understanding of climatic variations in the Levant during the last glacial cycle is n...
Changes in the level of closed lakes such as the glacial Lake Lisan/Near East, that occupied the Jor...
Lake Lisan, the late Pleistocene precursor of the Dead Sea, existed from ∼70,000 to 15,000 yr B.P. I...
The Dead Sea is a terminal lake of one of the largest hydrological systems in the Levant and may thu...
Documentation of short-term climate variability during the glacial period has been limited by the av...
In this paper we describe the stratigraphy and sediments deposited in Lake Samra that occupied the D...
The lake level of the Dead Sea, Southern Levant, has fluctuated with an amplitude of ∼250 m in respo...
The rain regime of the Levant during the late Quaternary was controlled primarily by Mediterranean c...
Based on geomorphic observations, we discuss lake-level fluctuations, alluvial deposition and river ...
Calcite speleothems are a hitherto hardly documented occurrence in the nowadays arid to hyper-arid r...
The Dead Sea is located on the boundary between the Sahara and the Mediterranean climatic zones. Its...
The southern Levant is a key region for studying vegetation developments in relation to climate dyna...
The sedimentary sections that were deposited from the Holocene Dead Sea and its Pleistocene precurso...
of late glacial Lake Lisan and fan delta surfaces between 280 and 365m bmsl (meters below mean sea l...
These datasets provide sedimentological data partly at annual resolution and an age model for the la...
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