Jorg F W Negendank

Biographic Data

ID	5601292
NAME	Jorg F W Negendank
GIVEN NAMES	Jorg F W
FAMILY NAME	Negendank
SIGNATURE	NEGENDANK J F W
AFFILIATIONS	GFZ Helmholtz Centre for Geosciences
VERIFIED	No
TOTAL WORKS	18
TOTAL CITATIONS	11
WORKS AS AUTHOR	18
WORKS AS EDITOR	0
FIRST PUBLICATION YEAR	1999
LATEST PUBLICATION YEAR	2012
H-INDEX	2

Palaeovegetation and palaeoclimate in low-latitude southern China during the Last Glacial Maximum
Open AccessShuyun Wang, Houyuan Lu et al.ARTICLEQuaternary International2012
Influence of the intertropical convergence zone on the East Asian monsoon
Open AccessGergana Yancheva, Norbert R Nowaczyk et al.ARTICLENature2007
Holocene Climate Variability and Cultural Evolution in the Near East from the Dead Sea Sedimentary Record
Open AccessClaudia Migowski, Mordechai Stein et al.ARTICLEQuaternary Research2006
A comprehensive record of lake level changes in the Dead Sea has been reconstructed using multiple, well dated sediment cores recovered from the Dead Sea shore. Interpreting the lake level changes as monitors of precipitation in the Dead Sea drainage area and the regional eastern Mediterranean palaeoclimate, we document the presence of two major wet phases (∼ 10–8.6 and ∼ 5.6–3.5 cal kyr BP) and multiple abrupt arid events during the Holocene. Th…
Rapid climate change during the early Holocene in western Europe and Greenland
Open AccessSushma Prasad, Achim Brauer et al.ARTICLEThe Holocene2006Cited by: 1References: 8
Based on microfacies analyses of seasonally laminated varved sediments from lake Holzmaar, Germany, we report evidence of decadal-to century-scale climate variability during the early Holocene. The shifts in climate are documented in the thickness variations and changes in the composition of the varves in response to subtle shifts in limnological conditions. The close similarity between the Holzmaar varve record and the GRIP oxygen isotope record…
The late Quaternary limnological history of Lake Kinneret (Sea of Galilee), Israel
Open AccessNissim Hazan, Mordechai Stein et al.ARTICLEQuaternary Research2005
The freshwater Lake Kinneret (Sea of Galilee) and the hypersaline Dead Sea are remnant lakes, evolved from ancient water bodies that filled the tectonic depressions along the Dead Sea Transform (DST) during the Neogene–Quartenary periods. We reconstructed the limnological history (level and composition) of Lake Kinneret during the past ∼40,000 years and compared it with the history of the contemporaneous Lake Lisan from the aspect of the regional…
The Huguang maar lake—a high-resolution record of palaeoenvironmental and palaeoclimatic changes over the last 78,000 years from South China
Open AccessJens Mingram, Georg Schettler et al.ARTICLEQuaternary International2004
Tephrochronology of the 100ka lacustrine sediment record of Lago Grande di Monticchio (southern Italy)
Open AccessSabine Wulf, Michael Kraml et al.ARTICLEQuaternary International2004
The European Lake Drilling Programme (ELDP) from 1996–2001
Open AccessAchim Brauer, Jorg F W NegendankARTICLEQuaternary International2004
Indication of climatically induced natural eutrophication during the early Holocene period, based on annually laminated sediment from Lake Holzmaar, Germany
Open AccessCathrin Brüchmann, Jorg F W NegendankARTICLEQuaternary International2004
Environmental variability in East and West Eurasia
Open AccessYoshinori Yasuda, Jorg F W NegendankARTICLEQuaternary International2003
Correlation and synchronisation of Lateglacial continental sequences in northern central Europe based on annually laminated lacustrine sediments
Open AccessThomas Litt, Achim Brauer et al.ARTICLEQuaternary Science Reviews2001
Precision of Calibrated Radiocarbon Ages of Historic Earthquakes in the Dead Sea Basin
Open AccessRevital Ken-Tor, Mordechai Stein et al.ARTICLERadiocarbon2001Cited by: 4References: 9
The precise determination of the age of historical and geological events by radiocarbon dating is often hampered by the long intersection ranges of the measured data with the calibration curve. In this study we examine the possibility of narrowing the calibrated range of the 14 C ages of earthquake-disturbed sediments (seismites) from the Late Holocene lacustrine section in the Dead Sea Basin. The calibrated ranges of samples collected from seism…
Abrupt environmental oscillations during the Early Weichselian recorded at Lago Grande di Monticchio, southern Italy
Open AccessAchim Brauer, Jens Mingram et al.ARTICLEQuaternary International2000
Circum-Mediterranean lake records as archives of climatic and human history
Open AccessBernd Zolitschka, Sabine Wulf et al.ARTICLEQuaternary International2000
Sediments from Lago di Mezzano, central Italy
Open AccessAntje Ramrath, Laura Sadori et al.ARTICLEThe Holocene2000Cited by: 5References: 7
Microscopic, geochemical and pollen analysis of sediment samples of a Lateglacial/Holocene profile from Lago di Mezzano, a maar lake in central Italy, reveals evidence of significant climatic and human-induced environmental changes. Time control is provided by a combination of varve chronology and radiocarbon dating. The well-known Lateglacial climatic variations, a warmer interstadial and the Younger Dryas cold phase are clearly represented in a…
Rapid environmental changes in southern Europe during the last glacial period
Open AccessJudy R M Allen, Ute Brandt et al.ARTICLENature1999
Lateglacial calendar year chronology based on annually laminated sediments from Lake Meerfelder Maar, Germany
Open AccessAchim Brauer, Christoph Endres et al.ARTICLEQuaternary International1999
Geochemical evidence for Holocene palaeodischarge variations in lacustrine records from the Westeifel Volcanic Field, Germany
Open AccessGeorg Schettler, Bert Rein et al.ARTICLEThe Holocene1999Cited by: 1References: 4
Various chemical elements (Fe, Mn, U, Mo) can be transported in both dissolved and solid form and then deposited into lakes. Geochemical profiles of these elements in lacustrine records are therefore potential palaeoclimatic proxies since there should be a positive correlation between discharge from the catchment and dissolved element input. Flux rates for the dissolved input of uranium Ul(t) and the total allochthonous minerog enic deposit were …

Sediments from Lago di Mezzano, central Italy
Open AccessAntje Ramrath, Laura Sadori et al.ARTICLEThe Holocene2000Cited by: 5References: 7
Microscopic, geochemical and pollen analysis of sediment samples of a Lateglacial/Holocene profile from Lago di Mezzano, a maar lake in central Italy, reveals evidence of significant climatic and human-induced environmental changes. Time control is provided by a combination of varve chronology and radiocarbon dating. The well-known Lateglacial climatic variations, a warmer interstadial and the Younger Dryas cold phase are clearly represented in a…
Precision of Calibrated Radiocarbon Ages of Historic Earthquakes in the Dead Sea Basin
Open AccessRevital Ken-Tor, Mordechai Stein et al.ARTICLERadiocarbon2001Cited by: 4References: 9
The precise determination of the age of historical and geological events by radiocarbon dating is often hampered by the long intersection ranges of the measured data with the calibration curve. In this study we examine the possibility of narrowing the calibrated range of the 14 C ages of earthquake-disturbed sediments (seismites) from the Late Holocene lacustrine section in the Dead Sea Basin. The calibrated ranges of samples collected from seism…
Rapid climate change during the early Holocene in western Europe and Greenland
Open AccessSushma Prasad, Achim Brauer et al.ARTICLEThe Holocene2006Cited by: 1References: 8
Based on microfacies analyses of seasonally laminated varved sediments from lake Holzmaar, Germany, we report evidence of decadal-to century-scale climate variability during the early Holocene. The shifts in climate are documented in the thickness variations and changes in the composition of the varves in response to subtle shifts in limnological conditions. The close similarity between the Holzmaar varve record and the GRIP oxygen isotope record…
Geochemical evidence for Holocene palaeodischarge variations in lacustrine records from the Westeifel Volcanic Field, Germany
Open AccessGeorg Schettler, Bert Rein et al.ARTICLEThe Holocene1999Cited by: 1References: 4
Various chemical elements (Fe, Mn, U, Mo) can be transported in both dissolved and solid form and then deposited into lakes. Geochemical profiles of these elements in lacustrine records are therefore potential palaeoclimatic proxies since there should be a positive correlation between discharge from the catchment and dissolved element input. Flux rates for the dissolved input of uranium Ul(t) and the total allochthonous minerog enic deposit were …