J Vandenberghe

Datos Biográficos

ID	4131597
NOMBRE	J Vandenberghe
NOMBRES	J
APELLIDO	Vandenberghe
FIRMA	VANDENBERGHE J
AFILIACIONES	Vrije Universiteit Amsterdam
ORCID	0000-0001-9910-1319
VERIFICADO	Sí
TOTAL DE OBRAS	34
TOTAL DE CITAS	7
TOTAL COMO AUTOR	34
TOTAL COMO EDITOR	0
PRIMER AÑO DE PUBLICACIÓN	1985
AÑO MÁS RECIENTE DE PUBLICACIÓN	2025
ÍNDICE H	2

The Late Quaternary Aeolian Deposits in the Subtropical Bose–Bubing Basins, Southern China
Open AccessJiemei Zhong, Ping Lai et al.ARTICLEQuaternary2025
Aeolian deposits are globally recognized as sensitive recorders of Quaternary climate and environmental change, exemplified by the continuous loess sequences of the Chinese Loess Plateau in northern China, which document paleoclimatic and paleoenvironmental evolution since the Miocene. However, such deposits have rarely been confirmed in low-latitude inland regions of southern China. Here we present systematic evidence of aeolian deposition in a …
Aeolian dynamics at the northern edge of Deliblato (Banat) Sand Sea, Vojvodina, Serbia, at the time of the last deglaciation
Open AccessRastko S Marković, Zoran M Perić et al.ARTICLEQuaternary Research2024
The Deliblato (Banat) Sand Sea, which is one of the largest areas of аeolian sand in Europe, is located near the Iron Gate, which marks the crossing of the Danube River through the biggest gorge of this river. Here, Danubian alluvium has served as the sand source for the Banat Sand Sea, which was formed primarily through southeasterly (Košava) winds. Utilizing a multi-proxy approach, the objective of this study is to gain a better understanding o…
Prolonged Response of River Terrace Flooding to Climate Change
Open AccessJ Vandenberghe, Xianyan Wang et al.ARTICLEQuaternary2024
From the start of river incision onward, the abandoned terrace surface is only reached by floods during peak discharges. Two main flood facies are distinguished: a relatively high-energetic, coarse-grained facies and a relatively low-energetic, fine-grained facies. In general, the flood deposits become gradually finer-grained and the finer-grained facies relatively more prominent when the river incises progressively deeper. This signifies a delay…
Local Differentiation in the Loess Deposition as a Function of Dust Source
Open AccessSlobodan B Marković, J Vandenberghe et al.ARTICLEQuaternary2023
Typical patterns of the Late Pleistocene loess–paleosol units are preserved in the Novo Orahovo brickyard, Northern Serbia. Presented preliminary luminescence chronology supports the chronostratigraphic interpretations of global isotopic marine climate reconstructions. Magnetic susceptibility and sedimentological evidence exhibit general similarities with the marine oxygen-isotope stratigraphy. These records provide new insights into the dust acc…
Geomorphological evolution of the Petrovaradin Fortress Palaeolithic site (Novi Sad, Serbia)
Open AccessSlobodan B Marković, J Vandenberghe et al.ARTICLEQuaternary Research2021
Two phases of archaeological investigation were performed in the Novi Sad City Museum at Petrovaradin Fortress. In this study, we summarize the results of geo-archaeological investigations of the second period of excavation inside the Novi Sad City Museum building. The fortress is situated on a Danube terrace with the top of the bedrock at ca.123 m asl. The investigated section consists of undisturbed fine-sandy silt. The grain-size distribution …
Diverse floodplain deposits of reworked loess in a monsoon climate (Hanzhong Basin, central China)
Open AccessJ Vandenberghe, Xun Yang et al.ARTICLEQuaternary Research2021
This paper describes an assemblage of diverse floodplain facies of reworked loess (facies b, c) in a Middle Pleistocene monsoonal setting of the Hanzhong Basin, central China. The vertical and lateral sedimentary sequences show changing energy conditions. Apart from the highest energy in the channel facies (facies a), a relatively high energy floodplain environment (facies b) prevailed in waterlogged conditions, with small, laterally migrating (s…
Extension of the Upper Yellow River into the Tibet Plateau
Open AccessZhengchen Li, Xianyan Wang et al.ARTICLEQuaternary2021
The Wufo Basin at the margin of the northeastern Tibet Plateau connects the upstream reaches of the Yellow River with the lowland catchment downstream, and the fluvial terrace sequence in this basin provides crucial clues to understand the evolution history of the Yellow River drainage system in relation to the uplift and outgrowth of the Tibetan Plateau. Using field survey and analysis of Digital Elevation Model/Google Earth imagery, we found at…
The Sound of ”Quaternary”
Open AccessJ VandenbergheARTICLEQuaternary2020
It is useful to re-consider at specific times the strategy of a journal. Some thoughts are expressed here at the occasion of the renewal of the editorship of ”Quaternary”. No changes are envisaged in the multidisciplinary character of the journal. In addition, it is felt necessary to increasingly attract the creative input from underrepresented researchers in Quaternary science (e.g., young scientists, female scientists, scientists from weakly de…
Quaternary Permafrost in China
Open AccessHuijun Jin, J Vandenberghe et al.ARTICLEQuaternary2020
The framework of Quaternary permafrost in China was reconstructed for the first time on the basis of available periglacial, glacial, and other proxies. During the Early Pleistocene (2.68–0.80 Ma BP), permafrost advanced southwards to 47–50° N in northern China and possibly occurred in alpine regions in western China. During the Middle Pleistocene (800–130 ka BP), permafrost occurred extensively on the Qinghai-Tibet Plateau (QTP) and in alpine or …
Interaction of fluvial and eolian sedimentation processes, and response to climate change since the last glacial in a semiarid environment along the Yellow River
Open AccessXianyan Wang, Junfei Ma et al.ARTICLEQuaternary Research2019
Interactions of fluvial and eolian processes are prominent in dryland environments and can significantly change Earth surface morphology. Here, we report on sediment records of eolian and fluvial interactions since the last glacial period, in the semiarid area of northwest China, at the limit of the Southeast Asian monsoon. Sediment sequences of last glacial and Holocene terraces of the Yellow River are composed of channel gravels, overlain by fl…
Tectonic and climatic controls on Quaternary fluvial processes and river terrace formation in a Mediterranean setting, the Göksu River, southern Turkey
Open AccessNurcan Avşin, J Vandenberghe et al.ARTICLEQuaternary Research2019
Climate and tectonics effect the fluvial evolution of the Mediterranean Mut basin. The basin contains a river terrace staircase of 16 levels (T16–T1) ranging from 365 to 10 m above the current Göksu River in its middle and lower sections. These river terraces records tectonic uplift in the Mut basin. Optically stimulated luminescence (OSL) dating of the fluvial sediments of the youngest terrace (T16) provides a chronology for the assessment of th…
High-resolution proxy record of the environmental response to climatic variations during transition MIS3/MIS2 and MIS2 in Central Europe
Open AccessPál Sümegi, Dávid Molnár et al.ARTICLEQuaternary International2019
Approaches and challenges to the study of loess—Introduction to the LoessFest Special Issue
Open AccessRandall J Schaetzl, E Arthur Bettis et al.ARTICLEQuaternary Research2018
In September 2016, the annual meeting of the International Union for Quaternary Research’s Loess and Pedostratigraphy Focus Group, traditionally referred to as a LoessFest, met in Eau Claire, Wisconsin, USA. The 2016 LoessFest focused on “thin” loess deposits and loess transportation surfaces. This LoessFest included 75 registered participants from 10 countries. Almost half of the participants were from outside the United States, and 18 of the pa…
Episodic Sedimentary Evolution of an Alluvial Fan (Huangshui Catchment, NE Tibetan Plateau)
Open AccessLinman Gao, Xianyan Wang et al.ARTICLEQuaternary2018
Alluvial-fan successions record changes in hydrological processes and environments that may reflect tectonic activity, climate conditions and changes, intrinsic geomorphic changes, or combinations of these factors. Here, we focus on the evolution of a stream-dominated fan in a tectonic depression of the Xining basin of China, laid down under a semi-arid climate in the northeastern Tibetan Plateau (NETP). The fan succession is composed of three fa…
Specific Exogenetic (External) and Endogenetic (Internal) Effects on Fluvial System Evolution
Open AccessJ Vandenberghe, David Bridgland et al.ARTICLEQuaternary2018
A collection of papers appears under the title “Special External Effects on Fluvial System Evolution” in the journal, Quaternary. This is a new Special Issue under the aegis of the Fluvial Archives Group (FLAG), illustrating the recent progress made in paleo-fluvial research. These papers highlight the high complexity of the external forcing of fluvial dynamics, and especially, the combined results of several interfering variables. In addition, i…
Specifying the External Impact on Fluvial Lowland Evolution
Open AccessJ Vandenberghe, C Kasse et al.ARTICLEQuaternary2018
External impact on the development of fluvial systems is generally exerted by changes in sea level, climate and tectonic movements. In this study, it is shown that a regional to local differentiation of fluvial response may be caused by semi-direct effects of climate change and tectonic movement; for example, vegetation cover, frozen soil, snow cover and longitudinal gradient. Such semi-direct effects may be responsible for specific fluvial activ…
Mesolithic–Neolithic settlements Minino 2 and Zamostye 5 in their geo-environmental setting (Upper Volga Lowland, Central Russia)
Open AccessR Gracheva, J Vandenberghe et al.ARTICLEQuaternary International2015
River terraces as a response to climatic forcing
Open AccessJ VandenbergheARTICLEQuaternary International2015
Site-specific variability of loess and palaeosols (Ruma, Vojvodina, northern Serbia)
Open AccessJ Vandenberghe, S B Marković et al.ARTICLEQuaternary International2014
From natural to human-dominated floodplain geoecology - A Holocene perspective for the Dijle catchment, Belgium
Open AccessNils Broothaerts, Gert Verstraeten et al.ARTICLEAnthropocene2014Citada por: 3Referencias: 44
Late Quaternary paleoclimatic and geomorphological evolution at the interface between the Menyuan basin and the Qilian Mountains, northeastern Tibetan Plateau
Open AccessXianyan Wang, Dimitri Vandenberghe et al.ARTICLEQuaternary Research2013
The Tibetan Plateau is regarded as an amplifier and driver of environmental change in adjacent regions because of its extent and high altitude. However, reliable age control for paleoenvironmental information on the plateau is limited. OSL appears to be a valid method to constrain the age of deposits of glacial and fluvial origin, soils and periglacial structures in the Menyuan basin on the northeastern Tibetan Plateau. Dating results show glacie…
Sensitivity of floodplain geoecology to human impact
Open AccessNils Broothaerts, Gert Verstraeten et al.ARTICLEThe Holocene2013Citada por: 4Referencias: 9
Floodplain deposition rates have increased markedly under influence of human impact throughout the late Holocene in many western and central European catchments. Consequently the geomorphology and ecology of many floodplains changed. In this study we discuss this human impact and its influence on the floodplain geoecology during the middle and late Holocene for the headwaters of the Dijle catchment, located in the Belgian loess belt. The floodpla…
Forcing of permafrost retreat
Open AccessJ VandenbergheARTICLEQuaternary International2012
Contrasting dust supply patterns across the north-western Chinese Loess Plateau during the last glacial-interglacial cycle
Open AccessMirjam Vriend, Maarten A Prins et al.ARTICLEQuaternary International2011
Atmospheric circulation patterns in central and eastern Europe during the Weichselian Pleniglacial inferred from loess grain-size records
Open AccessM P Bokhorst, J Vandenberghe et al.ARTICLEQuaternary International2011