Liviu Giosan

Dados Biográficos

ID	387361
NOME	Liviu Giosan
PRENOMES	Liviu
SOBRENOME	Giosan
ASSINATURA	GIOSAN L
AFILIAÇÕES	Woods Hole Oceanographic Institution
ORCID	0000-0001-6769-5204
VERIFICADO	Sim
TOTAL DE OBRAS	19
TOTAL DE CITAÇÕES	14
TOTAL COMO AUTOR	19
TOTAL COMO EDITOR	0
PRIMEIRO ANO DE PUBLICAÇÃO	2009
ANO MAIS RECENTE DE PUBLICAÇÃO	2025
ÍNDICE H	2

The Flooding of Lagash (Iraq)
Open AccessReed Goodman, Liviu Giosan et al.ARTICLEGeoarchaeology2025Referências: 3
High‐resolution remote sensing, magnetometry, and trench stratigraphy identify a significant flood event at Lagash (modern Tell al‐Hiba) during the late Early Dynastic period (ca. 2400–2350 BC ). Satellite imagery and magnetometry reveal a 90‐meter‐wide meander belt—3–15 times broader than documented canals—adjacent to primary temple districts. Test trenches further exposed over one meter of flood‐deposited silt covering existing architecture. Op…
Emerging climate threats to the Mississippi River Delta
Open AccessJohn W Day, Yanqing Xu et al.ARTICLEOne Earth2024
Adaptation for changing deltas
Open AccessTuhin Ghosh, Ho Huu Loc et al.ARTICLEOne Earth2023
Response to Emily Hammer’s article
Open AccessHolly Pittman, Reed Goodman et al.ARTICLEJournal of Anthropological…2023Referências: 11
Holocene paleoenvironmental changes in the marginal marine basin of Great Rann of Kachchh, western India
Open AccessAbhishek Kumar, D M Maurya et al.ARTICLEQuaternary International2021
A Brief Commentary on the Interpretation of Chinese Speleothem δ18O Records as Summer Monsoon Intensity Tracers
Open AccessDaniel Gebregiorgis, Steven C Clemen et al.ARTICLEQuaternary2020
Zhang et al [...]
Using Stable Carbon Isotopes to Quantify Radiocarbon Reservoir Age Offsets in the Coastal Black Sea
Open AccessGuillaume Soulet, Liviu Giosan et al.ARTICLERadiocarbon2019Citada por: 2Referências: 58
Constraining radiocarbon ( 14 C) reservoir age offsets is critical to deriving accurate calendar-age chronologies from 14 C dating of materials which did not draw carbon directly from the atmosphere. The application of 14 C dating to such materials is severely limited in hydrologically sensitive environments like the Black Sea because of the difficulty to quantify reservoir age offsets, which can vary quickly and significantly through time, due t…
Marginal deltaic coasts in transition
Open AccessConstantinescu, Stefan Constantinescu et al.ARTICLEAnthropocene2017Referências: 19
Multi-proxy records of Holocene palaeoenvironmental changes in the Varna Lake area, western Black Sea coast
Open AccessMariana Filipova-Marinova, Danail Pavlov et al.ARTICLEQuaternary International2016
Holocene palaeoenvironmental evolution of the Ebro Delta (Western Mediterranean Sea)
Open AccessAlejandro Cearreta, Xavier Benito et al.ARTICLEThe Holocene2016Citada por: 2Referências: 2
Major Mediterranean deltas began to develop during a period between 8000 and 6000 yr BP when the rate of fluvial sediment input overtook the declining rate of sea-level rise. However, different authors have argued that the Ebro Delta primarily formed during the late Middle Ages as a consequence of increased anthropogenic pressure on its river basin and these arguments are supported by the scarcity of previous geological studies and available radi…
Evolution of Chilia lobes of the Danube delta
Open AccessFlorin Filip, Liviu GiosanARTICLEAnthropocene2014Referências: 19
Comment on “Landscape change and archaeological settlements in the lower Danube valley and delta from early Neolithic to Chalcolithic time
Open AccessLiviu GiosanARTICLEQuaternary International2013
First high-resolution marinopalynological stratigraphy of Late Quaternary sediments from the central part of the Bulgarian Black Sea area
Open AccessMariana Filipova-Marinova, Danail Pavlov et al.ARTICLEQuaternary International2013
Maintenance of large deltas through channelization
Open AccessLiviu Giosan, Constantinescu et al.ARTICLEAnthropocene2013Citada por: 2Referências: 40
Anthropocene metamorphosis of the Indus Delta and lower floodplain
Open AccessJames P M Syvitski, Albert J Kettner et al.ARTICLEAnthropocene2013Referências: 19
Clay mineral variations in Holocene terrestrial sediments from the Indus Basin
Open AccessAnwar Alizai, Stephen Hillier et al.ARTICLEQuaternary Research2012
We employed X-ray diffraction methods to quantify clay mineral assemblages in the Indus Delta and flood plains since ~ 14 ka, spanning a period of strong climatic change. Assemblages are dominated by smectite and illite, with minor chlorite and kaolinite. Delta sediments integrate clays from across the basin and show increasing smectite input between 13 and 7.5 ka, indicating stronger chemical weathering as the summer monsoon intensified. Changes…
Fluvial landscapes of the Harappan civilization
Open AccessLiviu Giosan, Peter D Clift et al.ARTICLEProceedings of the National…2012
The collapse of the Bronze Age Harappan, one of the earliest urban civilizations, remains an enigma. Urbanism flourished in the western region of the Indo-Gangetic Plain for approximately 600 y, but since approximately 3,900 y ago, the total settled area and settlement sizes declined, many sites were abandoned, and a significant shift in site numbers and density towards the east is recorded. We report morphologic and chronologic evidence indicati…
Simulating fluvial fluxes in the Danube watershed
Open AccessKerry McCarney-Castle, G Voulgaris et al.ARTICLEThe Holocene2011Citada por: 8Referências: 4
Climate change and human activities in Europe have altered erosion and riverine sediment transport for thousands of years. The Danube River basin, the second largest watershed in Europe, provides a unique study area to examine these impacts on fluvial discharge through available reconstructed climate data during the ‘Little Ice Age’ cold interval, as well as documented timing of deforestation and large dam emplacement. Suspended sediment flux of …
Sinking deltas due to human activities
Open AccessJames P M Syvitski, Albert J Kettner et al.ARTICLENature Geoscience2009

Simulating fluvial fluxes in the Danube watershed
Open AccessKerry McCarney-Castle, G Voulgaris et al.ARTICLEThe Holocene2011Citada por: 8Referências: 4
Climate change and human activities in Europe have altered erosion and riverine sediment transport for thousands of years. The Danube River basin, the second largest watershed in Europe, provides a unique study area to examine these impacts on fluvial discharge through available reconstructed climate data during the ‘Little Ice Age’ cold interval, as well as documented timing of deforestation and large dam emplacement. Suspended sediment flux of …
Using Stable Carbon Isotopes to Quantify Radiocarbon Reservoir Age Offsets in the Coastal Black Sea
Open AccessGuillaume Soulet, Liviu Giosan et al.ARTICLERadiocarbon2019Citada por: 2Referências: 58
Constraining radiocarbon ( 14 C) reservoir age offsets is critical to deriving accurate calendar-age chronologies from 14 C dating of materials which did not draw carbon directly from the atmosphere. The application of 14 C dating to such materials is severely limited in hydrologically sensitive environments like the Black Sea because of the difficulty to quantify reservoir age offsets, which can vary quickly and significantly through time, due t…
Holocene palaeoenvironmental evolution of the Ebro Delta (Western Mediterranean Sea)
Open AccessAlejandro Cearreta, Xavier Benito et al.ARTICLEThe Holocene2016Citada por: 2Referências: 2
Major Mediterranean deltas began to develop during a period between 8000 and 6000 yr BP when the rate of fluvial sediment input overtook the declining rate of sea-level rise. However, different authors have argued that the Ebro Delta primarily formed during the late Middle Ages as a consequence of increased anthropogenic pressure on its river basin and these arguments are supported by the scarcity of previous geological studies and available radi…
Maintenance of large deltas through channelization
Open AccessLiviu Giosan, Constantinescu et al.ARTICLEAnthropocene2013Citada por: 2Referências: 40