Abstract is: Liviu Giosan is a Romanian and American marine geologist studying the interactions between climate, landscapes and humans. In the public sphere, he initiated "Ad Astra", an association of scientists from Romania and Romanian diaspora, and has been actively involved in efforts to reform Romania's post-communist science and academia.
human | Q5 |
P227 | GND ID | 1169953786 |
P2671 | Google Knowledge Graph ID | /g/11cn93wns9 |
P496 | ORCID iD | 0000-0001-6769-5204 |
P214 | VIAF ID | 3650154075990111860003 |
P27 | country of citizenship | Romania | Q218 |
P69 | educated at | University of Bucharest | Q608338 |
Stony Brook University | Q969850 | ||
P108 | employer | Woods Hole Oceanographic Institution | Q1404053 |
P734 | family name | Giosan | Q107221580 |
Giosan | Q107221580 | ||
Giosan | Q107221580 | ||
P735 | given name | Liviu | Q28035139 |
Liviu | Q28035139 | ||
P106 | occupation | geologist | Q520549 |
researcher | Q1650915 | ||
P551 | residence | Falmouth | Q1523514 |
P21 | sex or gender | male | Q6581097 |
Q60290293 | 24. Varna Lake (north-eastern Bulgaria): vegetation history and human impact during the last 8000 years |
Q57880928 | A 43 kyr record of protist communities and their response to oxygen minimum zone variability in the Northeastern Arabian Sea |
Q58160336 | A new look at old carbon in active margin sediments |
Q60066798 | Academia resists clean-up in Romania |
Q107613819 | Annually resolved sediments in the classic Clarkia lacustrine deposits (Idaho, USA) during the middle Miocene Climate Optimum |
Q105256256 | Anomalous porosity preservation and preferential accumulation of gas hydrate in the Andaman accretionary wedge, NGHP-01 site 17A |
Q59304072 | Anthropocene metamorphosis of the Indus Delta and lower floodplain |
Q112603405 | Approaches to defining deltaic sustainability in the 21st century |
Q57090033 | Arctic Deltaic Lake Sediments As Recorders of Fluvial Organic Matter Deposition |
Q116977763 | Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years |
Q113643347 | Black Sea paleosalinity evolution since the last deglaciation reconstructed from alkenone-inferred Isochrysidales diversity |
Q59840002 | Branched GDGT signals in fluvial sediments of the Danube River basin: Method comparison and longitudinal evolution |
Q59840031 | Branched glycerol dialkyl glycerol tetraethers in Arctic lake sediments: Sources and implications for paleothermometry at high latitudes |
Q30874175 | Climate change: protect the world's deltas. |
Q38669062 | Climate oscillations reflected within the microbiome of Arabian Sea sediments. |
Q53070222 | Climatic control of Mississippi River flood hazard amplified by river engineering. |
Q58408935 | Comment on “Geochemistry of buried river sediments from Ghaggar Plains, NW India: Multi-proxy records of variations in provenance, paleoclimate, and paleovegetation patterns in the late quaternary” by Ajit Singh, Debajyoti Paul, Rajiv Sinha, Kris |
Q59839961 | Constraining Instantaneous Fluxes and Integrated Compositions of Fluvially Discharged Organic Matter |
Q60164980 | Contributions to the European Pollen Database. 22. Vegetation development in the central part of the Bulgarian Black Sea coast during the last 13 000 years |
Q59840007 | Corrigendum to “Branched GDGT signals in fluvial sediments of the Danube River basin: Method comparison and longitudinal evolution” [Organic Geochem. 103 (2017) 88–96] |
Q100515428 | Corrigendum to “Comment on “Landscape change and archaeological settlements in the lower Danube valley and delta from early Neolithic to Chalcolithic time: A review” by Jean-Michel Carozza, Christian Micu, Florian Mihail, Laurent Carozza (Quate |
Q60164987 | DNA and lipid molecular stratigraphic records of haptophyte succession in the Black Sea during the Holocene |
Q28601650 | Decrease in coccolithophore calcification and CO2 since the middle Miocene |
Q28728167 | Early anthropogenic transformation of the Danube-Black Sea system |
Q111729197 | Enhanced Late Miocene Chemical Weathering and Altered Precipitation Patterns in the Watersheds of the Bay of Bengal Recorded by Detrital Clay Radiogenic Isotopes |
Q113102371 | Enhancing mud supply from the Lower Missouri River to the Mississippi River Delta USA: Dam bypassing and coastal restoration |
Q59839982 | Evolution of biomolecular loadings along a major river system |
Q28686151 | Evolution of the plankton paleome in the Black Sea from the Deglacial to Anthropocene |
Q60164981 | First high-resolution marinopalynological stratigraphy of Late Quaternary sediments from the central part of the Bulgarian Black Sea area |
Q28727737 | Fluvial landscapes of the Harappan civilization |
Q30722099 | Fluvial response to climate variations and anthropogenic perturbations for the Ebro River, Spain in the last 4,000 years |
Q117424590 | From soil to sea: sources and transport of organic carbon traced by tetraether lipids in the monsoonal Godavari River, India |
Q60142346 | Geochemical record of Holocene to Recent sedimentation on the Western Indus continental shelf, Arabian Sea |
Q57575913 | High-resolution and high-precision correlation of dark and light layers in the Quaternary hemipelagic sediments of the Japan Sea recovered during IODP Expedition 346 |
Q61469220 | Holocene aridification of India |
Q57604044 | Holocene erosion of the Lesser Himalaya triggered by intensified summer monsoon |
Q57850068 | Holocene palaeoenvironmental evolution of the Ebro Delta (Western Mediterranean Sea): Evidence for an early construction based on the benthic foraminiferal record |
Q63645916 | Holocene paleodepositional changes reflected in the sedimentary microbiome of the Black Sea |
Q114177226 | Human practices behind the aquatic and terrestrial ecological decoupling to climate change in the tropical Andes |
Q106957615 | Impacts of sediment supply and local tectonics on clinoform distribution: the seismic stratigraphy of the mid Pleistocene-Holocene Indus Shelf |
Q57564625 | Indian monsoon variations during three contrasting climatic periods: The Holocene, Heinrich Stadial 2 and the last interglacial–glacial transition |
Q117743044 | Influence of Hydraulic Connectivity on Carbon Burial Efficiency in Mackenzie Delta Lake Sediments |
Q60058673 | Influence of total organic carbon deposition on the inventory of gas hydrate in the Indian continental margins |
Q106730117 | Intercomparison of XRF Core Scanning Results From Seven Labs and Approaches to Practical Calibration |
Q114556484 | Large deltas, small deltas: Toward a more rigorous understanding of coastal marine deltas |
Q63406164 | Large-scale coastal and fluvial models constrain the late Holocene evolution of the Ebro Delta |
Q105620122 | Late Quaternary vegetation and climate of SE Europe–NW Asia according to pollen records in three offshore cores from the Black and Marmara seas |
Q60058674 | Long-timescale variation in bulk and clay mineral composition of Indian continental margin sediments in the Bay of Bengal, Arabian Sea, and Andaman Sea |
Q53586627 | Marginal deltaic coasts in transition: From natural to anthropogenic along the southern Romanian cliffed coast |
Q57603985 | Monsoon control over erosion patterns in the Western Himalaya: possible feed-back into the tectonic evolution |
Q60058676 | Monsoon-influenced variation in productivity and lithogenic sediment flux since 110 ka in the offshore Mahanadi Basin, northern Bay of Bengal |
Q57880925 | Neoglacial Climate Anomalies and the Harappan Metamorphosis |
Q60131817 | Neoglacial climate anomalies and the Harappan metamorphosis |
Q111729133 | No modern Irrawaddy River until the late Miocene-Pliocene |
Q58408916 | On the Holocene Evolution of the Ayeyawady Megadelta |
Q58408904 | On the Holocene evolution of the Ayeyawady megadelta |
Q114742636 | Palaeoecology and Geoarchaeology of Varna Lake, Northeastern Bulgaria |
Q114107248 | Pliocene expansion of C4 vegetation in the Core Monsoon Zone on the Indian Peninsula |
Q111729207 | Provenance and Weathering of Clays Delivered to the Bay of Bengal During the Middle Miocene: Linkages to Tectonics and Monsoonal Climate |
Q61905799 | Radiogenic fingerprinting reveals anthropogenic and buffering controls on sediment dynamics of the Mississippi River system |
Q59839970 | Reconciling drainage and receiving basin signatures of the Godavari River system |
Q57745070 | SHORT COMMUNICATION: Massive Erosion in Monsoonal Central India Linked to Late Holocene Landcover Degradation |
Q113361698 | Sediment storage and reworking on the shelf and in the Canyon of the Indus River-Fan System since the last glacial maximum |
Q57745042 | Short communication: Massive erosion in monsoonal central India linked to late Holocene land cover degradation |
Q57150238 | Sinking deltas due to human activities |
Q58459794 | South Asian monsoon history over the past 60 kyr recorded by radiogenic isotopes and clay mineral assemblages in the Andaman Sea |
Q58395266 | Spatial variations in geochemical characteristics of the modern Mackenzie Delta sedimentary system |
Q104067227 | Subseafloor Archaea reflect 139 kyrs of paleodepositional changes in the northern Red Sea |
Q109317027 | Temporal deconvolution of vascular plant-derived fatty acids exported from terrestrial watersheds |
Q63226580 | The Geographic, Geological and Oceanographic Setting of the Indus River |
Q63257728 | The Mighty Susquehanna—Extreme Floods in Eastern North America During the Past Two Millennia |
Q39134352 | Tracing the Vedic Saraswati River in the Great Rann of Kachchh |
Q57603803 | U-PB Detrital Zircon Geochronology of the Lower Danube and Its Tributaries: Implications for the Geology of the Carpathians |
Q55952006 | Was the Black Sea catastrophically flooded in the early Holocene? |
Q104602276 | Wave-angle control of delta evolution |
Q58081355 | What makes a delta wave-dominated? |
Q59746264 | Young Danube delta documents stable Black Sea level since the middle Holocene: Morphodynamic, paleogeographic, and archaeological implications |