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Is it really organic? – Multi-isotopic analysis as a tool to discriminate between organic and conventional plants

Food chemistry, 2013-12, Vol.141 (3), p.2812-2820

2013

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Exhumed hydrocarbon-seep authigenic carbonates from Zakynthos Island (Greece): Concretions not archaeological remains

Marine and petroleum geology, 2016-09, Vol.76, p.16-25

2016

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Seasonality in sea surface temperatures from δ18O in Cladocora caespitosa: modern Adriatic to late Pleistocene, Gulf of Corinth

Journal of quaternary science, 2015-05, Vol.30 (4), p.298-311

2015

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Sedimentary and water column processes in the Oyster Grounds: A potentially hypoxic region of the North Sea

Marine environmental research, 2008-04, Vol.65 (3), p.235-249

2008

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Geochemical constraints on the origin of enigmatic cemented chalks, Norfolk, UK

Geological magazine, 2009-03, Vol.146 (2), p.291-299

2009

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Charophyte growth in small temperate water bodies: Extreme isotopic disequilibrium and implications for the palaeoecology of shallow marl lakes

Palaeogeography, palaeoclimatology, palaeoecology, 2006-10, Vol.240 (3), p.389-404

2006

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Enregistrement des variations climatiques au cours des interglaciaires d'après l'étude des isotopes stables de la calcite de tufs calcaires pléistocènes du nord de la France : exemple des séquences de Caours (SIM 5e; Somme) et de la Celle-sur-Seine (SIM 11; Seine-et-Marne)

Quaternaire (Paris), 2011-12, Vol.22 (4), p.275-283

2011

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High-resolution δ18O seasonality record in a French Eemian tufa stromatolite (Caours, Somme Basin)

Palaeogeography, palaeoclimatology, palaeoecology, 2015-11, Vol.438, p.277-284

2015

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High-resolution delta 18O seasonality record in a French Eemian tufa stromatolite (Caours, Somme Basin)

Palaeogeography, palaeoclimatology, palaeoecology, 2015-11, Vol.438, p.277-284

2015

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Seasonality in sea surface temperatures from [delta]18O in Cladocora caespitosa: modern Adriatic to late Pleistocene, Gulf of Corinth

Journal of quaternary science, 2015-05, Vol.30 (4), p.298

2015

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Seasonality in sea surface temperatures from [delta] super(18)O in Cladocora caespitosa: modern Adriatic to late Pleistocene, Gulf of Corinth

Journal of quaternary science, 2015-05, Vol.30 (4), p.298-311

2015

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Seasonality in sea surface temperatures from δ 18 O in Cladocora caespitosa : modern Adriatic to late Pleistocene, Gulf of Corinth: SEA SURFACE TEMPERATURES FROM CLADOCORA CAESPITOSA

Journal of quaternary science, 2015-05, Vol.30 (4), p.298-311

2015

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Depositional continuity of seasonally laminated tufas: Implications for delta 18O based palaeotemperatures

Global and planetary change, 2010-04, Vol.71 (3-4), p.160-167

2010

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Isotope hydrology of dripwaters in a Scottish cave and implications for stalagmite palaeoclimate research

Hydrology and earth system sciences discussions, 2008-03, Vol.5 (2), p.547-577

2008

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Climatic variations in MIS 11 recorded by stable isotopes and trace elements in a French tufa (La Celle, Seine Valley)

Journal of quaternary science, 2012-11, Vol.27 (8), p.790-799

2012

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Climatic and environmental variations during the last interglacial recorded in a Northern France tufa(Caours, Somme basin). comparisons with regional records

Quaternaire (Paris), 2016-09 (Vol. 27/3), p.249-261

2016

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Stable isotopic evidence for nitrification and denitrification in a High Arctic glacial ecosystem

Biogeochemistry, 2013-05, Vol.113 (1-3), p.341-357

2013

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Rock pool tufa stromatolites on a modern South African wave-cut platform: partial analogues for Archaean stromatolites?

Terra nova (Oxford, England), 2011-12, Vol.23 (6), p.375-381

2011

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Tracing estuarine organic matter sources into the southern North Sea using C and N isotopic signatures

Biogeochemistry, 2013-05, Vol.113 (1-3), p.9-22

2013

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Enregistrement des variations climatiques au cours des interglaciaires d’après l’étude des isotopes stables de la calcite de tufs calcaires pléistocènes du nord de la France : exemple des séquences de Caours (SIM 5e ; Somme) et de La Celle (SIM 11 ; Seine-et-Marne)

Quaternaire (Paris), 2017-03, p.275-283

2017

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Variations climatiques et environnementales au cours du dernier interglaciaire dans un tuf du nord de la France (Caours, bassin de la Somme). Comparaison avec des enregistrements régionaux

Quaternaire (Paris), 2016-09 (27/3), p.249-261

2016

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Tracing estuarine organic matter sources into the southern North Sea using C and N isotopic signatures : Marine Ecosystem Connections: Essential Indicators of Healthy, Productive and Biologically Diverse Seas

Biogeochemistry, 2013, Vol.113 (1-3), p.9-22

2013

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Depositional continuity of seasonally laminated tufas: Implications for δ18O based palaeotemperatures

Global and planetary change, 2010-04, Vol.71 (3-4), p.160-167

2010

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Depositional continuity of seasonally laminated tufas: Implications for δ 18O based palaeotemperatures

Global and planetary change, 2010, Vol.71 (3), p.160-167

2010

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Volume 27 Numéro 3

Quaternaire (Paris), 2016-11

2016

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Is it really organic? – Multi-isotopic analysis as a tool to discriminate between organic and conventional plants

Exhumed hydrocarbon-seep authigenic carbonates from Zakynthos Island (Greece): Concretions not archaeological remains

Seasonality in sea surface temperatures from δ18O in Cladocora caespitosa: modern Adriatic to late Pleistocene, Gulf of Corinth

Sedimentary and water column processes in the Oyster Grounds: A potentially hypoxic region of the North Sea

Geochemical constraints on the origin of enigmatic cemented chalks, Norfolk, UK

Charophyte growth in small temperate water bodies: Extreme isotopic disequilibrium and implications for the palaeoecology of shallow marl lakes

Enregistrement des variations climatiques au cours des interglaciaires d'après l'étude des isotopes stables de la calcite de tufs calcaires pléistocènes du nord de la France : exemple des séquences de Caours (SIM 5e; Somme) et de la Celle-sur-Seine (SIM 11; Seine-et-Marne)

High-resolution δ18O seasonality record in a French Eemian tufa stromatolite (Caours, Somme Basin)

High-resolution delta 18O seasonality record in a French Eemian tufa stromatolite (Caours, Somme Basin)

Seasonality in sea surface temperatures from [delta]18O in Cladocora caespitosa: modern Adriatic to late Pleistocene, Gulf of Corinth

Seasonality in sea surface temperatures from [delta] super(18)O in Cladocora caespitosa: modern Adriatic to late Pleistocene, Gulf of Corinth

Seasonality in sea surface temperatures from δ 18 O in Cladocora caespitosa : modern Adriatic to late Pleistocene, Gulf of Corinth: SEA SURFACE TEMPERATURES FROM CLADOCORA CAESPITOSA

Depositional continuity of seasonally laminated tufas: Implications for delta 18O based palaeotemperatures

Isotope hydrology of dripwaters in a Scottish cave and implications for stalagmite palaeoclimate research

Climatic variations in MIS 11 recorded by stable isotopes and trace elements in a French tufa (La Celle, Seine Valley)

Climatic and environmental variations during the last interglacial recorded in a Northern France tufa(Caours, Somme basin). comparisons with regional records

Stable isotopic evidence for nitrification and denitrification in a High Arctic glacial ecosystem

Rock pool tufa stromatolites on a modern South African wave-cut platform: partial analogues for Archaean stromatolites?

Tracing estuarine organic matter sources into the southern North Sea using C and N isotopic signatures

Enregistrement des variations climatiques au cours des interglaciaires d’après l’étude des isotopes stables de la calcite de tufs calcaires pléistocènes du nord de la France : exemple des séquences de Caours (SIM 5e ; Somme) et de La Celle (SIM 11 ; Seine-et-Marne)

Variations climatiques et environnementales au cours du dernier interglaciaire dans un tuf du nord de la France (Caours, bassin de la Somme). Comparaison avec des enregistrements régionaux

Tracing estuarine organic matter sources into the southern North Sea using C and N isotopic signatures : Marine Ecosystem Connections: Essential Indicators of Healthy, Productive and Biologically Diverse Seas

Depositional continuity of seasonally laminated tufas: Implications for δ18O based palaeotemperatures

Depositional continuity of seasonally laminated tufas: Implications for δ 18O based palaeotemperatures

Volume 27 Numéro 3

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