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1
Datasets archeologisch syntheseonderzoek "Door de bomen het bos zien": palynologie, macrobotanie, radiokoolstof-dateringen
Datasets archeologisch syntheseonderzoek "Door de bomen het bos zien": palynologie, macrobotanie, radiokoolstof-dateringen
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Datasets archeologisch syntheseonderzoek "Door de bomen het bos zien": palynologie, macrobotanie, radiokoolstof-dateringen

Wouter van der Meer ; Bart Cherretté ; Cateline Clement

Zenodo 2021

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2
Cross-border correlations showing diachronous lithostratigraphic units in the southeastern North Sea Basin during the Early Oligocene (middle-late Rupelian)
Cross-border correlations showing diachronous lithostratigraphic units in the southeastern North Sea Basin during the Early Oligocene (middle-late Rupelian)
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Cross-border correlations showing diachronous lithostratigraphic units in the southeastern North Sea Basin during the Early Oligocene (middle-late Rupelian)

Munsterman, Dirk K. ; Deckers, Jef

Netherlands Journal of Geosciences, 2024-05, Vol.103

Cambridge, UK: Cambridge University Press

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3
A proposal for an updated and revised stratigraphical framework of the Miocene in the Achterhoek (eastern Netherlands)
A proposal for an updated and revised stratigraphical framework of the Miocene in the Achterhoek (eastern Netherlands)
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A proposal for an updated and revised stratigraphical framework of the Miocene in the Achterhoek (eastern Netherlands)

Munsterman, Dirk K. ; Van den Bosch, Maarten ; Wesselingh, Frank P. ; Helwerda, Marian ; Busschers, Freek S.

Geologie en mijnbouw, 2024-04, Vol.103

Cambridge, UK: Cambridge University Press

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4
Eemian to Early Weichselian regional and local vegetation development and sedimentary and geomorphological controls, Amersfoort Basin, The Netherlands
Eemian to Early Weichselian regional and local vegetation development and sedimentary and geomorphological controls, Amersfoort Basin, The Netherlands
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Eemian to Early Weichselian regional and local vegetation development and sedimentary and geomorphological controls, Amersfoort Basin, The Netherlands

Kasse, Cees ; van der Woude, John D. ; Woolderink, Hessel A. G. ; Schokker, Jeroen

Geologie en mijnbouw, 2022-01, Vol.101, Article e7

Cambridge, UK: Cambridge University Press

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5
The Lower Rhine (Germany) in Late Antiquity: a time of dissolving structures
The Lower Rhine (Germany) in Late Antiquity: a time of dissolving structures
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The Lower Rhine (Germany) in Late Antiquity: a time of dissolving structures

Gerlach, Renate ; Meurers-Balke, Jutta ; Kalis, Arie J.

Geologie en mijnbouw, 2022-01, Vol.101, Article e14

Cambridge, UK: Cambridge University Press

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6
Waldo Heliodoor Zagwijn (1928–2018): the instigator and architect of European chronostratigraphy
Waldo Heliodoor Zagwijn (1928–2018): the instigator and architect of European chronostratigraphy
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Waldo Heliodoor Zagwijn (1928–2018): the instigator and architect of European chronostratigraphy

Hooghiemstra, Henry ; Hoek, Wim Z.

Netherlands Journal of Geosciences, 2019, Vol.98, Article e7

Dordrecht: Cambridge University Press

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7
Aspects of Permian palaeobotany and palynology. XVIII. On the morphology and ultrastructure of Potonieisporites novicus (prepollen of Late Carboniferous/Early Permian Walchiaceae)
Aspects of Permian palaeobotany and palynology. XVIII. On the morphology and ultrastructure of Potonieisporites novicus (prepollen of Late Carboniferous/Early Permian Walchiaceae)
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Aspects of Permian palaeobotany and palynology. XVIII. On the morphology and ultrastructure of Potonieisporites novicus (prepollen of Late Carboniferous/Early Permian Walchiaceae)

Poort, Ruud J. ; Veld, Harry

Acta Botanica Neerlandica, 1997-06, Vol.46 (2), p.161-173 [Periódico revisado por pares]

Koninklijke Nederlandse Botanische Vereniging

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8
Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands – northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly summer winds
Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands – northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly summer winds
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Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands – northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly summer winds

Kasse, Cornelis ; Woolderink, Hessel A.G. ; Kloos, Marjan E. ; Hoek, Wim Z.

Geologie en mijnbouw, 2020, Vol.99, Article e13

Cambridge, UK: Cambridge University Press

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9
PALYNOLOGY OF THE MIDDLE PART (30–78 METRES) OF THE 120 M DEEP SECTION IN NORTHERN GREECE (MACEDONIA)
PALYNOLOGY OF THE MIDDLE PART (30–78 METRES) OF THE 120 M DEEP SECTION IN NORTHERN GREECE (MACEDONIA)
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PALYNOLOGY OF THE MIDDLE PART (30–78 METRES) OF THE 120 M DEEP SECTION IN NORTHERN GREECE (MACEDONIA)

Wijmstra, T. A. ; Smit, A.

Acta Botanica Neerlandica, 1976-08, Vol.25 (4), p.297-312 [Periódico revisado por pares]

Koninklijke Nederlandse Botanische Vereniging

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10
PALYNOLOGY OF A SECTION FROM THE RAISED PEAT BOG ‘WIETMARSCHER MOOR‘, WITH SPECIAL REFERENCE TO FUNGAL REMAINS
PALYNOLOGY OF A SECTION FROM THE RAISED PEAT BOG ‘WIETMARSCHER MOOR‘, WITH SPECIAL REFERENCE TO FUNGAL REMAINS
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PALYNOLOGY OF A SECTION FROM THE RAISED PEAT BOG ‘WIETMARSCHER MOOR‘, WITH SPECIAL REFERENCE TO FUNGAL REMAINS

Van Geel, B.

Acta Botanica Neerlandica, 1972-06, Vol.21 (3), p.261-284 [Periódico revisado por pares]

Koninklijke Nederlandse Botanische Vereniging

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