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Plants escaped an ancient mass extinction

Nature (London), 2019-03, Vol.567 (7746), p.1-2

Gastaldo, Robert A

2019

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Ancient plants escaped the end-Permian mass extinction

Nature (London), 2019-03, Vol.567 (7746), p.38-39

Gastaldo, Robert A

2019

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The base of the Lystrosaurus Assemblage Zone, Karoo Basin, predates the end-Permian marine extinction

Nature communications, 2020-03, Vol.11 (1), p.1428-1428, Article 1428

2020

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Comment on: “Anatomy of a mass extinction: Sedimentological and taphonomic evidence for drought-induced die-offs at the Permo–Triassic boundary in the main Karoo Basin, South Africa” by R.M.H. Smith and J. Botha-Brink, Palaeogeography, Palaeoclimatology, Palaeoecology 396:99-118

Palaeogeography, palaeoclimatology, palaeoecology, 2016-04, Vol.447, p.88-91

2016

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Nature through Time: Virtual field trips through the Nature of the past

1st Edition 2020, 2020

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Enigmatic fossil plants with three-dimensional, arborescent-growth architecture from the earliest Carboniferous of New Brunswick, Canada

Current biology, 2024-02, Vol.34 (4), p.781-792.e3

2024

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Peat or no peat: Why do the Rajang and Mahakam Deltas differ?

International journal of coal geology, 2010-08, Vol.83 (2), p.162-172

Gastaldo, Robert A.

2010

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A multidisciplinary approach to review the vertical and lateral facies relationships of the purported vertebrate-defined terrestrial Permian–Triassic boundary interval at Bethulie, Karoo Basin, South Africa

Earth-science reviews, 2019-02, Vol.189, p.220-243

2019

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Portrait of a Gondwanan ecosystem: A new late Permian fossil locality from KwaZulu-Natal, South Africa

Review of palaeobotany and palynology, 2009-09, Vol.156 (3), p.454-493

2009

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Taphonomy and paleobiology

Paleobiology, 2000-12, Vol.26 (sp4), p.103-147

2000

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An autochthonous glossopterid flora with latest Permian palynomorphs and its depositional setting in the Dicynodon Assemblage Zone of the southern Karoo Basin, South Africa

Palaeogeography, palaeoclimatology, palaeoecology, 2010-06, Vol.292 (3), p.391-408

2010

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Trends in Stable Isotopes and Climate Proxies From Late Changhsingian Ghost Landscapes of the Karoo Basin, South Africa

Frontiers in ecology and evolution, 2020-12, Vol.8

2020

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Response of Late Carboniferous and Early Permian Plant Communities to Climate Change

Annual review of earth and planetary sciences, 2001-01, Vol.29 (1), p.461-487

2001

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Ecological persistence in the Late Mississippian (Serpukhovian, Namurian A) megafloral record of the Upper Silesian Basin, Czech Republic

Palaios, 2009-06, Vol.24 (6), p.336-350

2009

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KATBERGIA GEN. NOV., A NEW TRACE FOSSIL FROM UPPER PERMIAN AND LOWER TRIASSIC ROCKS OF THE KAROO BASIN: IMPLICATIONS FOR PALAEOENVIRONMENTAL CONDITIONS AT THE P/TR EXTINCTION EVENT

Palaeontology, 2008-01, Vol.51 (1), p.215-229

2008

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Taphonomic Trends of Macrofloral Assemblages Across the Permian–Triassic Boundary, Karoo Basin, South Africa

Palaios, 2005-10, Vol.20 (5), p.479-497

2005

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Sedimentology and paleontology of a Carboniferous log jam

International journal of coal geology, 2007-01, Vol.69 (1), p.103-118

2007

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The influence of taphonomy and time on the paleobotanical record of the Permian–Triassic transition of the Karoo basin (and elsewhere)

Journal of African earth sciences (1994), 2023-08, Vol.204, p.104960, Article 104960

2023

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Discussion of “Permian—Triassic vertebrate footprints from South Africa: Ichnotaxonomy, producers and biostratigraphy through two major faunal crises” by Marchetti, L., Klein, H., Buchwitz, M., Ronchi, A., Smith, R.M.H., DeKlerk, W.J., Sciscio, L., and Groenewald, G.H. (2019)

Gondwana research, 2020-02, Vol.78, p.375-378

2020

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NO MAJOR STRATIGRAPHIC GAP EXISTS NEAR THE MIDDLE–UPPER PENNSYLVANIAN (DESMOINESIAN–MISSOURIAN) BOUNDARY IN NORTH AMERICA

Palaios, 2011-03, Vol.26 (3), p.125-139

2011

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Editorial: Permian Extinctions

Frontiers in earth science (Lausanne), 2021-09, Vol.9

2021

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Changes in shell durability of common marine taxa through the Phanerozoic: evidence for biological rather than taphonomic drivers

Paleobiology, 2011-03, Vol.37 (2), p.303-331

2011

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The relationship between bedform and log orientation in a Paleogene fluvial channel, Weisselster Basin, Germany; implications for the use of coarse woody debris for paleocurrent analysis

Palaios, 2004-12, Vol.19 (6), p.587-597

Gastaldo, Robert A

2004

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Megafloral perturbation across the Enna Marine Zone in the Upper Silesian Basin attests to Late Mississippian (Serpukhovian) deglaciation and climate change

Palaios, 2009-06, Vol.24 (6), p.351-366

2009

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THE EFFECT OF LEAF ORIENTATION TO SUNLIGHT ON STOMATAL PARAMETERS OF QUERCUS RUBRA AROUND THE BELGRADE LAKES, CENTRAL MAINE

Palaios, 2010-05, Vol.25 (5), p.339-346

2010

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Plants escaped an ancient mass extinction

Ancient plants escaped the end-Permian mass extinction

The base of the Lystrosaurus Assemblage Zone, Karoo Basin, predates the end-Permian marine extinction

Comment on: “Anatomy of a mass extinction: Sedimentological and taphonomic evidence for drought-induced die-offs at the Permo–Triassic boundary in the main Karoo Basin, South Africa” by R.M.H. Smith and J. Botha-Brink, Palaeogeography, Palaeoclimatology, Palaeoecology 396:99-118

Nature through Time: Virtual field trips through the Nature of the past

Enigmatic fossil plants with three-dimensional, arborescent-growth architecture from the earliest Carboniferous of New Brunswick, Canada

Peat or no peat: Why do the Rajang and Mahakam Deltas differ?

A multidisciplinary approach to review the vertical and lateral facies relationships of the purported vertebrate-defined terrestrial Permian–Triassic boundary interval at Bethulie, Karoo Basin, South Africa

Portrait of a Gondwanan ecosystem: A new late Permian fossil locality from KwaZulu-Natal, South Africa

Taphonomy and paleobiology

An autochthonous glossopterid flora with latest Permian palynomorphs and its depositional setting in the Dicynodon Assemblage Zone of the southern Karoo Basin, South Africa

Trends in Stable Isotopes and Climate Proxies From Late Changhsingian Ghost Landscapes of the Karoo Basin, South Africa

Response of Late Carboniferous and Early Permian Plant Communities to Climate Change

Ecological persistence in the Late Mississippian (Serpukhovian, Namurian A) megafloral record of the Upper Silesian Basin, Czech Republic

KATBERGIA GEN. NOV., A NEW TRACE FOSSIL FROM UPPER PERMIAN AND LOWER TRIASSIC ROCKS OF THE KAROO BASIN: IMPLICATIONS FOR PALAEOENVIRONMENTAL CONDITIONS AT THE P/TR EXTINCTION EVENT

Taphonomic Trends of Macrofloral Assemblages Across the Permian–Triassic Boundary, Karoo Basin, South Africa

Sedimentology and paleontology of a Carboniferous log jam

The influence of taphonomy and time on the paleobotanical record of the Permian–Triassic transition of the Karoo basin (and elsewhere)

Discussion of “Permian—Triassic vertebrate footprints from South Africa: Ichnotaxonomy, producers and biostratigraphy through two major faunal crises” by Marchetti, L., Klein, H., Buchwitz, M., Ronchi, A., Smith, R.M.H., DeKlerk, W.J., Sciscio, L., and Groenewald, G.H. (2019)

NO MAJOR STRATIGRAPHIC GAP EXISTS NEAR THE MIDDLE–UPPER PENNSYLVANIAN (DESMOINESIAN–MISSOURIAN) BOUNDARY IN NORTH AMERICA

Editorial: Permian Extinctions

Changes in shell durability of common marine taxa through the Phanerozoic: evidence for biological rather than taphonomic drivers

The relationship between bedform and log orientation in a Paleogene fluvial channel, Weisselster Basin, Germany; implications for the use of coarse woody debris for paleocurrent analysis

Megafloral perturbation across the Enna Marine Zone in the Upper Silesian Basin attests to Late Mississippian (Serpukhovian) deglaciation and climate change

THE EFFECT OF LEAF ORIENTATION TO SUNLIGHT ON STOMATAL PARAMETERS OF QUERCUS RUBRA AROUND THE BELGRADE LAKES, CENTRAL MAINE

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