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Volume 37, Number 5

May 2022

ISSN 0883-1351

EISSN 1938-5323

CESSATION OF A SUBTROPICAL GLASS RAMP DURING THE PERMIAN CHERT EVENT: MURDOCK MOUNTAIN FORMATION, WESTERN U.S.A.

ZACK WISTORT; KATHLEEN RITTERBUSH; SEANA C. HOOD

Abstract

View articletitled, CESSATION OF A SUBTROPICAL GLASS RAMP DURING THE PERMIAN CHERT EVENT: MURDOCK MOUNTAIN FORMATION, WESTERN U.S.A.

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PALAIOS May 24, 2022, Vol.37, 129-144. doi:https://doi.org/10.2110/palo.2021.034

IS ABERRANCY A RELIABLE INDICATOR FOR MAJOR PALEOCLIMATIC DISTURBANCE?

STEPHEN STUKINS

Abstract

View articletitled, IS ABERRANCY A RELIABLE INDICATOR FOR MAJOR PALEOCLIMATIC DISTURBANCE?

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PALAIOS May 24, 2022, Vol.37, 145-149. doi:https://doi.org/10.2110/palo.2021.019

TAPHONOMIC CONTROLS ON MICROBIALITE TEXTURES FROM THE STEAMBOAT POINT MEMBER, UPPER ORDOVICIAN BIGHORN DOLOMITE, WESTERN TETON MOUNTAINS, USA

ANDREW BAYS; YADIRA IBARRA; SONICAH SANON; CLIVE HAYZELDEN

Abstract

View articletitled, TAPHONOMIC CONTROLS ON MICROBIALITE TEXTURES FROM THE STEAMBOAT POINT MEMBER, UPPER ORDOVICIAN BIGHORN DOLOMITE, WESTERN TETON MOUNTAINS, USA

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PALAIOS May 24, 2022, Vol.37, 150-164. doi:https://doi.org/10.2110/palo.2021.042

LOWER CAMBRIAN RUSOPHYCUS FROM ELLESMERE ISLAND, ARCTIC CANADA: ICHNOFOSSIL OF A PREDATORY, NON-TRILOBITE ARTHROPOD

BRIAN R. PRATT

Abstract

View articletitled, LOWER CAMBRIAN <em>RUSOPHYCUS</em> FROM ELLESMERE ISLAND, ARCTIC CANADA: ICHNOFOSSIL OF A PREDATORY, NON-TRILOBITE ARTHROPOD

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PALAIOS May 27, 2022, Vol.37, 165-184. doi:https://doi.org/10.2110/palo.2021-066

DYNAMICS OF DEPOSITION AND FOSSIL PRESERVATION AT THE EARLY EOCENE OKANAGAN HIGHLANDS OF BRITISH COLUMBIA, CANADA: INSIGHTS FROM ORGANIC GEOCHEMISTRY

ALEXANDER J. LOWE; AARON F. DIEFENDORF; KRISTEN M. SCHLANSER; JAMES SUPER; CHRISTOPHER K. WEST; DAVID R. GREENWOOD

Abstract

View articletitled, DYNAMICS OF DEPOSITION AND FOSSIL PRESERVATION AT THE EARLY EOCENE OKANAGAN HIGHLANDS OF BRITISH COLUMBIA, CANADA: INSIGHTS FROM ORGANIC GEOCHEMISTRY

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PALAIOS May 31, 2022, Vol.37, 185-200. doi:https://doi.org/10.2110/palo.2021.007

ICHNOLOGY OF MUDDY SHALLOW-WATER CONTOURITES FROM THE UPPER JURASSIC–LOWER CRETACEOUS VACA MUERTA FORMATION, ARGENTINA: IMPLICATIONS FOR TRACE-FOSSIL MODELS

MAXIMILIANO PAZ; M. GABRIELA MÁNGANO; LUIS A. BUATOIS; PATRICIO R. DESJARDINS; RAÚL NOTTA; FEDERICO GONZÁLEZ TOMASSINI; NOELIA B. CARMONA

Abstract

View articletitled, ICHNOLOGY OF MUDDY SHALLOW-WATER CONTOURITES FROM THE UPPER JURASSIC–LOWER CRETACEOUS VACA MUERTA FORMATION, ARGENTINA: IMPLICATIONS FOR TRACE-FOSSIL MODELS

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PALAIOS May 31, 2022, Vol.37, 201-218. doi:https://doi.org/10.2110/palo.2020.028

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COVER EXPLANATION.—Montello Canyon chert tubes, Montello Canyon, Permian, Nevada, USA.
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CESSATION OF A SUBTROPICAL GLASS RAMP DURING THE PERMIAN CHERT EVENT: MURDOCK MOUNTAIN FORMATION, WESTERN U.S.A.

IS ABERRANCY A RELIABLE INDICATOR FOR MAJOR PALEOCLIMATIC DISTURBANCE?

TAPHONOMIC CONTROLS ON MICROBIALITE TEXTURES FROM THE STEAMBOAT POINT MEMBER, UPPER ORDOVICIAN BIGHORN DOLOMITE, WESTERN TETON MOUNTAINS, USA

LOWER CAMBRIAN RUSOPHYCUS FROM ELLESMERE ISLAND, ARCTIC CANADA: ICHNOFOSSIL OF A PREDATORY, NON-TRILOBITE ARTHROPOD

DYNAMICS OF DEPOSITION AND FOSSIL PRESERVATION AT THE EARLY EOCENE OKANAGAN HIGHLANDS OF BRITISH COLUMBIA, CANADA: INSIGHTS FROM ORGANIC GEOCHEMISTRY

ICHNOLOGY OF MUDDY SHALLOW-WATER CONTOURITES FROM THE UPPER JURASSIC–LOWER CRETACEOUS VACA MUERTA FORMATION, ARGENTINA: IMPLICATIONS FOR TRACE-FOSSIL MODELS

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CESSATION OF A SUBTROPICAL GLASS RAMP DURING THE PERMIAN CHERT EVENT: MURDOCK MOUNTAIN FORMATION, WESTERN U.S.A.

IS ABERRANCY A RELIABLE INDICATOR FOR MAJOR PALEOCLIMATIC DISTURBANCE?

TAPHONOMIC CONTROLS ON MICROBIALITE TEXTURES FROM THE STEAMBOAT POINT MEMBER, UPPER ORDOVICIAN BIGHORN DOLOMITE, WESTERN TETON MOUNTAINS, USA

LOWER CAMBRIAN RUSOPHYCUS FROM ELLESMERE ISLAND, ARCTIC CANADA: ICHNOFOSSIL OF A PREDATORY, NON-TRILOBITE ARTHROPOD

DYNAMICS OF DEPOSITION AND FOSSIL PRESERVATION AT THE EARLY EOCENE OKANAGAN HIGHLANDS OF BRITISH COLUMBIA, CANADA: INSIGHTS FROM ORGANIC GEOCHEMISTRY

ICHNOLOGY OF MUDDY SHALLOW-WATER CONTOURITES FROM THE UPPER JURASSIC–LOWER CRETACEOUS VACA MUERTA FORMATION, ARGENTINA: IMPLICATIONS FOR TRACE-FOSSIL MODELS

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