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Current Issue

Volume 95,

Number 1,

January 2020

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Impact Factor

1.591

16 out of 53 Paleontology

New Online

A new marine woodground ichnotaxon from the Lower Cretaceous Mannville Group, Saskatchewan, Canada

First evidence of Lower–?Middle Ordovician (Floian–?Dapingian) brachiopods from the Peruvian Altiplano and their paleogeographical significance

Plectatrypinae and other ribbed atrypides succeeding the end Ordovician extinction event, Central Oslo Region, Norway

First report of acrotretoid brachiopod shell beds in the lower Cambrian (Stage 4) Guanshan Biota of eastern Yunnan, South China

The oldest bifoliate cystoporate and two other bryozoan taxa from the Dapingian (Middle Ordovician) of north-western Russia

New onychochilid mollusks from the Middle and Upper Ordovician of Baltica and Laurentia

Redescription of †Yanosteus longidorsalis Jin et al., (Chondrostei, Acipenseriformes, †Peipiaosteidae) from the Early Cretaceous of China

Diversity and systematics of Middle-Late Ordovician calcified cyanobacteria and associated microfossils from Ordos Basin, North China

JPA volume 95 issue 1 Cover and Back matter

Full-text available from the year 2000 to current. Abstracts only from 1998 to 1999, citations only from 1927 to 1997.

Most Read
Most Cited

416 Microconchus cravenensis n. sp.: a giant among microconchid tubeworms

113 Micropaleontology of the lower Mesoproterozoic Roper Group, Australia, and implications for early eukaryotic evolution

42 New small-bodied ornithopods (Dinosauria, Neornithischia) from the Early Cretaceous Wonthaggi Formation (Strzelecki Group) of the Australian-Antarctic rift system, with revision of Qantassaurus intrepidus Rich and Vickers-Rich, 1999

39 New onychochilid mollusks from the Middle and Upper Ordovician of Baltica and Laurentia

37 Stratigraphy, mammalian paleontology, paleoecology, and age correlation of the Wasatch Formation, Fossil Butte National Monument, Wyoming

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Current Issue

Online ISSN 1937-2337
Print ISSN 0022-3360
Copyright © 2021 Paleontological Society

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