ProfessorsProfessors of University of Wisconsin-MilwaukeeStephen Q. Dornbos

Stephen Q. Dornbos

University of Wisconsin-Milwaukee

H-index: 23

North America-United States

About Stephen Q. Dornbos

Stephen Q. Dornbos, With an exceptional h-index of 23 and a recent h-index of 16 (since 2020), a distinguished researcher at University of Wisconsin-Milwaukee, specializes in the field of Paleoecology, Paleobiology, Geobiology, Geochemistry.

His recent articles reflect a diverse array of research interests and contributions to the field:

Multiple sustained increases in atmospheric oxygen and marine productivity through the Neoproterozoic and Paleozoic Eras

The sedimentary geochemistry and paleoenvironments project

The composition and weathering of the continents over geologic time

Evidence for a local reef eclipse in a shallow marine carbonate environment following the regional extinction of archaeocyaths in Laurentia (Stage 4, Cambrian)

Stephen Q. Dornbos Information

University	University of Wisconsin-Milwaukee
Position	___
Citations(all)	2253
Citations(since 2020)	584
Cited By	1916
hIndex(all)	23
hIndex(since 2020)	16
i10Index(all)	31
i10Index(since 2020)	22
Email	Access Email
University Profile Page	University of Wisconsin-Milwaukee
Google Scholar	View Google Scholar Profile

Stephen Q. Dornbos Skills & Research Interests

Paleoecology

Paleobiology

Geobiology

Geochemistry

Top articles of Stephen Q. Dornbos

Title	Journal	Author(s)	Publication Date
Multiple sustained increases in atmospheric oxygen and marine productivity through the Neoproterozoic and Paleozoic Eras		Richard Stockey Devon Cole Una Farrell Heda Agić Thomas Boag ...	2023/11/14
The sedimentary geochemistry and paleoenvironments project	Geobiology	Úna C Farrell Rifaat Samawi Savitha Anjanappa Roman Klykov Oyeleye O Adeboye ...	2021/11
The composition and weathering of the continents over geologic time		Alex George Lipp Oliver Shorttle Erik Sperling Jochen J Brocks Devon Cole ...	2020/8/21
Evidence for a local reef eclipse in a shallow marine carbonate environment following the regional extinction of archaeocyaths in Laurentia (Stage 4, Cambrian)	Facies	David R Cordie Stephen Q Dornbos Pedro J Marenco	2020/1