Richard K. Olsson

Lund University

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

Kenneth G. Miller

Rutgers, The State University of New Jersey

William A. Berggren

Woods Hole Oceanographic Institution

James V. Browning

Rutgers, The State University of New Jersey

Peter J. Sugarman

Behavioral Tech Research, Inc.

Christoph Hemleben

University of Tübingen

Mark D. Feigenson

Rutgers, The State University of New Jersey

Bridget S. Wade

University College London

James D. Wright

Rutgers, The State University of New Jersey

Paul N. Pearson

University College London

Brian T. Huber

National Museum of Natural History

Cooperative Institutions

Rutgers, The State University of New Jersey

United States Geological Survey

Rutgers Sexual and Reproductive Health and Rights

Lamont-Doherty Earth Observatory

Columbia University

Rütgers (Germany)

Planetary Science Institute

Lund University

Woods Hole Oceanographic Institution

Scripps Institution of Oceanography

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

WALL TEXTURES OF OLIGOCENE NORMAL PERFORATE PLANKTONIC FORAMINIFERA

Christoph Hemleben Richard K. Olsson Vlasta Premec Fuček Morana Hernitz Kučenjak

Source

Cite

Citations (3)

Presentation of the 2013 Charles Schuchert Award of the Paleontological Society to Bridget S. Wade

Journal of Paleontology (2014)

Richard K. Olsson

An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.

Presentation (obstetrics)

Content (measure theory)

Link (geometry)

10.1666/0022-3360-88.3.622

Cite

Citations (0)

TAXONOMY, BIOSTRATIGRAPHY, AND PHYLOGENY OF EOCENE DENTOGLOBIGERINA

Richard K. Olsson Christoph Hemleben Paul N. Pearson

Source

Cite

Citations (4)

Shore Laboratory Report on the Foraminifera from Leg 27 Sites, Deep Sea Drilling Project

U.S. Government Printing Office eBooks (1974)

Richard K. Olsson

Tables 1 through 5 show the distribution of planktonic foraminifera at Leg 27 sites, with indication of abundance and preservation.The symbols used in the tables are as follows:Relative Abundance 0-Absent 1-Rare (1-10 specimens) 2-Moderately rare (11-25 specimens) 3-Common (26-50 specimens) 4-Abundant (51-100 specimens)5-Very abundant (100 specimens) *-Hundred to thousands of specimens P-Present

10.2973/dsdp.proc.27.144.1974

Cite

Citations (2)

Phylogeny and Physiology

Evolution (1988)

George Lauder R. E. Foreman Aubrey Gorbman Julian Dodd Richard K. Olsson

10.2307/2408930

Cite

Citations (1)

Bass River Site

Kenneth G. Miller Peter J. Sugarman James V. Browning Richard K. Olsson Stephen F. Pekar

10.2973/odp.proc.ir.174ax.101.1998

Cite

Citations (42)

TAXONOMY, BIOSTRATIGRAPHY, AND PHYLOGENY OF OLIGOCENE SUBBOTINA

Bridget S. Wade Richard K. Olsson Paul N. Pearson Kirsty M. Edgar Isabella Premoli Silvá

The taxonomy, biostratigraphy, and phylogeny of Oligocene Subbotina is discussed and reviewed. We include forms that have teeth extending into the umbilicus. A total of nine species are accepted as distinct, namely Subbotina angiporoides (Hornibrook), Subbotina corpulenta (Subbotina), Subbotina eocaena (Gumbel), Subbotina gortanii (Borsetti), Subbotina linaperta (Finlay), Subbotina minima (Jenkins), Subbotina projecta Olsson, Pearson, and Wade n. sp., Subbotina tecta Pearson and Wade, and Subbotina utilisindex (Jenkins and Orr).

Source

Cite

Citations (1)

Data Report: 40Ar/39Ar and Additional Paleontologic Age Constraints, Site 862, Taitao Ridge

Randall D. Forsythe Robert T. Drake Richard K. Olsson

This paper presents additional chronological data for samples obtained during Leg 141 of the Ocean Drilling Program.The samples were obtained from Hole 862C, located on the Taitao Ridge, an anomalous bathymetric promontory that juts out from the Pacific continental margin of South America near the Chile Margin Triple Junction (latitude ~46-47°S).Four samples were selected for 40 Ar/ 39 Ar isotopic dating.Two of these samples were hornblende rhyolite, and the other two were phyric basalt.Hornblende separates from the rhyolitic samples provide ages of 1.54 ± 0.08 Ma and 2.2 ± 0.4 Ma.Low K contents in the basaltic samples and their slight alteration inhibited more precise age determinations.One sample, Sample 141-862C-6R-1, 36-44 cm (Piece 6), from the Taitao Ridge, is an indurated fragment of sandstone with carbonate and volcanic clasts.Foraminifer tests isolated from this fragment have yielded age diagnostic planktonic species indicative of a very late Paleocene age.The benthic and planktonic species suggest middle shelf depths.

10.2973/odp.proc.sr.141.045.1995

Cite

Citations (3)

TAXONOMY, BIOSTRATIGRAPHY, AND PHYLOGENY OF OLIGOCENE GLOBANOMALINIDAE (PSEUDOHASTIGERINA AND TURBOROTALIA)

Paul N. Pearson Richard K. Olsson Silvia Spezzaferri R. M. Leckie

Source

Cite

Citations (0)

Late Cretaceous Planktonic Foraminifera from New Jersey and Delaware

Micropaleontology (1964)

Richard K. Olsson

Upper Campanian and Maestrichtian Atlantic Coastal Plain sediments of New Jersey contain abundant delicately preserved planktonic foraminifera, and well-preserved late Campanian planktonic foraminifera have been recognized from Delaware Coastal Plain sediments. Twenty-eight species of planktonic foraminifera have been identified from the New Jersey and Delaware samples. One new species of Hedbergella is described and illustrated. Apparently the Maestrichtian Boreal planktonic foraminiferal faunas differed somewhat from those of the Tethys.

10.2307/1484638

Cite

Citations (73)