Accretionary Mechanisms and Temporal Sequence of Formation of the Boda Limestone Mud-Mounds (Upper Ordovician), Siljan District, Sweden

2016 ◽  
Vol 86 (4) ◽  
pp. 363-379 ◽  
Author(s):  
Björn Kröger ◽  
Jan Ove R. Ebbestad ◽  
Oliver Lehnert
Keyword(s):  
Temporal Sequence ◽  
Upper Ordovician ◽  
Mud Mounds

BRYOZOAN MUD-MOUNDS FROM THE UPPER ORDOVICIAN JIFARAH (DJEFFARA) FORMATION OF TRIPOLITANIA, NORTH-WEST LIBYA

Palaeontology ◽  
2007 ◽  
Vol 50 (2) ◽  
pp. 479-494 ◽  
Author(s):  
CAROLINE J. BUTTLER ◽  
LESLEY CHERNS ◽  
DOMINIQUE MASSA
Keyword(s):  
Upper Ordovician ◽  
Mud Mounds ◽  
North West

Carbonate mud mounds, conglomerates, and sea-level history in the Katian (Upper Ordovician) of central Sweden

Facies ◽  
2009 ◽  
Vol 56 (1) ◽  
pp. 157-172 ◽  
Author(s):  
Mikael Calner ◽  
Oliver Lehnert ◽  
Michael Joachimski
Keyword(s):  
Sea Level ◽  
Upper Ordovician ◽  
Mud Mounds ◽  
And Sea Level

Vagrant benthos (Annelida; Polychaeta) associated with Upper Ordovician carbonate mud-mounds of subsurface Gotland, Sweden

2009 ◽  
Vol 146 (3) ◽  
pp. 451-462 ◽  
Author(s):  
MATS E. ERIKSSON ◽  
OLLE HINTS
Keyword(s):  
Principal Component Analysis ◽  
Principal Component ◽  
Component Analysis ◽  
Taxonomic Composition ◽  
Upper Ordovician ◽  
Mud Mounds ◽  
Faunal Element ◽  
Fossil Assemblages ◽  
Abundance And Diversity

AbstractMicropalaeontological investigations of Upper Ordovician carbonate mud-mounds and enclosing strata of subsurface Gotland, Sweden, demonstrate that jaw-bearing polychaetes formed the most diverse faunal element associated with these build-ups. Although not present within the mound cores (intra-mound facies), scolecodonts, or polychaete jaws, occur abundantly immediately below and particularly above the mounds; the supra-mound facies also has the most diverse fossil assemblages. By contrast to the scolecodont distribution, the most diverse conodont faunas were recorded in the intra-mound facies. This reinforces the fact that scolecodont and conodont abundance and diversity numbers are commonly inverse to one another, suggesting that these metazoans occupied different niches and responded differently to taphonomical processes. The polychaete assemblage has no less than 27 species belonging to 12 genera, of which Oenonites, Mochtyella and Pistoprion are the most abundant. The assemblage has a characteristic Baltic signature and is similar in taxonomic composition to coeval ones from other areas of the Baltoscandian palaeobasin, such as that of present-day Estonia. A principal component analysis clusters the Gotland assemblage most closely to those recorded from shallow to transitional shelf environments of Estonia, indicating that the mud-mounds were formed in such environments.

Precursors to heterophobia: An examination of temporal sequence among a sample of gay men.

2019 ◽  
Vol 20 (4) ◽  
pp. 647-653
Author(s):  
Mike C. Parent ◽  
Aaron B. Rochlen ◽  
Lexie Wille
Keyword(s):  
Gay Men ◽  
Temporal Sequence
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