Stromatolite‐rimmed thrombolite columns and domes constructed by microstromatolites, calcimicrobes and sponges in late Cambrian biostromes, Texas, USA. Issue 2 (11th November 2022)

• Record Type: Journal Article
• Authors: Lee, Jeong‐Hyun; Riding, Robert
• Is Part Of: Sedimentology. Volume 70:Issue 2(2023)
• Page Start: 293
• Page End: 334
• Publication Date: 2022-11-11
• Subjects: Cambrian -- dendrolite -- maceriate -- microbial carbonate -- microstromatolite -- stromatolite -- thrombolite; Sedimentology -- Periodicals; 552.5
• DOI: 10.1111/sed.13048
• Languages: English
• ISSNs: 0037-0746

Abstract

ABSTRACT: Microbial carbonates formed stromatolitic, thrombolitic, dendrolitic and maceriate (mazelike) fabrics in shallow marine Cambrian–Early Ordovician carbonates encircling Laurentia. However, poor preservation often hinders recognition of their specific components. Well‐preserved examples of normal shallow marine limestones in the ca 490 Ma upper Cambrian Point Peak Member, Wilberns Formation, central Texas, include stromatolitic cones, steep‐sided laminated rimmed columns with grainy interiors, and laminated and maceriate domes. Together these form decimetre to metre‐thick biostromes. In these examples, a single component, microstromatolite, on its own or with minor calcimicrobes, creates macroscopic stromatolitic, dendrolitic, thrombolitic and maceriate fabrics. Microstromatolites constructed upward widening stromatolitic cones that developed into columns with laminated rims surrounding slightly depressed interiors. These columns accumulated allochthonous sediment by a 'bucket effect'. Their interiors contain either clusters of dendrolitic microstromatolite or ragged columns of laminated stromatolite–sponge biolithite, and are often characterized by a 'mottled' fabric that superficially resembles thrombolite. This mottling was formed by localized dolomitization around millimetric burrows that otherwise do not appear to have significantly influenced the biolithite fabric. Calcimicrobes, including cyanobacteria ( Razumovskia ) and microproblematica ( Renalcis and Tarthinia ), impart a mesoscopic clotted appearance to maceriate fabric, and locally to column rims, both of which are dominated by microstromatolite. Similar component‐fabric relationships should be recognizable in rimmed columns and domes that were locally abundant elsewhere in Cambrian–Early Ordovician shallow carbonate seas.