About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The AAPG/Datapages Combined Publications Database
Journal of Sedimentary Research (SEPM)
Abstract
Formation of Peloids in Plant Rootlets, Grand Cayman, British West Indies
Brian Jones, Cheryl A. Squair
ABSTRACT
Spherical to elliptical peloids, averaging 80 µm in length, occur inside plant rootlets that penetrate limestones of the Pleistocene Ironshore Formation on Grand Cayman. The peloids, which are associated with desiccated fragments of mites, are formed of minute calcite platelets and fragments of algal and/or fungal filaments bound by organic-rich material. The calcite platelets are morphologically similar to platelets that occur in the epidermal cells of the surrounding rootlets. The peloids probably originated as fecal pellets produced by mites which mined into the softer cores of the roots. In so doing, they recombined the calcite platelets, algal/fungal filaments, and organic material into coprogeneous material. Subsequent diagenetic modification produced peloids formed of mic ite that are morphologically identical to peloids found in many caliche units.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
| Watermarked PDF Document: $14 | |
| Open PDF Document: $24 |