La D├ęsirade Island, Lesser Antilles, Massive coral breccia (Pleistocene of Guadeloupe)

Where: Guadeloupe (16.3° N, 61.0° W: paleocoordinates 16.3° N, 61.0° W)

• coordinate estimated from map

• outcrop-level geographic resolution

When: Late/Upper Pleistocene (0.1 - 0.0 Ma)

Environment/lithology: reef, buildup or bioherm; breccia

• bedded (up to 3 m thick), commonly inverse-graded, clayey, sand-supported, red breccia. The sand-sized matrix contains carbonate bioclasts dominated by mmsized, geniculate red algae fragments, substratum-originated

•minerals, and volcanic clasts, often coated by mm-to cm-thick encrusting

•red algae. Breccia clasts are a few tens of cm up to 2m-sized reworked corals fragments, commonly entire or fragmented columnar colonies of Orbicella spp., often large fragments of Acropora palmata branches, and rarely broken thin branches of Acropora cervicornis. Rare reworked, overturned, and massive Diploria

•are observed at the base of the Acropora-dominated breccia. Mixing in the same breccia bed of Orbicella fragments with Acropora or Diploria fragments is rare.

• massive coral breccia

Size class: macrofossils

Primary reference: E. Vernhet, G. Conesa, and P. O. Bruna. 2017. Reworking processes and deposits in coral reefs during (very) high-energy events: Example from a Pleistocene coral formation (125 ka), La D├ęsirade Island, Lesser Antilles. Palaeogeography, Palaeoclimatology, Palaeoecology [W. Kiessling/M. Krause]more details

Purpose of describing collection: paleoecologic analysis

PaleoDB collection 189821: authorized by Wolfgang Kiessling, entered by Mihaela Krause on 17.11.2017

Creative Commons license: CC BY (attribution)

Taxonomic list

Anthozoa
 Scleractinia - Acroporidae
Acropora palmata Lamarck 1816 stony coral
Acropora cervicornis Lamarck 1816 stony coral
 Scleractinia - Merulinidae
Orbicella sp. Dana 1846 stony coral
 Scleractinia - Faviidae
Diploria sp. Milne-Edwards and Haime 1848 stony coral