Schugurocaris Community, Upper Silurian, Sarthe, Laval Synclinorium (Silurian to of France)

Also known as Warneticaris Community, Upper Silurian, Sarthe, Laval Synclinorium

Where: France (47.5° N, 0.5° W: paleocoordinates 57.3° S, 44.0° E)

• coordinate based on political unit

• local area-level geographic resolution

When: Ludlow to Ludlow (427.4 - 419.2 Ma)

• "Upper Ludlow or more probably Pridoli"

Environment/lithology: marine; black shale

• General statement of Central Armorican trough during Llandovery through Lochkovian: "depositional patterns typical of a platform environment...Silurian is mainly an alternating succession of unfossiliferous sandstones and locally fossiliferous black shales...The arenaceous deposits are probably related to the eustatic regression and corresponding high sedimentation rate during the Pridolian and Lochkovian...Outside the A. Massif the Pridoli-Lochkovian succesion in Artois (boreholes) is characterized by shallow marine shales and limestones overlain by areanceous deposits that correspond to the Early Devonian transgression."

•For this Community: "The preservation of the phyllocarids...and crinoids (with stems and arms still articulated to the calyx) are suggestive of rapid burial. Rolfe and Beckett (1984) assgined the Laval Basin, Silurian phyllocarid localities to the 'restricted marine A' environment, which they interprted as lagoonal or estuarine with ephemeral brackish or hypersaline waters. The fauna is cosmopolitan and low diversity, but the presence of true, marine faunal elements...precludes such an environment...[lithology and preservation] suggest a quiet environment...well below wave base...the abundance of Myodocopida ('Bolbozoe') implies an offshore, epicontinental shel setting-probably BA 4 or 5..In the eastern Armorican Massif these nodular shales represent the deepest facies."

• General statement: "In Brittany there are two kinds of black shale and limestone deposits during the Llandovery to lowermost Devonian interval: (1) black shales (commonly described as sapropelites) are widespread in space and time and (2) black, micritic limestones or argillaceous limestones are restricted to two localities in the eastern part of the Armorican Massif. The black shales are very rich in organic matter and locally contain detrital mica, pyrite, and nodules..."

•For this community: "The fauna occurs exclusively in nodules interbedded in black shales...sediment finely laminated and shows no evidence of bioturbation..."

Primary reference: P. R. Racheboeuf. 1999. Lower Silurian to Lower Devonian communities from the Armorican Massif (western France) and Artois (northern France). In A. J. Boucot, J. D. Lawson (eds.), Paleocommunities--a case study from the Silurian and Lower Devonian 260-270 [M. Foote/M. Foote/P. Wagner]more details

Purpose of describing collection: paleoecologic analysis

PaleoDB collection 26120: authorized by Michael Foote, entered by Michael Foote on 04.10.2002

Creative Commons license: CC BY (attribution)

Taxonomic list

Malacostraca
 Archaeostraca - Ceratiocarididae
Ceratiocaris bohemica Barrande 1853
 Archaeostraca -
Schugurocaris sp.
"[=Warneticaris cenomauense]"
Ostracoda
 Cypridinida - Bolbozoidae
"Bolbozoe" sp. Barrande 1872 ostracod
 Myodocopida -
Myodocopida indet. Sars 1866 ostracod
Cephalopoda
 Orthoceratoidea -
Crinoidea
 Monobathrida - Melocrinitidae
Melocrinitidae indet. Wachsmuth and Springer Sea lily