TY - JOUR

T1 - A mid-cretaceous (Albian-Cenomanian) shell-rubble bryozoan fauna from the goshoura group, kyushu, Japan

AU - Dick, Matthew H.

AU - Komatsu, Toshifumi

AU - Takashima, Reishi

AU - Ostrovsky, Andrew N.

PY - 2014/5/19

Y1 - 2014/5/19

N2 - Early Cretaceous bryozoans are key to understanding the evolutionary radiation of order Cheilostomata, the dominant modern group. Prior to the current study, there were few records of any Cretaceous cheilostomes from eastern Asia, and no pre-Cenomanian records. We found bryozoan fossils to be common in brackish-water to marine deposits representing estuary-tidal-flat and shoreface-inner-shelf habitats in the late Albian-early Cenomanian Goshoura Group, Goshoura Island, Kyushu, Japan. Bryozoans from the Goshoura Group were poorly preserved; for identification, we made silicone casts of colony moulds and studied them by scanning electron microscopy (SEM). We detected six cheilostome and one cyclostome species (Berenicea sp. 1), all forming multiserial encrusting colonies.We erect the new genus Haplostoechios for two new Conopeum-like malacostegans (H. hayamiae and H. clusum), and describe another new malacostegan as Charixa goshouraensis. Additionally, we briefly describe three species detected from a single specimen each: the malacostegan Incertae sedis sp. 1 and neocheilostomes Incertae sedis sp. 2 and sp. 3. The Goshoura fauna is dominated by cheilostomes rather than cyclostomes, with malacostegans marginally outnumbering neocheilostomes. Bryozoans were a common component of the shell-rubble community, encrusting shells of one brachiopod and a broad variety of molluscan species, including 15 bivalves, two gastropods, an ammonite, a nautiloid and wood fragments containing Teredolites. Bryozoans were less diverse in estuary-tidal-flat deposits (three cheilostomes) than in shoreface-inner-shelf deposits (four cheilostomes and Berenicea sp. 1. Cheilostome average zooid length differed between the estuary-tidal-flat deposits (≤0.38 mm) and the shoreface-inner-shelf deposits (most specimens ≥0.49 mm). This study demonstrates that bryozoan assemblages worldwide were not of similar composition at the onset of cheilostome radiation, and underscores the need for further work in less studied regions.

AB - Early Cretaceous bryozoans are key to understanding the evolutionary radiation of order Cheilostomata, the dominant modern group. Prior to the current study, there were few records of any Cretaceous cheilostomes from eastern Asia, and no pre-Cenomanian records. We found bryozoan fossils to be common in brackish-water to marine deposits representing estuary-tidal-flat and shoreface-inner-shelf habitats in the late Albian-early Cenomanian Goshoura Group, Goshoura Island, Kyushu, Japan. Bryozoans from the Goshoura Group were poorly preserved; for identification, we made silicone casts of colony moulds and studied them by scanning electron microscopy (SEM). We detected six cheilostome and one cyclostome species (Berenicea sp. 1), all forming multiserial encrusting colonies.We erect the new genus Haplostoechios for two new Conopeum-like malacostegans (H. hayamiae and H. clusum), and describe another new malacostegan as Charixa goshouraensis. Additionally, we briefly describe three species detected from a single specimen each: the malacostegan Incertae sedis sp. 1 and neocheilostomes Incertae sedis sp. 2 and sp. 3. The Goshoura fauna is dominated by cheilostomes rather than cyclostomes, with malacostegans marginally outnumbering neocheilostomes. Bryozoans were a common component of the shell-rubble community, encrusting shells of one brachiopod and a broad variety of molluscan species, including 15 bivalves, two gastropods, an ammonite, a nautiloid and wood fragments containing Teredolites. Bryozoans were less diverse in estuary-tidal-flat deposits (three cheilostomes) than in shoreface-inner-shelf deposits (four cheilostomes and Berenicea sp. 1. Cheilostome average zooid length differed between the estuary-tidal-flat deposits (≤0.38 mm) and the shoreface-inner-shelf deposits (most specimens ≥0.49 mm). This study demonstrates that bryozoan assemblages worldwide were not of similar composition at the onset of cheilostome radiation, and underscores the need for further work in less studied regions.

KW - Bryozoa

KW - Cretaceous

KW - Diversity

KW - Ecology

KW - New species

KW - Taxonomy

UR - http://www.scopus.com/inward/record.url?scp=84896068064&partnerID=8YFLogxK

U2 - 10.1080/14772019.2013.765926

DO - 10.1080/14772019.2013.765926

M3 - Article

VL - 12

SP - 401

EP - 425

JO - Journal of Systematic Palaeontology

JF - Journal of Systematic Palaeontology

SN - 1477-2019

IS - 4

ER -