Pregled bibliografske jedinice broj: 309695
Decapod Crustaceans (Brachyura) from the Eocene Tepetate Formation, Baja California Sur, Mexico
Decapod Crustaceans (Brachyura) from the Eocene Tepetate Formation, Baja California Sur, Mexico // Annals of the Carnegie Museum, 76 (2007), 1; 1-14 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 309695 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Decapod Crustaceans (Brachyura) from the Eocene Tepetate Formation, Baja California Sur, Mexico
Autori
Schweitzer, Carrie ; Feldmann, Rodney ; Gonzalez-Barba, Gerardo ; Ćosović, Vlasta
Izvornik
Annals of the Carnegie Museum (0097-4463) 76
(2007), 1;
1-14
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Decapoda; Brachyura; Mexico; Eocene; Bateque Formation; Tepetate Formation; Bartonian
Sažetak
A large collection of brachyuran specimens from the middle Eocene Tepetate Formation, Baja California Sur, Mexico, has yielded sufficiently well preserved specimens to provide revised descriptions and diagnoses for genera and species previously known from the area. Revised, more complete descriptions are given for Eriosachila bajaensis Schweitzer et al., 2002, and Lobonotus mexicanus Rathbun, 1930. A goneplacid specimen is questionably referred to Carcinoplax, which has a well established Pacific record during the Miocene. All of the specimens of Amydrocarcinus dantei Schweitzer et al., 2002, thus far collected for which gender can be determined are males, suggesting that there may have been environmental or behavioral segregation of males and females of this species. Analysis of benthic and planktonic foraminiferans suggests that the Tepetate Formation was deposited in subtropical conditions, probably within the photic zone but below the seasonal thermocline, perhaps below 100-120 m. The age of the Tepetate formation, according to larger foraminiferans, is middle Eocene, and according to planktonic foraminiferans is further constrained as upper middle Eocene )Bartonian). The age corresponds to the P14 foraminiferal zone based upon the Berggren et al. (1995) scheme and the E13 zone based upon the work of berggren and Pearson (2005).
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119-1191152-1167 - Terroir naslaga taloženih između 108 i 35 milijuna godina u SZ Hrvatskoj (Ćosović, Vlasta, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Vlasta Ćosović
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus