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siliciclastic sediments compared to<br />

dominantly carbonate sediments. The<br />

most important factors limiting the<br />

postmortem persistence of shell material<br />

are (1) exposure above the sedimentwater<br />

interface, which is enhanced in<br />

coarser-grained carbonate sediments and<br />

permits attack by bioeroders and encrusters;<br />

(2) the availability of abundant<br />

reactive iron mineral phases in the sediments,<br />

which promotes supersaturated<br />

pore waters and limits acid production;<br />

and (3) shell microstructure (rather than<br />

mineralogy), particularly organic content<br />

that is the focus of intense microbial<br />

attack. Thus, there is significant potential<br />

for enhanced carbonate shell preservation<br />

in areas receiving ferric-rich<br />

tropical weathering products, which are<br />

common in much of the tropics today<br />

and are associated with subduction systems<br />

in the geologic past. This suggests<br />

that paleodiversity estimates from carbonate<br />

tropical settings are minima and<br />

that siliciclastic settings are probably<br />

underestimated regions for carbon burial,<br />

given the large proportion of tropical<br />

shelf area characterized by such conditions<br />

and the relatively high proportional<br />

capture there of local carbonate production<br />

2010010223<br />

泰 国 东 部 中 二 叠 统 瓜 德 鲁 普 世 稀 有 的<br />

似 蜓 螺 型 腹 足 类 Magnicapitatus 属 一<br />

新 种 = A new species of the rare neritopsid<br />

gastropod Magnicapitatus from<br />

the Guadalupian (Middle Permian) of<br />

East Thailand (the Indochina Terrane).<br />

( 英 文 ). Sone M. Alcheringa, 2010, 34(1):<br />

1 - 6<br />

A new species of the rare neritopsid<br />

gastropod genus Magnicapitatus is<br />

documented from a fusulinoid-rich limestone<br />

of the Khao Taa Ngog Formation<br />

(Capitanian, Middle Permian) at Khao<br />

Makha in East Thailand near the Cambodian<br />

border (in the Indochina Terrane).<br />

This represents the first record of this<br />

Permo-Triassic genus outside South<br />

China and from the Capitanian. Magnicapitatus<br />

is one of the typical molluscan<br />

Lazarus taxa that apparently disappeared<br />

at the end of the Permian but reappeared<br />

after the Early Triassic.<br />

2010010224<br />

腹 足 类 证 据 不 支 持 早 三 叠 世 小 型 化 效<br />

应 假 说 = Gastropod evidence against<br />

the Early Triassic Lilliput effect. ( 英 文 ).<br />

Brayard A; Nützel A; Stephen D; Bylund<br />

K G; Jenks J; Bucher H. Geology,<br />

2010, 38(2): 147-150<br />

Size reduction in the aftermath of the<br />

Permian-Triassic mass extinction event<br />

has repeatedly been described for various<br />

marine organisms, including gastropods<br />

(the Lilliput effect). A Smithian<br />

gastropod assemblage from Utah, USA,<br />

reveals numerous large-sized specimens<br />

of different genera as high as 70 mm, the<br />

largest ever reported from the Early Triassic.<br />

Other gastropods reported from<br />

Serbia and Italy are also as large as 35<br />

mm. Size frequency distributions of the<br />

studied assemblages indicate that they<br />

were not unusually small when compared<br />

with later Mesozoic and modern<br />

faunas. The occurrence of large-sized<br />

gastropods less than 2 Ma after the Permian-Triassic<br />

mass extinction refutes the<br />

Lilliput hypothesis in this clade, at least<br />

for the last 75% of the Early Triassic<br />

2010010225<br />

伏 尔 加 河 中 下 游 地 区 由 P.A. Gerasimov<br />

采 集 的 早 白 垩 世 腹 足 类 = Early<br />

Cretaceous gastropods of the Middle-<br />

Lower Volga river region from P.A.<br />

Gerasimov’s collection. ( 英 文 ). Golovinova<br />

M A; Guzhov A V. Paleontological<br />

Journal, 2009, 43(5): 506-513 2 图<br />

版 .<br />

Based on the studying of gastropods<br />

collected by P.A. Gerasimov from the<br />

Cretaceous beds of the Volga region,<br />

four new species are established: Avellana<br />

hauteriviensis sp. nov. from the<br />

Upper Hauterivian of the Ulyanovsk re-<br />

72

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