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1 e biomineralization of shell valves in crown brachiopods.
2 ived from the isotopic composition of fossil brachiopods.
3 so reflected in other benthic faunas such as brachiopods.
4 latitudinal trend in shell thickness within brachiopods.
5 wo entoprocts, an ectoproct, an inarticulate brachiopod, a phoronid, two annelids, and a platyhelmint
6 temperatures that were obtained from fossil brachiopod and mollusc shells using the 'carbonate clump
7 exhibits an unusual combination of phoronid, brachiopod and tommotiid (Cambrian problematica) charact
8 ong diversification and sampling dynamics of brachiopods and bivalves and five paleoenvironmental pro
12 e of the earliest Paleozoic apatitic-shelled brachiopods and may also be indicators of siliceous biom
14 r; only pb (in T. transversa), Hox3 (in both brachiopods), and Dfd (in both brachiopods) show stagger
15 ter genes are most similar to known annelid, brachiopod, and nemertean Hox gene homeodomain sequences
19 occurred nearly in parallel across all major brachiopod clades (classes and orders) and is consistent
20 l size increases among major, more inclusive brachiopod clades from a single habitat type is best exp
21 allowing sessile suspension feeders such as brachiopods, corals, and bryozoans to recover rapidly.
22 competed brachiopods evolutionarily, because brachiopod diversity declined through time while bivalve
24 ing debate over whether bivalves outcompeted brachiopods evolutionarily, because brachiopod diversity
25 rocta are not sister taxa, (3) phoronids and brachiopods form a monophyletic clade, and (4) neither E
28 nction dynamics of fossil marine bivalve and brachiopod genera from the Ordovician through to the Rec
30 e-specific transcriptomic analyses show that brachiopod Hox genes are neither strictly temporally nor
31 n of lophotrochozoans, suggesting rooting of brachiopods into the sessile lophotrochozoans and the or
32 e a maximum-likelihood approach to show that brachiopod (lamp shell) abundance distributions from fou
33 brates: a crustacean Paraceradocus miersi, a brachiopod Liothyrella uva, two bivalve molluscs, Latern
34 nd echiurans) with nemerteans, phoronids and brachiopods, molluscs as sister to that assemblage, and
35 ay components in chaetae and shell fields in brachiopods, mollusks, and annelids provide molecular ev
37 bivalve extinction rates causally increased brachiopod origination rates, suggesting that bivalves h
38 indicate an affinity with the lophophorates (brachiopods, phoronids and tommotiids), substantially in
41 arkably, expression of the Hox genes in both brachiopod species demonstrates cooption of Hox genes in
42 cluster, and expression of Hox genes in two brachiopod species, Terebratalia transversa and Novocran
43 n assigned variously to stem-group annelids, brachiopods, stem-group molluscs or stem-group aculifera
44 Therefore, the ecological transition from brachiopods to bivalves was more protracted and complex
45 tterns suggests that the shift from abundant brachiopods to dominant molluscs was abrupt and largely
46 rals, fossil-plant matter, and shallow-water brachiopods, we estimated atmospheric partial pressure o
47 persistent rarity of drilling suggests that brachiopods were the secondary casualties of mistaken or
48 redation indicates that attacks on Paleozoic brachiopods were very rare, especially compared to those
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