ABSTRACT: Cryptic ecosystems of modern and ancient reefs contain substantial amounts of biodiversity. It remains uncertain, however, when and how metazoans adapted to such space. Early Cambrian reef systems witnessed the rise and fall of the earliest known cryptic sessile metazoans. Subsequent Middle Cambrian to Early Ordovician microbial-dominated reefs were generally devoid of true frame-building metazoans, as well as cryptic sessile fauna. The Early Ordovician microbial–siliceous sponge patch reefs of the Dumugol Formation, Korea represent one of the oldest in situ spiculate sponge-bearing cryptic communities exploiting intraskeletal cryptic environments. Less than half of these small millimeter- to centimeter-scale crypts contain low-di...
Successional theory proposes that fast growing and well dispersed opportunistic species are the firs...
The Ordovician saw the Great Ordovician Biodiversification Event and a transition from microbial- to...
The archaeocyath-bearing reefs that first appeared in South China in the Atdabanian were last seen i...
The Ordovician is a period when novel reef ecosystems appeared along with new reef constructors and ...
Cambrian-Ordovician sponge-microbial mounds in the Great Basin of the western USA reveal reef struct...
The Lower Ordovician records a transition from microbial- to metazoan-dominant reefs immediately pri...
A large, resistant buildup at the top of the Upper Ordovician (Hirnantian?) Red Head Rapids Formatio...
The Cambrian Series 3 Zhangxia Formation in Shandong Province, North China, includes small-scale lit...
The oldest bryozoan reefs occur in the Lower Ordovician (late Tremadocian) Fenhsiang Formation of th...
Microbial fabrics (stromatolites, thrombolites and calcimicrobes) occur in many Paleozoic carbonate ...
ABSTRACT: During the Furongian (late Cambrian) and Early Ordovician, maze-like (maceriate) microbial...
Sponges are primitive metazoan organisms which occur since the late Proterozoic. The oldest sponge r...
The Lower Ordovician (late Tremadocian-early Floian) Fenhsiang and the overlying Hunghuayuan Formati...
Bryozoans, stromatoporoid sponges, and tabulate corals, all colonial metazoans with lamellar, encrus...
Sponges and coralomorphs were sessile epibenthic suspension feeders living in normal marine environ...
Successional theory proposes that fast growing and well dispersed opportunistic species are the firs...
The Ordovician saw the Great Ordovician Biodiversification Event and a transition from microbial- to...
The archaeocyath-bearing reefs that first appeared in South China in the Atdabanian were last seen i...
The Ordovician is a period when novel reef ecosystems appeared along with new reef constructors and ...
Cambrian-Ordovician sponge-microbial mounds in the Great Basin of the western USA reveal reef struct...
The Lower Ordovician records a transition from microbial- to metazoan-dominant reefs immediately pri...
A large, resistant buildup at the top of the Upper Ordovician (Hirnantian?) Red Head Rapids Formatio...
The Cambrian Series 3 Zhangxia Formation in Shandong Province, North China, includes small-scale lit...
The oldest bryozoan reefs occur in the Lower Ordovician (late Tremadocian) Fenhsiang Formation of th...
Microbial fabrics (stromatolites, thrombolites and calcimicrobes) occur in many Paleozoic carbonate ...
ABSTRACT: During the Furongian (late Cambrian) and Early Ordovician, maze-like (maceriate) microbial...
Sponges are primitive metazoan organisms which occur since the late Proterozoic. The oldest sponge r...
The Lower Ordovician (late Tremadocian-early Floian) Fenhsiang and the overlying Hunghuayuan Formati...
Bryozoans, stromatoporoid sponges, and tabulate corals, all colonial metazoans with lamellar, encrus...
Sponges and coralomorphs were sessile epibenthic suspension feeders living in normal marine environ...
Successional theory proposes that fast growing and well dispersed opportunistic species are the firs...
The Ordovician saw the Great Ordovician Biodiversification Event and a transition from microbial- to...
The archaeocyath-bearing reefs that first appeared in South China in the Atdabanian were last seen i...