1994
DOI: 10.2307/3515056
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Siliceous Sponge-Microbe Biotic Associations and Their Recurrence through the Phanerozoic as Reef Mound Constructors

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Cited by 107 publications
(51 citation statements)
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“…Reef mounds constructed by siliceous sponges and cyanobacterial mats, with the latter represented in part by stromatolites still found today, flourished in (sub)tropical marine waters as far back as the early Cambrian (43). The fact that sponges and microbes closely coexisted hundreds of millions of years ago is thus clear, but the nature of that interaction (e.g., whether microbes lived within sponge tissues) remains less certain.…”
Section: Sponge-associated Microorganisms: Ancient Partners or Recentmentioning
confidence: 99%
See 1 more Smart Citation
“…Reef mounds constructed by siliceous sponges and cyanobacterial mats, with the latter represented in part by stromatolites still found today, flourished in (sub)tropical marine waters as far back as the early Cambrian (43). The fact that sponges and microbes closely coexisted hundreds of millions of years ago is thus clear, but the nature of that interaction (e.g., whether microbes lived within sponge tissues) remains less certain.…”
Section: Sponge-associated Microorganisms: Ancient Partners or Recentmentioning
confidence: 99%
“…The final type of evidence for ancient, close associations between sponges and microorganisms comes from the fossil record (43,261,377). Reef mounds constructed by siliceous sponges and cyanobacterial mats, with the latter represented in part by stromatolites still found today, flourished in (sub)tropical marine waters as far back as the early Cambrian (43).…”
Section: Sponge-associated Microorganisms: Ancient Partners or Recentmentioning
confidence: 99%
“…It is important to note that taxa with carbonate skeletons are not the only organisms that diversified during Ordovician time. For example, siliceous sponges, often associated with microbial mounds, diversified in the Early Ordovician (Brunton and Dixon, 1994;Carrera and Rigby, 2004), and trace fossils, indicators of soft-bodied diversity, show an increase in diversity during the Ordovician radiation (Mángano and Droser, 2004). The overall depth and extent of bioturbation also increased, albeit not until the Late Ordovician (e.g., Droser and Bottjer, 1989).…”
Section: Discussionmentioning
confidence: 99%
“…Fossil Record and Systematics of Glass Sponges.-Hexactinellids were important components of deep-and at times also shallowerwater benthic ecosystems throughout the Phanerozoic, often associated with reef communities (e.g., Finks 1960;Mehl 1992;Brunton and Dixon 1994;Leinfelder et al 1994;Krautter et al 2001;Carrera and Botting 2008). Their rich fossil record (see Krautter 2002;Pisera 2006) dates back to the late Neoproterozoic (Steiner et al 1993;Gehling and Rigby 1996;Brasier et al 1997).…”
Section: Introductionmentioning
confidence: 99%