Assessing the veracity of Precambrian ‘sponge’ fossils using in situ nanoscale analytical techniques
Authors:
Muscente et al
Abstract:
Paleontological inferences, molecular clocks, and biomarker fossils indicate sponges evolved in the Cryogenian, but Precambrian sponge fossils are rare, poorly substantiated, and controversial. Spicule-like microstructures (SLMs) hosted in phosphatized fossils from the Ediacaran Doushantuo Formation (∼635–551 Ma) at Weng’an of South China have been interpreted as cylindrical siliceous monaxons, and their hosting fossils as the oldest demosponges in the fossil record. In order to assess their veracity as the oldest spiculate demosponges, we utilize a suite of in situ nanoscale analytical techniques—including scanning electron microscopy, synchrotron X-ray fluorescence mapping, X-ray absorption near edge structure (XANES) spectroscopy, focused ion beam electron microscopy, and transmission electron microscopy—to evaluate the ultrastructures and elemental, chemical, and mineralogical compositions of the SLMs. Our data decisively shows that the SLMs are carbonaceous in composition and rectangular in transverse sections, and therefore, are not cylindrical siliceous spicules. Instead, the SLMs may be microbial strands, axial filaments of early hexactinellids, or acicular crystals molded by organic matter. Regardless, our new data invalidate the oldest and only Precambrian demosponges with mineralized spicules. These results indicate that interpretations of Precambrian sponge fossils should be scrutinized with compositional, mineralogical, and ultrastructural data collected using in situ analytical techniques. In addition, our conclusions affirm that no unequivocal biomineralizing sponges occur below the Ediacaran–Cambrian boundary. If hexactinellids and demosponges did diverge in the Cryogenian as suggested by molecular clocks and biomarkers, they either evolved biomineralization long after their divergence or their biomineralized spicules were never preserved until after the Ediacaran–Cambrian boundary. In either case, the dearth of biomineralizing sponge fossils in the Precambrian and their abundance in the early Cambrian must reflect a geobiologically significant aspect of the Precambrian–Phanerozoic transition.
Showing posts with label sponges. Show all posts
Showing posts with label sponges. Show all posts
Friday, April 24, 2015
Claim: Cryogenian NeoProterozoic Sponge Fossils are not Sponges, but Microbial Traces
Labels:
cryogenian,
demosponges,
fossils,
Neoproterozoic,
paleontology,
precambrian,
Proterozoic,
sponges
Friday, April 10, 2015
Demosponges Diverged From Other Animals During the Cryogenian Sturtian Glaciations (Snowball Earth?)
Early divergence dates of demosponges based on mitogenomics and evaluated fossil calibrations
Authors:
Ma et al
Abstract:
Demosponges are among the most primitive biomineralized metazoans to appear first in the fossil record with hard skeletons; their confirmed earliest fossils are from the lower Cambrian rocks about 520 Ma, with putative demosponge biomarkers reported from 713∼635 Ma sediments. In this study, we use mitogenomic data to approach the early divergence timescale of demosponges using relaxed molecular clock techniques and likelihood-evaluated fossil calibration strategies. We found that among various molecular dating models, the correlated rate model yielded time estimates of demosponges in this analysis which is most congruent with the fossil appearance dates of demosponges. Our dating analyses show that crown groups of Demospongiae appeared at about 704 (674∼741) Ma, and the silicification in demosponges (divergence of spicular sponges) began about 633 (616∼648) Ma indicating a gap of over 100 million years between the origin of silicification and their first unequivocal appearance of siliceous spicules in the fossil record (520∼525 Ma); demosponges with tetraxon-type spicules (Tetractinellida) are dated here at about 514 (498∼530) Ma, an estimate comparable with the earliest tetraxial megasclere fossil records (510∼520 Ma, Ordian Age, middle Cambrian).
Friday, March 20, 2015
Eocyathispongia qiania: an Ediacaran NeoProterozoic Sponge With Fossil Cells
Sponge grade body fossil with cellular resolution dating 60 Myr before the Cambrian
Authors:
Yin et al
Abstract:
An extraordinarily well preserved, 600-million-year (Myr)-old, three-dimensionally phosphatized fossil displaying multiple independent characters of modern adult sponges has been analyzed by SEM and synchrotron X-ray tomography. The fossilized animal (Eocyathispongia qiania gen. et sp. nov.) is slightly more than 1.2 mm wide and 1.1 mm tall, is composed of hundreds of thousands of cells, and has a gross structure consisting of three adjacent hollow tubes sharing a common base. The main tube is crowned with a large open funnel, and the others end in osculum-like openings to the exterior. The external surface is densely covered with flat tile-like cells closely resembling sponge pinacocytes, and this layer is punctuated with smaller pores. A dense patch of external structures that display the form of a lawn of sponge papillae has also survived. Within the main funnel, an area where features of the inner surface are preserved displays a regular pattern of uniform pits. Many of them are surrounded individually by distinct collars, mounted in a supporting reticulum. The possibility cannot be excluded that these pits are the remains of a field of choanocytes. The character set evinced by this specimen, ranging from general anatomy to cell type, uniquely indicates that this specimen is a fossil of probable poriferan affinity. So far, we have only this single specimen, and although its organized and complex cellular structure precludes any reasonable interpretation that its origin is abiogenic, confirmation that it is indeed a fossilized sponge will clearly require discovery of additional specimens.
Labels:
Ediacaran,
fossils,
metazoans,
Neoproterozoic,
paleontology,
precambrian,
Proterozoic,
sponges
Friday, January 23, 2015
More Information About the Hettangian Jurassic/Post Triassic-Jurassic Mass Extinction Sponge Bob World
Andean sponges reveal long-term benthic ecosystem shifts following the end-Triassic mass extinction
Authors:
Ritterbush et al
Abstract:
Thick cherts and cherty dolomites in the basal Jurassic Aramachay Formation of Peru preserve a thriving continental shelf community dominated by siliceous sponges that followed the end-Triassic collapse of metazoan-rich carbonate accumulation. Similar Hettangian and Sineumurian deposits from Nevada, U.S.A., Austria, and Morocco suggest that an Early Jurassic siliceous sponge takeover was a widespread phenomenon that persisted for ~ 2 m.y. until metazoan-driven carbonate sedimentation recovered. The post-extinction dominance of siliceous sponges likely resulted from the confluence of metazoan carbonate reef collapse (removal of incumbents) and geochemical conditions that fostered the success of the siliceous sponge-dominated ecosystem. Simple mass balance calculations suggest the siliceous sponge takeover was likely permitted by an increased silica flux as a consequence of weathering Central Atlantic Magmatic Province (CAMP) basalts. The CAMP basalts alone could supply all the silica needed to sustain the sponge takeover, although contributions were also likely from increased hot-climate weathering of other silicates and possible reductions in dissolved silica demand by radiolarians. Detailed sedimentological, fossil, and microfacies analyses were conducted at six field sites across a shallow shelf system recorded in the central Peruvian Andes (Yauli Dome), focusing on the metazoan contribution to sedimentation. Sedimentary structures at all six sites demonstrated on-shelf deposition, similar to the underlying upper Triassic Chambará Formation (in contrast to the black shale-rich facies of the Aramachay Formation in other areas of Peru). Examination of up to 147 m of cherty dolomite from the Aramachay Formation revealed a siliceous sponge-dominated ecosystem, including sponge body fossils, compressed in situ sponge materials, and abundant transported spiculite sediments. Siliceous sponges, mostly demosponges and rare hexactinellids, account for the chert lithology and apparently dominated the local ecology for approximately two million years. The role of metazoan biocalcifiers in sediment production and ecological structure was profoundly reduced compared to the under- and overlying formations, representing a clear ecological state shift from pre-extinction carbonate to post-extinction siliceous dominated ecosystems before the carbonate system recovered ~ 2 m.y. after the extinction.
Labels:
andes,
benthic zone,
biotic recovery,
Hettangian,
Jurassic,
mesozoic,
paleoecology,
paleooceans,
Postmass extinction,
south america,
sponges,
TJ Event,
triassic-jurassic mass extinction
Thursday, January 22, 2015
Hettangian Jurassic Oceans Became Sponge Bob World After Triassic-Jurassic Extinction?
NEW EVIDENCE ON THE ROLE OF SILICEOUS SPONGES IN ECOLOGY AND SEDIMENTARY FACIES DEVELOPMENT IN EASTERN PANTHALASSA FOLLOWING THE TRIASSIC–JURASSIC MASS EXTINCTION
Authors:
Ritterbush et al
Abstract:
Paleoecological consequences of the global Triassic–Jurassic mass extinction (201.3 Ma) are poorly understood. Fossiliferous marine boundary records are rare, commonly condensed, and typically reveal facies changes previously attributed to eustacy. Sedimentology and biofacies analyses from stratigraphically expanded successions of the lowest Jurassic strata, New York Canyon, Nevada, were investigated with high-resolution paleoenvironmental observations, fossil surveys, and microfacies analysis. Following the collapse of the uppermost Triassic carbonate ramp, the lowest Jurassic Ferguson Hill Member of the Sunrise Formation records a midshelf habitat dominated by previously unrecognized siliceous sponges for approximately two million years. In addition, the earliest Jurassic strata from the Pucara Group, central Peruvian Andes, were examined and record a more greatly expanded stratigraphic succession of facies across the inner to middle shelf. Like Nevada, the lowest Jurassic Aramachay Formation is replete with intense concentrations of siliceous sponges. The revelation of widespread, ecologically dominant siliceous sponges has been overlooked despite detailed biofacies studies in both depositional systems. Sponges expanded across shallow environments with sparse benthic biocalcifier populations, and were likely aided by increased ocean silica concentrations from the weathering of the Central Atlantic Magmatic Province. Facies changes previously attributed to sea-level change are thus interpreted to result from the collapse of the carbonate factory concomitant with the mass extinction, with transition to an alternate state dominated by siliceous sponges before a return to carbonate platform development in the Sinemurian. Our study highlights the need to separate biofacies from paleoenvironmental analysis during mass extinction times when nonactualistic assemblages may dominate and deviate from expected environments (e.g., siliceous sponges as indicators of deep paleoenvironments).
Wednesday, December 17, 2014
New Articulated Protospongiid Sponges From the Camrbian Chengjiang Biota
New articulated protospongiid sponges from the early Cambrian Chengjiang biota
Authors:
Chen et al
Abstract:
Sponges are among the earliest diverging crown-group animals and widely regarded as the earliest biomineralizing animals. Indeed, unambiguous hexactine sponge spicules first occur in the lowermost Cambrian strata of the Fortunian Stage. Articulated sponge skeletons interpreted as hexactinellids and demosponges have been reported from Cambrian Stage 2–3 strata at multiple localities. Articulated sponge skeletons in the Chengjiang biota (Cambrian Stage 3), however, are dominated by forms interpreted as demosponges, despite the exceptional preservation in this biota. Here, we report new articulated sponge skeletons from the Chengjiang biota, including Paradiagoniella magna n. gen. n. sp. and P. xiaolantianensis n. gen. n. sp. The skeleton of both species consists of ranked stauractines and rare oxeas (straight or curved diactines), as well as hexactines in the former species. Their stauractines form irregular, nested, local sub-quadrules oriented obliquely to the sponge body axis. Sub-quadrules of different ranks are not in parallel arrangement. The two species are tentatively placed in the family Protospongiidae, which as currently defined may be a paraphyletic group including members of the total-group hexactinellids and perhaps stem-group siliceans. The phylogenetic placement of P. magna and P. xiaolantianensis is uncertain but, like many other protospongiids, they could be members of the total-group hexactinellids or stem-group siliceans. The diactines in the two species could be secondarily reduced hexactine-based spicules; alternatively, these two species may represent an evolutionary grade of stem-group siliceans with both diactines and hexactine-based spicules, the latter of which was lost in demosponges. A comprehensive cladistics analysis is needed to resolve the exact phylogenetic placement of the two species described here.
Labels:
cambrian,
chengjiang fauna,
china,
fossils,
paleontology,
paleozoic,
sponges
Tuesday, November 18, 2014
A Sponge Fossil From Cambrian Paleozoic Greenland
A crown-group demosponge from the early Cambrian Sirius Passet Biota, North Greenland
Authors:
Botting et al
Abstract:
Calibration of the divergence times of sponge lineages and understanding of their phylogenetic history are hampered by the difficulty in recognizing crown versus stem groups in the fossil record. A new specimen from the lower Cambrian (Series 2, Stage 3; approximately 515 Ma) Sirius Passet Biota of North Greenland has yielded a diagnostic spicule assemblage of the extant demosponge lineages Haploscleromorpha and/or Heteroscleromorpha. The specimen has disarticulated approximately in situ, but represents an individual sponge that possessed monaxon spicules combined with a range of slightly smaller sigma, toxa and unique spiral morphologies. The combination of spicule forms, together with their relatively large size, suggests that the sponge represents the stem lineage of Haploscleromorpha + Heteroscleromorpha. This is the first crown-group demosponge described from the early Cambrian and provides the most reliable calibration point currently available for phylogenetic studies.
Labels:
cambrian,
fossils,
paleontology,
paleozoic,
sponges
Tuesday, November 04, 2014
Evidence of Sponges in Cryogenian NeoProterozoic Reefs?
Enigmatic chambered structures in Cryogenian reefs: The oldest sponge-grade organisms?
Authors:
Wallace et al
Abstract:
Previously undescribed chambered structures are common and widespread in the Cryogenian (post-Sturtian glacial) carbonates of the Oodnaminta Reef Complex (Adelaide Geosyncline, South Australia), the Rasthof-Berg Aukas Formation (Namibia) and the Gauss Formation (Namibia). These carbonate structures have millimetre to centimetre-scale chambers separated by well-defined and generally thin micritic walls. Chamber walls now consist of dolomite, but were probably originally aragonitic. The chambers may have a lobate, polygonal or dendritic morphology and are often further divided into smaller chambers. Chambered structures occur as reefal growth frameworks; as cavity-fillings in neptunean dykes and growth cavities; and as intercolumnar material within stromatolite frameworks. In the Oodnaminta Reef Complex, these structures are only present in the sub-photic deep water framework.
These structures probably represent the calcified remains of an organism or community of organisms that was globally distributed and widespread for a significant time period following the Sturtian glaciation. No precisely analogous structures have been previously described from modern or ancient settings, but the complexity and degree of organization suggests a significant evolutionary advance over older Proterozoic fossils. The closest morphological analogues for the structures are: (a) some types of reef-dwelling sponges; and (b) some complex microbialites from Archaean and Paleoproterozoic carbonates. The structures lack spicules and ostia found in sponges, ruling out a true Poriferan origin. However, it is plausible that they are proto-sponges, sponge-grade organisms, or complex microbial precursors to sponge-grade organisms. Whatever their affinity, we suggest these structures record a significant evolutionary event on the path towards organic complexity.
Labels:
animals,
cryogenian,
fossils,
metazoans,
Neoproterozoic,
paleontology,
precambrian,
Proterozoic,
reefs,
sponges
Thursday, September 18, 2014
Evidence of Ediacaran NeoProterozoic Sponges From China?
Potential Ediacaran Sponge Gemmules from the Yangtze Gorges area in South China
Authors:
Du et al
Abstract:
Sponges are widely viewed as the most primitive metazoans. Sponge gemmule-like structures have been recovered from the lower part of the Doushantuo Formation in the Yangtze Gorges area (South China), that was deposited between 635 to 580 Ma. Gemmoscleres-like structures are embedded in the outer coat of the sponge structures. Electron probe microanalyses EPMA) of the gemmoscleres-indicate that they have siliceous composition. The naked subspheroidal sponge structures are composed of three layers, consistent with the preservation of a tri-layered theca embedded with the gemmosclere-like structures. The potential fossils of the Ediacaran sponge gemmules in the Doushantuo Formation may provide one of the earliest records of sponges.
Labels:
animals,
china,
Ediacaran,
fossils,
metazoans,
Neoproterozoic,
paleontology,
precambrian,
Proterozoic,
south china,
sponges,
yangtze
Tuesday, April 15, 2014
Attack of the Killer Sponges
Labels:
carnivorism,
invertebrates,
oceans,
sponges
Tuesday, March 11, 2014
A Deep Shelf Calcisponges From Late Permian China
Deep shelf biostrome of late Permian in south China and its implications for the adaptability of calcisponges to water depth
Authors:
Meng et al
Abstract:
The Yangtze platform of South China was an area of extensive carbonate accumulation during the Late Permian, with abundant benthic fossils and reef buildups. Its northern margin has long been considered to be bordered by deep shelf sediments rich in radiolarians and ammonoids. However, recent investigations found a sponge biostrome in deeper shelf settings in the uppermost Permian. The biostrome is about 0.45 m thick with an organic framework formed by autochthonous calcisponges. In contrast to more diverse shallow marine reef communities at this time, the biostrome was almost entirely constructed by the sponge genus Peronidella as the only frame-building organism. This low biodiversity reflects a relatively deep-water environment. Peronidella individuals in the biostrome are apparently larger than the same genus in shallow platform settings, including the diameters of both the sponge bodies and the central tubular spongocoel, as well as the thicknesses of the body walls. This increased size may be related to the low biodiversity and therefore to reduced competition, with sponge individuals having increased space in which to develop. Biostrome development was terminated by volcanic clay deposition.
Labels:
china,
fossils,
late permian,
paleontology,
Permian,
sponges
Thursday, March 06, 2014
Where What Sponges Lived During the Cambrian
Composition and tiering of the Cambrian sponge communities
Authors:
Wu et al
Abstract:
Sponges are dominant sessile suspension feeders in the Cambrian metazoan community; thus, sponge tiering and composition in the Cambrian communities will provide important information for elucidating the evolutionary history of the epifaunal community. Based on more than two thousand articulated sponge specimens from the early Cambrian Chengjiang fauna, the present study demonstrates that the Chengjiang sponge community is dominated by demosponges with a well-developed three-level tiering, consisting of 0–5 cm, 5–15 cm and 15–30 cm tiers. The majority of the sponges are restricted to the 0–15 cm tier, suggesting rich nutrients in the bottom seawater of the Cambrian ocean. Tiering in the Cambrian sponge communities is consistent and similar to that of the Ediacaran and Phanerozoic epifaunal communities, but the fourth tier (50–100 cm) in these latter communities is absent in the Cambrian communities. Demosponges dominate the shallow-water sponge communities and occur in all tiers. Hexactinellids are relatively rare and limited in the lower tiers in the shallow-water community, but dominate in the deep-water communities. The composition variation in the Cambrian sponge communities may be controlled by the differences in skeleton architecture between the Demospongiae and Hexactinellida.
Labels:
cambrian,
cambrian explosion,
fossils,
paleontology,
paleozoic,
sponges
Friday, February 07, 2014
Sponges Have Many of the Genes Associated With Complexity in
Sponges are an important animal for marine and freshwater ecology and represent a rich animal diversity found throughout the world, from tropical climates to the arctic poles. For evolutionary biologists, they also present an interesting animal for comparative study because they are simple filter feeders, and lack nervous, digestive or circulatory systems, suggesting that they diverged early from other animals.
To provide a wider framework for understanding the molecular complexity behind the evolution of sponges, authors Riesgo, Windsor, Farrar, Giribet, and Leys (from the University of Barcelona, University of Alberta and Harvard University), performed the largest sequencing study to date on the genes of representatives from eight sponge genera covering all four currently recognized sponge classes. They performed comparative analysis of animal genes important for signaling, neuronal and ionic conduction, epithelia, immunity and reproduction.
One of the remarkable results of this work, published in the journal Molecular Biology and Evolution, is the understanding that most higher animal genes, or the greater complement of genes involved in more complex gene pathways, are also present in all sponge groups. They found a number of genes that previously had been associated with complex structures of higher animals and were thought to be absent in sponges. This provides an important new resource to the question of which molecules might have been present in early animal groups, and more importantly, provides the framework for posing new hypotheses on determining gene function in sponges and the evolution of animal complexity.
link.
Labels:
animals,
genetics,
paleogenetics,
sponges
Saturday, December 28, 2013
A Cryptic Coral-crinoid "Hanging Garden" From Eifelian/Givetian Devonian Morocco
Cryptic coral-crinoid "hanging gardens" from the Middle Devonian of southern Morocco
Authors:
Jakubowicz et al
Abstract:
An unusual and exceptionally well preserved cryptic community of cnidarians, crinoids, sponges, and microbes developed in a submarine cavity of Middle Devonian age in the Hamar Laghdad area (Morocco). The biota encrusted the cavity roof and grew predominantly in an upside-down position, forming spectacular "hanging gardens." The investigated assemblage differs strikingly from both its Paleozoic and modern analogues; it constitutes one of a very few known examples of fossil cryptic assemblages developed in relatively deep water settings, and is the first report of a cryptic paleoecosystem dominated by rugose corals. The results support the view that during the middle Paleozoic there was no distinct polarization between open-surface and cryptic faunas in deep-water environments, but keen competition for space already existed in Devonian cryptic assemblages. The regional species pool seems to have been the main determinant of the ecological succession and structure of this cryptic community.
Labels:
cnidaria,
corals,
crinoids,
devonian,
eifelian,
fossils,
Givetian,
invertebrates,
morocco,
paleontology,
paleozoic,
sponges
Thursday, December 05, 2013
No Evidence of Nutrient Seasonality in Ediacaran Communities From Newfoundland
Population structure of the oldest known macroscopic communities from Mistaken Point, Newfoundland
Authors:
Simon A. F. Darroch , Marc Laflamme and Matthew E. Clapham
Abstract:
The presumed affinities of the Terminal Neoproterozoic Ediacara biota have been much debated. However, even in the absence of concrete evidence for phylogenetic affinity, numerical paleoecological approaches can be effectively used to make inferences about organismal biology, the nature of biotic interactions, and life history. Here, we examine the population structure of three Ediacaran rangeomorph taxa (Fractofusus, Beothukis, and Pectinifrons), and one non-rangeomorph taxon (Thectardis) across five fossil surfaces around the Avalon Peninsula, Newfoundland, through analysis of size-frequency distributions using Bayesian Information Criterion (BIC). Best-supported models resolve communities of all studied Ediacaran taxa at Mistaken Point as single cohorts with wide variance. This result is best explained in terms of a “continuous reproduction” model, whereby Ediacaran organisms reproduce aseasonally, so that multiple size modes are absent from preserved communities. Modern benthic invertebrates (both as a whole and within specific taxonomic groups) in deeper-water settings reproduce both seasonally and aseasonally; distinguishing between biological (i.e., continuous reproductive strategies) and environmental (lack of a seasonal trigger) causes for this pattern is therefore difficult. However, we hypothesize that the observed population structure could reflect the lack of a trigger for reproduction in deepwater settings (i.e., seasonal flux of organic matter), until the explosive appearance of mesozooplankton near the base of the Cambrian.
Labels:
Canada,
Ediacaran,
fossils,
Neoproterozoic,
newfoundland,
paleobiology,
paleoenvironment,
paleontology,
rangeomorphs,
sponges
Wednesday, January 09, 2013
Comb Jellies Are More Basal Than Sponges?
Animals evolved gradually, from the lowly sponge to the menagerie of tentacled, winged and brainy creatures that inhabit Earth today. This idea makes such intuitive sense that biologists are now stunned by genome-sequencing data suggesting that the sponges were preceded by complex marine predators called comb jellies.This is an incredible conjecture. I'll wait to see if more research backs this up. Extraordinary claims and all that. If so...the world is far, far weirder and the story of the evolution of the animal kingdom is far more complicated than we ever expected.
Although they are gelatinous like jellyfish, comb jellies form their own phylum, known as ctenophores. Trees of life typically root the comb jellies' lineage between the group containing jellyfish and sea anemones and the one containing animals with heads and rears — which include slugs, flies and humans. Comb jellies paddle through the sea with iridescent cilia and snare prey with sticky tentacles. They are much more complex than sponges — they have nerves, muscles, tissue layers and light sensors, all of which the sponges lack.
“It’s just wild to imagine” that comb jellies evolved before sponges, says Billie Swalla, a developmental biologist at the University of Washington in Seattle and a leading member of the team sequencing the genome of the comb jelly Pleurobrachia bachei. But the team is suggesting just that, in results they presented at the annual meeting of the Society for Integrative and Comparative Biology, held on 3–7 January in San Francisco, California.
Despite comb jellies' complexity, DNA sequences in the Pleurobrachia genome place them at the base of the animal tree of life, announced Swalla's colleague Leonid Moroz, a neurobiologist at the University of Florida in Gainesville. Another team presented results from genome sequencing for the comb jelly Mnemiopsis leidyi, and found that the phylum lands either below, or as close to the base as, sponges on the tree.
“We’ve always thought that predator–prey interactions and sensory adaptations evolved long after the origin of sponges,” Swalla says. “Now we need to imagine early life as a sponge, ctenophore and everything in between.” Because millions of species have gone extinct since animals appeared some 542 million years ago, Swalla says, the ancestor of all animals might look different from modern comb jellies and sponges.
Gene families, cell-signalling networks and patterns of gene expression in comb jellies support ancient origins as well. For example, Moroz and his team found that comb jellies grow their nerves with unique sets of genes. “These are aliens,” Moroz jokes. He suggests that comb jellies might be descendants of Ediacaran organisms, mysterious organisms that appear in the fossil record before animals. Indeed, in 2011, palaeontologists claimed that one of these 580-million-year-old fossils resembled comb jellies1.
Andy Baxevanis, a comparative biologist at the US National Human Genome Research Institute in Bethesda, Maryland, and a leader on the Mnemiopsis genome project, says that comb jellies are the only animals that lack certain genes crucial to producing microRNA — short RNA chains that help to regulate gene expression. Moreover, he points out, sponges and comb jellies lack other gene families that all other animals possess2, 3.
If comb jellies evolved before sponges, the sponges probably lost some of their ancestors' complexity. Alternatively, says Sally Leys, a biologist at the University of Alberta in Edmonton, sponges may have complexity that scientists have yet to appreciate. “A lot of sponges are more exquisite than a lump on a rock,” she says.
A quick thought is to look for pseudogenes in sponges that are relics from something basal to a sponge and the ctenophores.
Labels:
ctenophores,
evolution,
genetics,
invertebrates,
phylogenetics,
sponges
Wednesday, February 08, 2012
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