Adjusting Global Extinction Rates to Account for Taxonomic Susceptibility

Total Page:16

File Type:pdf, Size:1020Kb

Adjusting Global Extinction Rates to Account for Taxonomic Susceptibility Paleobiology, 34(4), 2008, pp. 434–455 Adjusting global extinction rates to account for taxonomic susceptibility Steve C. Wang and Andrew M. Bush Abstract.—Studies of extinction in the fossil record commonly involve comparisons of taxonomic extinction rates, often expressed as the percentage of taxa (e.g., families or genera) going extinct in a time interval. Such extinction rates may be influenced by factors that do not reflect the intrinsic severity of an extinction trigger. Two identical triggering events (e.g., bolide impacts, sea level changes, volcanic eruptions) could lead to different taxonomic extinction rates depending on fac- tors specific to the time interval in which they occur, such as the susceptibility of the fauna or flora to extinction, the stability of food webs, the positions of the continents, and so on. Thus, it is pos- sible for an extinction event with a higher taxonomic extinction rate to be caused by an intrinsically less severe trigger, compared to an event with a lower taxonomic extinction rate. Here, we isolate the effects of taxonomic susceptibility on extinction rates. Specifically, we quan- tify the extent to which the taxonomic extinction rate in a substage is elevated or depressed by the vulnerability to extinction of classes extant in that substage. Using a logistic regression model, we estimate that the taxonomic susceptibility of marine fauna to extinction has generally declined through the Phanerozoic, and we adjust the observed extinction rate in each substage to estimate the intrinsic extinction severity more accurately. We find that mass extinctions do not generally occur during intervals of unusually high susceptibility, although susceptibility sometimes increas- es in post-extinction recovery intervals. Furthermore, the susceptibility of specific animal classes to extinction is generally similar in times of background and mass extinction, providing no evi- dence for differing regimes of extinction selectivity. Finally, we find an inverse correlation between extinction rate within substages and the evenness of diversity of major taxonomic groups, but fur- ther analyses indicate that low evenness itself does not cause high rates of extinction. Steve C. Wang. Department of Mathematics and Statistics, Swarthmore College, Swarthmore, Pennsylvania 19081. E-mail: [email protected] Andrew M. Bush. Department of Ecology and Evolutionary Biology and Center for Integrative Geosciences, University of Connecticut, 75 North Eagleville Rd, Unit 3043, Storrs, Connecticut 06269. E-mail: [email protected] Accepted: 2 June 2008 Introduction identity of taxa going extinct in a geologic time interval determine the consequences of Measuring extinction intensity by the per- an extinction event for the history of life, but centage of taxa that go extinct is like measur- these rates are a measure of the intensity of ing the strength of an earthquake by the effect, which may not directly reflect the in- amount of damage inflicted, either in lives lost tensity of cause. Given the same environmen- or property destroyed. In actuality, the dam- tal conditions or extinction trigger, two faunas age caused by an earthquake reflects two fac- may have different extinction rates, just as two tors: the strength of the earthquake itself and locations may suffer different amounts of the susceptibility of the local population and death and damage from an earthquake of the infrastructure. The former (intensity of cause) same intensity. Here, we attempt to infer the can be measured on the familiar Richter scale, intensity of cause of extinctions in the marine but the latter (intensity of effect) is affected by fossil record, at least in a partial fashion. Spe- factors like population density and the resis- cifically, we focus on the potential of faunas of tance of buildings to damage. From the stand- different taxonomic composition to suffer dif- point of an earthquake’s effects on society, the ferent extinction rates given causal triggers of amount of damage is the more important var- similar physical intensity. Our goal is to an- iable, but for understanding the causes of an swer the following questions: (1) Does the re- earthquake, its physical intensity must be lationship between the intensity of cause and known as well. Likewise, the proportion and effect change in important ways through the ᭧ 2008 The Paleontological Society. All rights reserved. 0094-8373/08/3404-0002/$1.00 TAXONOMIC SUSCEPTIBILITY AND EXTINCTION 435 Phanerozoic, or among mass extinctions, re- jects, including gender bias in graduate ad- coveries, and background intervals? (2) Are missions (Bickel et al. 1975), airline on-time there other ways, at a very broad scale, in rates (Barnett 1994), and racial bias in capital which the changing taxonomic composition of punishment (Gross and Mauro 1984). A clas- the marine fauna affected extinction rates? sic example of Simpson’s paradox occurred in Other paleontologists have also examined a study on heart disease and a follow-up the relationship between extinction rates and study conducted 20 years later (Appleton et al. the changing composition of the marine biota, 1996). The authors found, surprisingly, that ascribing the Phanerozoic decline in extinc- women who smoked had a lower death rate af- tion rates to a shift in dominance from taxa ter 20 years than women who had never with high rates to those with low rates (Stan- smoked (24% mortality rate versus 31%, re- ley 1979, 2007; Sepkoski 1984, 1991; Van Valen spectively). Because this finding contradicted 1985, 1987; Gilinsky 1994). Our goal is not to a priori medical knowledge, the authors in- replicate these efforts, but rather to analyti- vestigated further, dividing the women into cally remove the effects of changing taxonom- subgroups according to age. A different pic- ic composition on observed extinction rates, ture then emerged: the smokers’ death rate allowing us to see how changes in composi- equaled or exceeded the non-smokers’ death tion might bias our views of the intrinsic in- rate in every age subgroup, as would be ex- tensity of extinction triggers. For example, pected. Why, then, when the subgroups were were the effects of some mass extinctions mit- aggregated, did smoking appear to increase igated by a particularly extinction-resistant longevity? fauna? Were the effects of other mass extinc- This apparent paradox occurred because tions especially severe because they affected the smokers’ age distribution differed from extinction-prone taxa? We also introduce a that of the non-smokers. The non-smokers in- method for analytically estimating how much cluded a higher percentage of older women of the decline in extinction rates resulted from (who grew up when smoking among women the changing taxonomic composition of the was less common), and older women have in- marine biosphere. herently higher death rates regardless of whether or not they smoke. The smokers, on Simpson’s Paradox: Do Smokers the other hand, disproportionately included Live Longer? younger women. Once age differences in the Comparisons of taxonomic extinction rates two groups were taken into account, it became (whether using percentage extinction or an- clear that smoking did indeed increase mor- other metric) are the basis of many quantita- tality. tive studies of mass extinction events (e.g., This kind of pattern defines Simpson’s par- Raup and Sepkoski 1982, 1984; Benton 1995; adox: trends in aggregated percentages dis- Wang 2003; Bambach et al. 2004; MacLeod appear or even reverse themselves when one 2004; Rohde and Muller 2005; Bambach 2006). partitions the data into subgroups, such as age However, such comparisons of aggregate ex- groups. In this example, discovering Simp- tinction rates can be misleading. It is possible son’s paradox was not difficult: the aggregat- for one event to have a higher extinction rate ed data were clearly misleading, because we for each of several subgroups within the data knew a priori that smoking is detrimental to set, yet for another event to have a higher ex- one’s health. We also knew that age is related tinction rate for the data set as a whole. This to mortality rate, so it was natural to separate apparent contradiction can appear when sub- the data into subgroups by age. groups with different extinction rates change In other cases, however, Simpson’s paradox in relative abundance through time—a statis- can be more insidious. We may have no a tical artifact known as Simpson’s paradox priori belief that an aggregated data set is (Simpson 1951). yielding a misleading conclusion, so we may Examples of Simpson’s paradox appear in not suspect a need to partition the data into the statistical literature on a variety of sub- subgroups. Even if we have reason to subdi- 436 STEVE C. WANG AND ANDREW M. BUSH TABLE 1. Diversity of major molluscan classes in the Ordovician (Ashgillian) and end-Permian (Djhulfian) mass extinctions. Columns give the number of genera going extinct in the interval (Extinct), total diversity in the interval (Diversity), and extinction rate (Percent) for each extinction event. These data demonstrate Simpson’s paradox: the Permian has a higher intrinsic severity, because the extinction rate for each class is higher in the Permian than in the Ordovician. However, when the classes are combined, the overall molluscan extinction rate is higher in the Ordovician. This misleading effect occurs because the Ordovician fauna has a large number of extinction-suscep- tible cephalopods, whereas the Permian fauna has a large number of extinction-resistant gastropods. Data are from Sepkoski’s genus compendium (2002), as compiled by Bambach (1999) and Bambach et al. (2004); non-integer counts are due to fractional allocation of poorly-resolved genera. Ordovician Permian Extinct Diversity Percent Extinct Diversity Percent Cephalopoda 77.9 103.9 75 37.3 48.3 77 Bivalvia 48.1 80.1 60.0 48.3 80.3 60.1 Gastropoda 31.6 73.6 43 52.2 101.2 52 Mollusca 157.6 257.6 61 137.8 229.8 60 vide the data, there may no natural criterion Considering all three classes combined, by which to do so.
Recommended publications
  • Associated Organisms Inhabiting the Calcareous Sponge Clathrina Lutea in La Parguera Natural
    bioRxiv preprint doi: https://doi.org/10.1101/596429; this version posted April 3, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Associated organisms inhabiting the calcareous sponge Clathrina lutea in La Parguera Natural 2 Reserve, Puerto Rico 3 4 Jaaziel E. García-Hernández1,2*, Nicholas M. Hammerman2,3*, Juan J. Cruz-Motta2 & Nikolaos V. 5 Schizas2 6 * These authors contributed equally 7 1University of Puerto Rico at Mayagüez, Department of Biology, PO Box 9000, Mayagüez, PR 8 00681 9 2University of Puerto Rico at Mayagüez, Department of Marine Sciences, Marine Genomic 10 Biodiversity Laboratory, PO Box 9000, Mayagüez, PR 00681 11 3School of Biological Sciences, University of Queensland, Gehrmann Laboratories, Level 8, 12 Research Road, St Lucia, QLD 4072, Australia 13 14 15 Nikolaos V. Schizas, [email protected], FAX: 787-899-5500 16 17 Running Head: Infauna of the calcareous sponge Clathrina lutea 18 19 20 1 bioRxiv preprint doi: https://doi.org/10.1101/596429; this version posted April 3, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 21 ABSTRACT 22 Sponges provide an array of ecological services and benefits for Caribbean coral reefs. They 23 function as habitats for a bewildering variety of species, however limited attention has been paid 24 in the systematics and distribution of sponge-associated fauna in the class Calcarea or for that 25 matter of sponges in the Caribbean.
    [Show full text]
  • End-Permian Mass Extinction in the Oceans: an Ancient Analog for the Twenty-First Century?
    EA40CH05-Payne ARI 23 March 2012 10:24 End-Permian Mass Extinction in the Oceans: An Ancient Analog for the Twenty-First Century? Jonathan L. Payne1 and Matthew E. Clapham2 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305; email: [email protected] 2Department of Earth and Planetary Sciences, University of California, Santa Cruz, California 95064; email: [email protected] Annu. Rev. Earth Planet. Sci. 2012. 40:89–111 Keywords First published online as a Review in Advance on ocean acidification, evolution, isotope geochemistry, volcanism, January 3, 2012 biodiversity The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The greatest loss of biodiversity in the history of animal life occurred at the 10.1146/annurev-earth-042711-105329 end of the Permian Period (∼252 million years ago). This biotic catastro- Annu. Rev. Earth Planet. Sci. 2012.40:89-111. Downloaded from www.annualreviews.org Copyright c 2012 by Annual Reviews. phe coincided with an interval of widespread ocean anoxia and the eruption All rights reserved of one of Earth’s largest continental flood basalt provinces, the Siberian by Stanford University - Main Campus Robert Crown Law Library on 06/04/12. For personal use only. 0084-6597/12/0530-0089$20.00 Traps. Volatile release from basaltic magma and sedimentary strata dur- ing emplacement of the Siberian Traps can account for most end-Permian paleontological and geochemical observations. Climate change and, per- haps, destruction of the ozone layer can explain extinctions on land, whereas changes in ocean oxygen levels, CO2, pH, and temperature can account for extinction selectivity across marine animals.
    [Show full text]
  • 1 Class Stenolaemata Order Cyclostomata Philip E
    1 Class Stenolaemata Order Cyclostomata Philip E. Bock, Paul D. Taylor, Peter J. Hayward and Dennis P. Gordon 1.1 Definition and general description may be encrusting or erect and branching or foli- Stenolaemata is the most ancient bryozoan class, ose. They are typically dense, opaque white in with a fossil record beginning in the earliest Ordo- colour, occasionally flushed pink or purple, and vician, ~500 million years ago (Taylor and Ernst the calcification can appear speckled because of the 2004; Ma et al. 2015). Seven orders are recognised presence of numerous tissue-plugged pseudopores. currently (Taylor and Waeschenbach 2015), of In the Crisiidae, exemplifying the erect, branching which only Cyclostomata survives and includes all Articulata, the zooids are arranged in narrow rows living stenolaemate species. Globally, the order with openings on only one side of the slender, flex- Cyclostomata includes some 543 species assigned ible colony of branches linked by cuticular joints to 98 genera and 23 families (Bock and Gordon (nodes). Erect colonies of species of Tubuliporina, 2013). The group comprises, on average, ~11% of Cancellata and Cerioporina are unjointed (with the the species in any Recent bryozoan fauna (range single exception of the tubuliporine genus Crisuli- 0–24%, Banta 1991) and only rarely dominates in pora), gracile to robust, and have zooids arranged terms of numbers of colonies or biomass. evenly, in clusters or in ordered transverse rows. Stenolaemates are commonly termed ‘tubular Many species of Tubuliporina have encrusting col- bryozoans’, in reference to their elongate, slender, onies, occasionally taking the form of simple, uni- usually cylindrical zooids.
    [Show full text]
  • The Evolution of the Mitochondrial Genomes of Calcareous Sponges and Cnidarians Ehsan Kayal Iowa State University
    Iowa State University Capstones, Theses and Graduate Theses and Dissertations Dissertations 2012 The evolution of the mitochondrial genomes of calcareous sponges and cnidarians Ehsan Kayal Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/etd Part of the Evolution Commons, and the Molecular Biology Commons Recommended Citation Kayal, Ehsan, "The ve olution of the mitochondrial genomes of calcareous sponges and cnidarians" (2012). Graduate Theses and Dissertations. 12621. https://lib.dr.iastate.edu/etd/12621 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. The evolution of the mitochondrial genomes of calcareous sponges and cnidarians by Ehsan Kayal A dissertation submitted to the graduate faculty in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Major: Ecology and Evolutionary Biology Program of Study Committee Dennis V. Lavrov, Major Professor Anne Bronikowski John Downing Eric Henderson Stephan Q. Schneider Jeanne M. Serb Iowa State University Ames, Iowa 2012 Copyright 2012, Ehsan Kayal ii TABLE OF CONTENTS ABSTRACT ..........................................................................................................................................
    [Show full text]
  • Monophyly of Bryozoa
    Chapter 7 Summarizing discussion The studies in the preceding chapters have all focussed on morphological characters of the Bryozoa that are potentially of phylogenetic signifi cance, but suffer from a lack of knowl- edge or ambiguous scoring. Both molecular analyses and morphology-based phylogenies have so far failed to provide a consistent hypothesis of the position of the Bryozoa in the phylogenetic system. Further questions that are controversially discussed include the inter- nal relationships of Bryozoa and their monophyly. In the following section, I will review these problems and discuss in synopsis the impact of the present results on the different hypotheses. Relationships within Bryozoa The relationships between the recent bryozoan higher taxa are still relatively uncertain and so far only few phylogenetic accounts exist (Cuffey and Blake 1991, Todd 2000). Phylactolaemata and Cheilostomata are generally regarded as monophyletic (Mundy et al. 1981, Taylor 1990, Okuyama et al. 2006), whereas some evidence, mainly from palaeontology argues for paraphyly of ctenostomes (Taylor and Larwood 1990, Todd 2000). Stenolaemata are also suggested to be paraphyletic (Ernst and Schäfer 2006), but Cyclostomata, their only recent representatives are likely monophyletic (Borg 1927, Schäfer 1991, Taylor and Weedon 2000, but see Boardman 1998). Traditionally, Phylactolaemata are thought to be sister-group to the remaining Bryozoa (e.g., Silén 1942, Marcus 1958, Hyman 1959, Ax 2001). However, Cuffey and Blake (1991) regard Stenolaemata as sister to a taxon compris- ing Phylactolaemata and Gymnolaemata. Considerable morphological differences have long been recognized between Phylactolaemata on the one side and Stenolaemata and Gymnolaemata on the other (Allman 1856, see Hyman 1959, Ryland 1970, Mukai et al.
    [Show full text]
  • Paleophysiology and End-Permian Mass Extinction ⁎ Andrew H
    Earth and Planetary Science Letters 256 (2007) 295–313 www.elsevier.com/locate/epsl Frontiers Paleophysiology and end-Permian mass extinction ⁎ Andrew H. Knoll a, , Richard K. Bambach b, Jonathan L. Payne c, Sara Pruss a, Woodward W. Fischer d a Department of Organimsic and Evolutionary Biology, Harvard University, Cambridge MA 02138, USA b Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington DC 20560, USA c Department of Geological and Environmental Sciences, Stanford University, Stanford CA 94305, USA d Department of Earth and Planetary Sciences, Harvard University, USA Received 13 October 2006; received in revised form 17 January 2007; accepted 6 February 2007 Available online 11 February 2007 Editor: A.N. Halliday Abstract Physiological research aimed at understanding current global change provides a basis for evaluating selective survivorship associated with Permo-Triassic mass extinction. Comparative physiology links paleontological and paleoenvironmental observations, supporting the hypothesis that an end-Permian trigger, most likely Siberian Trap volcanism, touched off a set of physically-linked perturbations that acted synergistically to disrupt the metabolisms of latest Permian organisms. Global warming, anoxia, and toxic sulfide probably all contributed to end-Permian mass mortality, but hypercapnia (physiological effects of elevated PCO2) best accounts for the selective survival of marine invertebrates. Paleophysiological perspectives further suggest that persistent or recurring hypercapnia/global warmth also played a principal role in delayed Triassic recovery. More generally, physiology provides an important way of paleobiological knowing in the age of Earth system science. © 2007 Elsevier B.V. All rights reserved. Keywords: Permian; Triassic; mass extinction; physiology; paleontology 1. Introduction strophic environmental change has impacted both the diversity and ecological structure of marine and ter- Paleontologists have traditionally focused on mor- restrial biotas.
    [Show full text]
  • Evolution, Origins and Diversification of Parasitic Cnidarians
    1 Evolution, Origins and Diversification of Parasitic Cnidarians Beth Okamura*, Department of Life Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom. Email: [email protected] Alexander Gruhl, Department of Symbiosis, Max Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359 Bremen, Germany *Corresponding author 12th August 2020 Keywords Myxozoa, Polypodium, adaptations to parasitism, life‐cycle evolution, cnidarian origins, fossil record, host acquisition, molecular clock analysis, co‐phylogenetic analysis, unknown diversity Abstract Parasitism has evolved in cnidarians on multiple occasions but only one clade – the Myxozoa – has undergone substantial radiation. We briefly review minor parasitic clades that exploit pelagic hosts and then focus on the comparative biology and evolution of the highly speciose Myxozoa and its monotypic sister taxon, Polypodium hydriforme, which collectively form the Endocnidozoa. Cnidarian features that may have facilitated the evolution of endoparasitism are highlighted before considering endocnidozoan origins, life cycle evolution and potential early hosts. We review the fossil evidence and evaluate existing inferences based on molecular clock and co‐phylogenetic analyses. Finally, we consider patterns of adaptation and diversification and stress how poor sampling might preclude adequate understanding of endocnidozoan diversity. 2 1 Introduction Cnidarians are generally regarded as a phylum of predatory free‐living animals that occur as benthic polyps and pelagic medusa in the world’s oceans. They include some of the most iconic residents of marine environments, such as corals, sea anemones and jellyfish. Cnidarians are characterised by relatively simple body‐plans, formed entirely from two tissue layers (the ectoderm and endoderm), and by their stinging cells or nematocytes.
    [Show full text]
  • Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park
    Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park By Linda Sue Lassiter1, Justin S. Tweet2, Frederick A. Sundberg3, John R. Foster4, and P. J. Bergman5 1Northern Arizona University Department of Biological Sciences Flagstaff, Arizona 2National Park Service 9149 79th Street S. Cottage Grove, Minnesota 55016 3Museum of Northern Arizona Research Associate Flagstaff, Arizona 4Utah Field House of Natural History State Park Museum Vernal, Utah 5Northern Arizona University Flagstaff, Arizona Introduction As impressive as the Grand Canyon is to any observer from the rim, the river, or even from space, these cliffs and slopes are much more than an array of colors above the serpentine majesty of the Colorado River. The erosive forces of the Colorado River and feeder streams took millions of years to carve more than 290 million years of Paleozoic Era rocks. These exposures of Paleozoic Era sediments constitute 85% of the almost 5,000 km2 (1,903 mi2) of the Grand Canyon National Park (GRCA) and reveal important chronologic information on marine paleoecologies of the past. This expanse of both spatial and temporal coverage is unrivaled anywhere else on our planet. While many visitors stand on the rim and peer down into the abyss of the carved canyon depths, few realize that they are also staring at the history of life from almost 520 million years ago (Ma) where the Paleozoic rocks cover the great unconformity (Karlstrom et al. 2018) to 270 Ma at the top (Sorauf and Billingsley 1991). The Paleozoic rocks visible from the South Rim Visitors Center, are mostly from marine and some fluvial sediment deposits (Figure 5-1).
    [Show full text]
  • Marine Flora and Fauna of the Northeastern United States Erect Bryozoa
    NOAA Technical Report NMFS 99 February 1991 Marine Flora and Fauna of the Northeastern United States Erect Bryozoa John S. Ryland Peter J. Hayward U.S. Department of Commerce NOAA Technical Report NMFS _ The major responsibilities of the National Marine Fisheries Service (NMFS) are to monitor and assess the abundance and geographic distribution of fishery resources, to understand and predict fluctuations in the quantity and distribution of these resources, and to establish levels for their optimum use. NMFS i also charged with the development and implementation of policies for managing national fishing grounds, development and enforcement of domestic fisheries regulations, urveillance of foreign fishing off nited States coastal waters, and the development and enforcement of international fishery agreements and policies. NMFS also assists the fishing industry through marketing service and economic analysis programs, and mortgage in­ surance and ve sel construction subsidies. It collects, analyzes, and publishes statistics on various phases of the industry. The NOAA Technical Report NMFS series was established in 1983 to replace two subcategories of the Technical Reports series: "Special Scientific Report-Fisheries" and "Circular." The series contains the following types of reports: Scientific investigations that document long-term continuing programs of NMFS; intensive scientific report on studies of restricted scope; papers on applied fishery problems; technical reports of general interest intended to aid conservation and management; reports that review in considerable detail and at a high technical level certain broad areas of research; and technical papers originating in economics studies and from management investigations. Since this is a formal series, all submitted papers receive peer review and those accepted receive professional editing before publication.
    [Show full text]
  • Marine Ecology Progress Series 378:113
    Vol. 378: 113–124, 2009 MARINE ECOLOGY PROGRESS SERIES Published March 12 doi: 10.3354/meps07850 Mar Ecol Prog Ser Independent evolution of matrotrophy in the major classes of Bryozoa: transitions among reproductive patterns and their ecological background Andrew N. Ostrovsky1, 4,*, Dennis P. Gordon2, Scott Lidgard3 1Department of Invertebrate Zoology, Faculty of Biology & Soil Science, St. Petersburg State University, Universitetskaja nab. 7/9, 199034, St. Petersburg, Russia 2National Institute of Water & Atmospheric Research, Private Bag 14901, Kilbirnie, Wellington, New Zealand 3Department of Geology, Field Museum of Natural History, 1400 S. Lake Shore Dr., Chicago, Illinois 60605, USA 4Present address: Department of Palaeontology, Faculty of Earth Sciences, Geography and Astronomy, Geozentrum, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria ABSTRACT: Bryozoa are unique among invertebrates in possessing placenta-like analogues and exhibiting extraembryonic nutrition in all high-level (class) taxa. Extant representatives of the classes Stenolaemata and Phylactolaemata are evidently all placental. Within the Gymnolaemata, placenta- like systems have been known since the 1910s in a few species, but are herein reported to be wide- spread within this class. Placental forms include both viviparous species, in which embryonic devel- opment occurs within the maternal body cavity, and brooding species, in which development proceeds outside the body cavity. We have also identified an unknown reproductive pattern involv- ing macrolecithal oogenesis and placental nutrition from a new, taxonomically extensive anatomical study of 120 species in 92 genera and 48 families of the gymnolaemate order Cheilostomata. Results support the hypothesis of evolution of oogenesis and placentation among Cheilostomata from oligolecithal to macrolecithal oogenesis, followed by brooding, through incipient matrotrophy com- bining macrolecithal oogenesis and placentation, to oligolecithal oogenesis with subsequent placen- tal brooding.
    [Show full text]
  • Bryozoans in Archaeology 1. Introduction 2. Bryozoan Biology
    Reprinted from Internet Archaeology, 35 (2013) Bryozoans in Archaeology Matthew Law School of History, Archaeology and Religion, Cardiff University, Colum Drive, Cardiff, CF10 3EU. Email: [email protected] ORCID: 0000-0002-6127-5353 Summary Bryozoans (Phylum Bryozoa) are colony-forming invertebrates found in marine and freshwater contexts. Many are calcified, while some others have chitinous buds, and so have archaeological potential, yet they are seldom investigated, perhaps due to considerable difficulties with identification. This article presents an overview of bryozoans, as well as summarising archaeological contexts in which bryozoans might be expected to occur, and highlighting some previous work. It also presents methods and directions to maximise the potential of bryozoans in archaeological investigations. Features o Keywords: Bryozoa, environmental archaeology, palaeoecology, biological remains, marine shells, freshwater sediments, marine sediments 1. Introduction Bryozoans (Phylum Bryozoa), also known as sea mats or moss animals and formerly as Polyzoa or Entroprocta, are colony-forming sessile invertebrates, comprising communities of separate individuals known as zooids. There are around 6000 living species known in the world (Benton and Harper 2009, 314). Most are marine, although brackish and freshwater species exist. Generally, they occur on hard substrates such as rocks, shells and the fronds of seaweeds, although there are forms that live on mud and sand. Many are calcified, and others have chitinous buds, and have the potential to be preserved in archaeological contexts, yet they are seldom investigated, perhaps due to considerable difficulties with identification. Considerably more work has been done on geological assemblages and more still on living colonies; however, in general the group is not well known (Francis 2001, 106).
    [Show full text]
  • (Use Bookmarks to Browse) News from the Membership New
    BBuulllleettiinn Volume 7 Number 2 July 2011 (Use bookmarks to browse) News from the Membership New Members Frank Kenneth (Ken) McKinney, 1943-2011 Ken McKinney: How I Discovered Bryozoans Sea Drift – Remembering Ken McKinney European Journal of Taxonomy Report from the 10th Larwood Meeting Announcement: 11th Larwood Meeting Award for the Bryozoa Home Page New from the IBA: Annals of Bryozoology 3 Bryozoan Bookstall In Memoriam: Karen Emilie Bille Hansen In Memoriam: Rory Milne Featured Journal Covers Meetings and Conferences Recent Publications Copyright © 2011 by the International Bryozoology Association. Eckart Håkansson, President Timothy S. Wood, Secretary Abigail Smith, Treasurer ISSN 1941-7918 Comments regarding this Bulletin should be addressed to the IBA Secretary: [email protected] Further information at www.bryozoa.net/iba News from the Membership Priska Schäfer, Andrej Ernst, and Joachim Scholz. We would like to inform the IBA community, that the conference volume of "Bryozoan studies 2010" is in good progress. We intend to have the volume published in spring 2012. Best wishes from Kiel! Alex Gruhl. I am very pleased to have received an EU Marie Curie post-doctoral fellowship to work for two more years with Beth Okamura at the NHM in London. In this project we will continue research on myxozoan parasites, with a specific focus on development and evolution of major body plan features in this group. And of course I will also not neglect their hosts - bryozoans! More soon on one of the next meetings! Masato Hirose. Recently, I have got postdoctoral fellow in the National Museum of Nature and Sciences Tokyo.
    [Show full text]