Paul D. Taylor

ORCID: 0000-0002-3127-080X
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About
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Research Areas
  • Marine Ecology and Invasive Species
  • Marine Biology and Ecology Research
  • Marine Biology and Environmental Chemistry
  • Myxozoan Parasites in Aquatic Species
  • Paleontology and Stratigraphy of Fossils
  • Marine and coastal plant biology
  • Maritime and Coastal Archaeology
  • Marine Invertebrate Physiology and Ecology
  • Geology and Paleoclimatology Research
  • Coral and Marine Ecosystems Studies
  • Parasite Biology and Host Interactions
  • Aquatic Invertebrate Ecology and Behavior
  • Methane Hydrates and Related Phenomena
  • Marine Bivalve and Aquaculture Studies
  • Silicon Carbide Semiconductor Technologies
  • Ocean Acidification Effects and Responses
  • Plant Diversity and Evolution
  • Evolution and Paleontology Studies
  • Semiconductor materials and devices
  • Cephalopods and Marine Biology
  • Diamond and Carbon-based Materials Research
  • Marine and environmental studies
  • Ichthyology and Marine Biology
  • Paleontology and Evolutionary Biology
  • Silicon and Solar Cell Technologies

Natural History Museum
2015-2024

Dynex Semiconductor (United Kingdom)
2001-2024

Forest Research
2021-2024

The University of Western Australia
2024

University of Leeds
1974-2022

Forestry Commission England
2021

Northern Research Station
2021

German Oceanographic Museum
1994-2018

American Museum of Natural History
1997-2015

Duke University
2015

The PRINTS database houses a collection of protein fingerprints. These may be used to assign uncharacterised sequences known families and hence infer tentative functions. September 2002 release (version 36.0) includes 1800 fingerprints, encoding ∼11 000 motifs, covering range globular membrane proteins, modular polypeptides so on. In addition its continued steady growth, we report here the development an automatic supplement, prePRINTS, designed increase coverage resource reduce some manual...

10.1093/nar/gkg030 article EN Nucleic Acids Research 2003-01-01

Mass extinctions are recognized through the study of fossil groups across event horizons, and from analyses long-term trends in taxonomic richness diversity. Both approaches have inherent flaws, data that once seemed reliable can be readily superseded by discovery new fossils and/or application analytical techniques. Herein current state Cretaceous-Tertiary (K-T) biostratigraphical record is reviewed for most major clades, including: calcareous nannoplankton, dinoflagellates, diatoms,...

10.1144/gsjgs.154.2.0265 article EN Journal of the Geological Society 1997-03-01

Other| October 01, 2002 A New Terminology for Marine Organisms Inhabiting Hard Substrates PAUL D. TAYLOR; TAYLOR 1Department of Palaeontology, The Natural History Museum, London, SW7 5BD UK Search other works by this author on: GSW Google Scholar MARK A. WILSON 2Department Geology, College Wooster, OH 44691 Author and Article Information Publisher: SEPM Society Sedimentary Geology Accepted: 27 Mar First Online: 03 2017 Online ISSN: 1938-5323 Print 0883-1351 PALAIOS (2002) 17 (5): 522–525....

10.1669/0883-1351(2002)017<0522:antfmo>2.0.co;2 article EN Palaios 2002-10-01

10.1016/j.ympev.2011.11.011 article EN Molecular Phylogenetics and Evolution 2011-12-01

Abstract Although only a small fraction of the estimated 6000 extant bryozoan species has been analysed in molecular phylogenetic context, resultant trees have increased our understanding interrelationships between major groups, as well bryozoans and other metazoan phyla. Molecular systematic analyses failed to recover L ophophorata monophyletic clade until recently, when phylogenomic data placed B rachiopoda sister formed by P horonida + ryozoa. Among bryozoans, class hylactolaemata shown...

10.1111/pala.12170 article EN Palaeontology 2015-05-11

Based on the examination of type and newly discovered specimens, scope calloporid genus Pyriporoides Hayward & Thorpe, 1989 is expanded to include Daisyella Gordon, 1989. All species have colonies branching uniserial runners acleithral ovicells that are borne and/or develop concurrently with a distal heterozooid, not autozooid. The ooecial heterozooid usually kenozooidal but can be avicularian. Correlated characters include, inter alia: raised granular rim encloses generally well-developed...

10.11646/zootaxa.4242.2.1 article EN Zootaxa 2017-03-10

The cheilostome bryozoan family Steginoporellidae in New Zealand comprises seven living species of Steginoporella. Three these are new to science-Steginoporella discors n. sp., Steginoporella lineata sp. and modesta sp.-and one (Steginoporella magnifica) additionally occurs as a Plio-Pleistocene fossil. A Early Pleistocene fossil species, tiara is also recognised. exhibit the full range colonial morphologies known for genus, two deep-shelf taxa described herein have smallest colonies, both...

10.11646/zootaxa.4350.2.9 article EN Zootaxa 2017-11-17

Abstract Bryozoans (also known as ectoprocts or moss animals) are aquatic, dominantly sessile, filter-feeding lophophorates that construct an organic calcareous modular colonial (clonal) exoskeleton 1–3 . The presence of six major orders bryozoans with advanced polymorphisms in lower Ordovician rocks strongly suggests a Cambrian origin for the largest and most diverse lophophorate phylum 2,4–8 However, lack convincing bryozoan fossils from period has hampered resolution true origins...

10.1038/s41586-021-04033-w article EN cc-by Nature 2021-10-27

Calcareous tube-worms generally identified as Spirorbis range from Ordovician to Recent, often profusely encrusting shells and other substrates. Whereas Recent is a polychaete annelid, details of tube structure in pre-Cretaceous ‘ ’ suggest affinities with the Microconchida, an extinct order possible lophophorates. Although characteristically Palaeozoic, microconchid survived Permian mass extinction before being replaced late Mesozoic ecosystems by true . stenohaline but spirorbiform...

10.1144/0016-764905-145 article EN Journal of the Geological Society 2006-02-10

Watersipora subtorquata (d'Orbigny, 1852) has been widely reported as a fouling species from tropical to temperate waters. The continued confusion over the correct name for this led us provide redescription of d'Orbigny's type Cellepora subtorquata, and make comparisons with other Watersipora. We show that majority specimens assigned W. subovoidea are morphologically distinct recently erected neotype subovoidea; these here reidentified subtorquata. Other previously belong subatra (Ortmann,...

10.11646/zootaxa.3857.2.1 article EN Zootaxa 2014-08-28

Bryozoans are a key group of sessile invertebrates in some reef frameworks but typically neglected environmental monitoring programs. Abrolhos Bank (Brazil) is the largest complex South Atlantic Ocean, encompassing several landscapes over an area 46,000 km2. A transition takes place across shelf from mangroves to soft sediments, coastal shallow reefs volcanic archipelago – surrounded by fringing and unique mushroom-shaped biogenic structures, with mesophotic pinnacle reefs, rhodolith beds,...

10.11646/zootaxa.4483.1.6 article EN Zootaxa 2018-09-20

Abstract Many animals and plants that colonize hard surfaces in the sea are sessile either bore into, or cement themselves permanently to substrate surface. Because they retain their life positions after fossilization, these sclerobionts offer scope for studying biotic interactions fossil record. Encrusting compete actively living space, with dominant competitors overgrowing edges of subordinates. In addition such marginal overgrowths, spatial competition may also occur through fouling which...

10.1111/pala.12239 article EN Palaeontology 2016-04-05

Beginning in December 2015, an unknown bryozoan with large, deep-orange colonies began to appear the Eastern Harbour of Alexandria, Egypt. Here we identify species as belonging predominantly Indo-Pacific cheilostome genus Calyptotheca Harmer, 1957 and describe it a new species, alexandriensis n. sp. The exhibits intensive growth sporadically on different hard substrata, including rocks, submerged concrete walls, ropes, ships’ hulls, metal pipes supporting marina piers. It is restricted...

10.11646/zootaxa.4276.4.9 article EN Zootaxa 2017-06-14

Microporella Hincks, 1877 is one of the most diverse genera cheilostome bryozoans, containing more than 150 named species. Distributed globally since early Miocene, majority species have sheet-like colonies encrusting hard and / or ephemeral substrates, while a limited number erect bifoliate starting from an base. Herein, four nominal (M. bifoliata, M. hastigera, hyadesi ordo) are revised, new Pliocene tanyae sp. nov.) three Recent ordoides nov., lingulata nov. modesta formally described....

10.5852/ejt.2020.678 article EN cc-by European Journal of Taxonomy 2020-07-02

A one‐dimensional, thermodynamic, and radiative model of a melt pond on sea ice is presented that explicitly treats the as an extra phase. two‐stream radiation model, which allows albedo to be determined from bulk optical properties, parameterization summertime evolution used. Heat transport within described using equation describing heat in mushy layer binary alloy (salt water). The tested by comparison numerical simulations with SHEBA data previous modeling. presence ponds surface...

10.1029/2004jc002361 article EN Journal of Geophysical Research Atmospheres 2004-12-01

Research Article| May 01, 1998 Bryozoan carbonates through time and space Paul D. Taylor; Taylor 1Department of Palaeontology, Natural History Museum, London SW7 5BD, United Kingdom Search for other works by this author on: GSW Google Scholar Peter A. Allison Kingdom2Department Geology, Imperial College, 2BP Author Article Information Publisher: Geological Society America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print 0091-7613 Geology (1998) 26 (5): 459–462....

10.1130/0091-7613(1998)026<0459:bcttas>2.3.co;2 article EN Geology 1998-01-01

A macroevolutionary model is developed to account for the "adaptive radiation"; of cheilostome bryozoans that commenced in Cenomanian after a long phase low diversity. Living species possess one two types larvae; planktotrophic (cyphonautes) larvae relatively duration, and brooded non‐planktotrophic (coronate) short duration. Planktotrophic characterize paraphyletic "malacostegans"; from which "advanced"; cheilostomes with are thought have evolved monophyletically. Research on other marine...

10.1080/08912968809386466 article EN Historical Biology 1988-01-01

We present a mathematical model describing the summer melting of sea ice. simulate evolution melt ponds and determine area coverage total surface ablation. The predictions are tested for sensitivity to rate unponded ice, enhanced beneath ponds, vertical seepage, horizontal permeability. is initialized with topographies derived from laser altimetry corresponding first‐year ice multiyear predict that there large differences in depth between two types also find seepage important determining...

10.1029/2004jc002818 article EN Journal of Geophysical Research Atmospheres 2006-02-01

10.1016/0031-0182(87)90039-3 article EN Palaeogeography Palaeoclimatology Palaeoecology 1987-01-01

Cheilostomes dominate bryozoan faunas today and are the only order of bryozoans to have evolved aragonitic, calcitic, bimineralic skeletons. New XRD analyses 177 recent species 34 Cretaceous–Eocene combined with published data probe mineralogical evolution cheilostomes. This is undertaken particular reference effects late Paleogene transition from calcite aragonite seas believed been driven by increasing Mg/Ca ratio in seawater. Aragonite was absent all Cretaceous Paleocene cheilostomes...

10.2110/palo.2008.p08-124r article EN Palaios 2009-07-01

Ecological interactions affect the survival and reproduction of individuals. However, ecological are notoriously difficult to measure in extinct populations, hindering our understanding how outcomes such as competition vary time influence long-term evolutionary changes. Here, spatial a temporally continuous community over timescales presented for first time. Our research domain is encrusting cheilostome bryozoans from Wanganui Basin New Zealand ca 2 Myr period (Pleistocene Recent). We find...

10.1098/rspb.2016.0981 article EN cc-by Proceedings of the Royal Society B Biological Sciences 2016-08-31
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