David A. T. Harper

ORCID: 0000-0003-1315-9494
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About
Contact & Profiles
Research Areas
  • Paleontology and Stratigraphy of Fossils
  • Geology and Paleoclimatology Research
  • Marine Biology and Ecology Research
  • Geological Studies and Exploration
  • Geological and Geochemical Analysis
  • Evolution and Paleontology Studies
  • Geochemistry and Elemental Analysis
  • Geological formations and processes
  • Paleontology and Evolutionary Biology
  • Geochemistry and Geologic Mapping
  • Hydrocarbon exploration and reservoir analysis
  • Geological Formations and Processes Exploration
  • Geological and Geophysical Studies
  • Marine and environmental studies
  • Marine and coastal plant biology
  • Cephalopods and Marine Biology
  • Isotope Analysis in Ecology
  • Pleistocene-Era Hominins and Archaeology
  • Aquatic Invertebrate Ecology and Behavior
  • Marine Bivalve and Aquaculture Studies
  • Astro and Planetary Science
  • Methane Hydrates and Related Phenomena
  • Morphological variations and asymmetry
  • Scientific Research and Discoveries
  • Space Exploration and Technology

Durham University
2016-2025

ProMedica Toledo Hospital
2025

University of Toledo
2024-2025

National Museums Scotland
2025

Natural History Museum
2001-2024

Medica (United States)
2024

Lund University
2010-2023

University of Tartu
2023

China University of Geosciences
2016-2023

McLean Hospital
2022-2023

The Ordovician biodiversification has been recognized since the 1960s; term 'The Great Biodiversification Event', abbreviated by many as 'GOBE', used for past 20 years. conceptual development and terminology applied to this crucial episode in marine life signify its considerable complexity. GOBE includes successive biodiversity phases of pelagic benthic biotas, possibly decoupled. Put simply, can be seen a sequence diversifications planktonic (late Cambrian–Early Ordovician), level-bottom...

10.1111/let.12259 article EN Lethaia 2018-01-22

Abstract The Great Ordovician Biodiversification Event (GOBE) was the most rapid and sustained increase in marine Phanerozoic biodiversity. What generated this biotic response across Palaeozoic seascapes is a matter of debate; several intrinsic extrinsic drivers have been suggested. One climate, which recent years has undergone paradigm shift from text-book example an extended greenhouse to interval with transient cooling intervals – at least during Late Ordovician. Here, we show first...

10.1038/srep18884 article EN cc-by Scientific Reports 2016-01-06

Xu Chen , Jiayu Rong, Junxuan Fan, Renbin Zhan Charles E. Mitchell, David A.T. Harper, Michael J. Melchin, Ping'an Peng, Stan C. Finney, Xiaofeng Wang. Episodes 2006;29:183-96. https://doi.org/10.18814/epiiugs/2006/v29i3/004

10.18814/epiiugs/2006/v29i3/004 article EN cc-by-nc Episodes 2006-09-01

10.1016/j.palaeo.2005.07.010 article EN Palaeogeography Palaeoclimatology Palaeoecology 2005-09-20

Abstract This paper is a revision of the standard chronostratigraphy Ordovician historical type area in England and Wales. The response to need for more precise definitions series stages, especially practical international correlation. In some cases this has entailed moving horizons Series bases away from those classical sections. scheme will be used as forthcoming Correlation Chart British System. divided into five series: Tremadoc, Arenig, Llanvirn, Caradoc Ashgill. Llanvirn extended...

10.1017/s0016756800011390 article EN Geological Magazine 1995-01-01

Late Ordovician to earliest Silurian is an important geological period marked by large and biological events. However, the strata fossils of this interval are not complete in many parts world. Based on studies 43 sites South China, particular continuous sections Yangtze platform, we recognize a succession including seven graptolite zones two shelly faunas. In ascending order, Dicellograptus complanatus , complexus Paraorthograptus pacificus (including Lower Subzone, Tangyagraptus typicus...

10.1017/s0016756800004702 article EN Geological Magazine 2000-11-01

ABSTRACT A global review of new and existing data on the distribution uppermost Ordovician (Hirnantian) brachiopods indicates existence at least three biogeographically distinct faunas. The typical Hirnantia fauna characterised subtropical temperate latitudes comprised a variety ecological associations; reached its acme during bohemicus uniformis zones. Atypical faunas, developed marginal to Gondwana, are low diversity have few species in common with fauna; their spatial probably marked...

10.1017/s026359330001436x article EN Transactions of the Royal Society of Edinburgh Earth Sciences 1988-01-01

“The Great Ordovician Biodiversification Event” (GOBE) was arguably the most important and sustained increase of marine biodiversity in Earth’s history. During a short time span 25 Ma, an “explosion” diversity at order, family, genus, species level occurred. The combined effects several geological biological processes helped generate GOBE. peak GOBE correlates with unique paleogeography, featuring greatest continental dispersal Paleozoic. Rapid sea-floor spreading during this coincided warm...

10.1130/gsatg37a.1 article EN GSA Today 2009-01-01

Preface. 1. Paleontology as a science . in the modern world. science. Steps to understanding. Fossils and evolution. today. Review questions. References. Further reading. 2. time space Frameworks. On ground: lithostratigraphy. Use of fossils: discovery biostratigraphy. Paleobiogeography. fold belts. 3. Taphonomy quality fossil record Fossil preservation. Quality record. 4. Paleoecology paleoclimates Paleoecology. Paleoclimates. 5. Macroevolution tree life. Evolution by natural selection. The...

10.5860/choice.46-6814 article EN Choice Reviews Online 2009-08-01

Abstract The phylogeographical evolution and the consequent changing distribution diversity of rhynchonelliform brachiopods through Ordovician are linked to dynamic palaeogeography period. Early (Tremadocian Floian) is characterized by globally low-diversity faunas with local biodiversity epicentres, notably on South China Palaeoplate; low-latitude porambonitoid-dominated early plectambonitoid clitambonitoid representatives, as well high-latitude assemblages mostly dominated orthoids, can be...

10.1144/m38.11 article EN Geological Society London Memoirs 2013-01-01

Abstract We present a new approach to laser ablation inductively coupled plasma mass spectrometry (LA‐ICP‐MS) U‐Pb dating of carbonates based on selection and pooling pixels from 2‐D elemental isotopic ratio maps. This image mapping technique is particularly useful for targeting subdomains in samples with complex geological histories. Key major trace elements that are sensitive detrital components, postformational fluid ingress, mineralogical changes, or diagenetic overprinting measured...

10.1029/2018gc007850 article EN Geochemistry Geophysics Geosystems 2018-11-28

The Ordovician biodiversification is considered one of the most significant radiations in marine ecosystems entire Phanerozoic. Originally recognized as 'Ordovician Radiation', a label retained during 1980s and 1990s, term 'Great Biodiversification Event' (GOBE) was coined late 1990s subsequently adopted by scientific community. biodiversification, has always been long-term adaptive radiation, resulting sum different individual diversifications all groups organisms that occurred...

10.2517/2021pr001 article EN Paleontological Research 2021-10-01
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