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The Furongian (late Cambrian) Biodiversity Gap: Real or apparent?

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TLDR
The Furongian gap as mentioned in this paper is defined as the gap between the Cambrian Explosion and the Great Ordovician Biodiversification Event, exemplified by a marked drop in biodiversity.
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This article is published in Palaeoworld.The article was published on 2019-03-01 and is currently open access. It has received 35 citations till now. The article focuses on the topics: Ordovician & Paleozoic.

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Early Palaeozoic diversifications and extinctions in the marine biosphere: a continuum of change

TL;DR: A review of biodiversity curves of marine organisms indicates that, despite fluctuations in amplitude (some large), a large-scale, long-term radiation of life took place during the early Palaeozoic Era; it was aggregated by a succession of more discrete and regionalized radiations across geographies and within phylogenies.
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Revisiting the Great Ordovician Diversification of land plants: Recent data and perspectives

TL;DR: In this paper, molecular clock data suggest with high probability a Cambrian origin of Embryophyta (also called land plants), indicating that their terrestrialization most probably started about 500 Ma.

Principles Of Paleontology

TL;DR: The principles of paleontology is available in our book collection and an online access to it is set as public so you can get it instantly as discussed by the authors, which is the only way to download any of our books like this one.
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The Great Ordovician Biodiversification Event (GOBE) is Not a Single Event

TL;DR: In this paper, a critical analysis of published biodiversity curves and of their own data confirm the traditional view; the Ordovician radiation is a complex, long-term process of multiple biodiversifications of marine organisms.
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A meta-analysis of the Steptoean Positive Carbon Isotope Excursion: The SPICEraq database

TL;DR: The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a prominent chemostratigraphic feature in the Lower Paleozoic. as discussed by the authors quantitatively evaluate the variability in SPICE records, and document that while the excursion is a global signature, its stratigraphic expression is influenced by such conditions as paleolatitude, paleocontinent, water depth, and facies.
References
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Ordovician and Silurian sea–water chemistry, sea level, and climate: A synopsis

TL;DR: The authors reviewed the relationships of the three major biotic events to chemical and physical processes occurring in the ocean and atmosphere during the Ordovician and Silurian, including sea-level changes, geochemical proxies (δ13C, δ18O, 87Sr/86Sr) of the ocean waters, and the evolution of the atmosphere (oxygen and carbon dioxide content).
Book

Principles of paleontology

TL;DR: The Nature of the Fossil Record Growth and Form Populations and Species Systematics Evolutionary Morphology Biostratigraphy Evolutionary Rates and Trends Global Diversity and Extinctions Paleoecology and Paleobiogeography Multidisciplinary Studies in Paleontology.
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Large-scale heterogeneity of the fossil record: implications for Phanerozoic biodiversity studies.

TL;DR: Data on rock outcrop area compiled for post-Palaeozoic sediments from Western Europe at stage level are presented and show a strongly cyclical pattern corresponding to first- and second-order sequence stratigraphical depositional cycles.
Book

The adequacy of the fossil record

TL;DR: The fossil record of cheilostome bryozoa in the Neogene and Quaternay of tropical America - adequacy for phylogenetic and evolutionary studies and the quality of the fossil record are studied.
Journal ArticleDOI

Advances in Cambrian stratigraphy and paleontology: Integrating correlation techniques, paleobiology, taphonomy and paleoenvironmental reconstruction

TL;DR: A generalized curve of carbon isotopes (δ13C) through the Cambrian suggests a relationship between major biotic events, sea level history and the development of deposits of exceptional preservation (Lagerstatten).
Related Papers (5)

Phanerozoic trends in the global diversity of marine invertebrates.

Frequently Asked Questions (2)
Q1. What are the contributions in this paper?

Indications suggest that there has been little attention paid to this interval compared with those below and above, while some of the classical areas for Cambrian research, such as Bohemia, have poor coverage through the Furongian. Moreover, based on information available in databases and the literature, together with the ghost ranges of many higher taxa through the Furongian, data suggest that biodiversity in this stage has been significantly underestimated. 

The latter presenting the intriguing possibility that the diversification of marine ecosystems was on a single trajectory that peaked in the Devonian.