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Data from: Pacman profiling: a simple procedure to identify stratigraphic outliers in high-density deep-sea microfossil data
负责人:
关键词:
microfossils;databases;diversity;Methods;plankton;Radiolaria;biostratigraphy;Cenozoic;Polycystinea
DOI:
doi:10.5061/dryad.2m7b0
摘要:
The deep-sea microfossil record is characterized by an extraordinarily high density and abundance of fossil specimens, and by a very high degree
Data from: Human-induced marine ecological degradation: micropaleontological perspectives
负责人:
关键词:
dinoflagellate;Foraminifera;diatom;microfossils;Coccolithophore;Ostracoda;eutrophication;species diversity;pollution;marine ecosystems;hypoxia;Radiolaria;Holocene
DOI:
doi:10.5061/dryad.2t604
摘要:
, deforestation and land clearance. Microfossils enable reconstruction of the ecological history of the past 102–103 years or even more, and, in conjunction
Data from: The effect of bioturbation by polychaetes (Opheliidae) on benthic foraminiferal assemblages and test preservation
负责人:
关键词:
Cádiz;taphonomy;burrowing;Miocene;benthic foraminifera;Spain
DOI:
doi:10.5061/dryad.395sm
摘要:
ystallization. Pervasive burrowing resulted in significant vertical reworking of microfossils. As a consequence, benthic foraminiferal assemblages in the bioturbated beds
Data from: Radiolarian biodiversity dynamics through the Triassic and Jurassic: implications for proximate causes of the end-Triassic mass extinction
负责人:
关键词:
ocean acidification;Global warming;extinctions;Triassic-Jurassic boundary;radiolarians
DOI:
doi:10.5061/dryad.31g77
摘要:
for the end-Triassic event and have been also suggested for the early Toarcian. Radiolarians, as the most abundant silica-secreting marine microfossils of the time
Data from: Taxonomic structure of the fossil record is shaped by sampling bias
负责人:
关键词:
Jurassic;Upper Jurassic;taxonomy;Linnean hierarchy;diversity;fossil record;Coccolithophores;Cretaceous;Cenozoic;Haptophyta
DOI:
doi:10.5061/dryad.8476
摘要:
d to estimate species diversity through time. Using the deep-sea record of coccolithophorid microfossils over the last 150 million years (myr), we demonstrate tha
Data from: Diversity of cnidarians and cycloneuralians in the Fortunian (early Cambrian) Kuanchuanpu Formation at Zhangjiagou, South China
负责人:
关键词:
cycloneuralians;fossil embryo;Fortunian Stage;Olivooides;Quadrapyrgites;Eopriapulites;Pseudooides
DOI:
doi:10.5061/dryad.1cn6b
摘要:
The latest discovery of microfossils from lower Cambrian (Fortunian Stage) Zhangjiagou Lagerst?tte in South China are presented. This lagerst?tte
Data from: New armoured scalidophorans (Ecdysozoa, Cycloneuralia) from the Cambrian Fortunian Zhangjiagou Lagerst?tte, South China
负责人:
关键词:
Qinscolex spinosus;Scalidophora;Zhangjiagou Lagerst?tte;South China;Orsten-type fossils;Shanscolex decorus;Fortunian Stage;Cambrian Fortunian Stage;Cycloneuralia
DOI:
doi:10.5061/dryad.jj6kp7b
摘要:
d. Here, we report new three?dimensionally phosphatized microfossils of cycloneuralians from the Fortunian Zhangjiagou Lagerst?tte, South China
Data from: Clitellate worms (Annelida) in lateglacial and Holocene sedimentary DNA records from the Polar Urals and northern Norway
负责人:
Lammers, Youri
关键词:
ancient DNA environmental DNA metabarcoding clitellates
DOI:
doi:10.5061/dryad.g0f4hv0
摘要:
While there are extensive macro- and microfossil records of a range of plants and animals from Quaternary records, earthworms and their close
Data from: Molecular dating, evolutionary rates, and the age of the grasses
负责人:
关键词:
divergence time;phylogeny;molecular dating;Poaceae;mutation rate
DOI:
doi:10.5061/dryad.t5v58
摘要:
for the age of core Poaceae around 51-55 Ma, but the inclusion of microfossil evidence pushes this age to 74-82 Ma and leads to lower estimated
Data from: Timing of morphological and ecological innovations in the cyanobacteria – a key to understanding the rise in atmospheric oxygen
负责人:
关键词:
cyanobacteria\/classification;Neoproterozoic;Cyanobacteria;phylogenetics;Paleoproterozoic;Mesoproterozoic;Evolution;cyanobacteria\/growth;Phanerozoic;oxygen;Precambrian
DOI:
doi:10.5061/dryad.11vj2
摘要:
vide an explanation for why cyanobacterial microfossils have not been observed until after 2.0 Ga, and make suggestions for how future paleobiological searches for ea

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