Diversificatio biotorum Ordovicia
Diversificatio biotorum Ordovicia,[1][2] Anglice aut Ordovician radiation aut great Ordovician biodiversification event, est multiplicatio specierum novarum quae media periodo Ordovicia accidisse constat, circa annorum 465 milies milium ante praesentem, post magnam pluviam meteoritarum L chondritarum[3] severamque glaciationem.
Notae
recensere- ↑ Haec appellatio a Vicipaediano e lingua indigena in sermonem Latinum conversa est. Extra Vicipaediam huius locutionis testificatio vix inveniri potest.
- ↑ Verbum "diversificatio" habes in Henrici Bateni Speculo (saec. XIII) (p. 244 apud Google Books)
- ↑ Hans-Peter Gail, Mario Trieloff, "Thermal history modeling of the L chondrite parent body" (1 Iulii 2019) apud arXiv.org pro Astronomy & Astrophysics
Bibliographia
recensere- A. Lindskog et al., "Refined Ordovician timescale reveals no link between asteroid breakup and biodiversification" in Nature Communications vol. 8 (24 Ianuarii 2017) no. 14066
- Christian M. Ø. Rasmussen et al., "Onset of main Phanerozoic marine radiation sparked by emerging Mid Ordovician icehouse" in Scientific Reports vol. 6 no. 18884 (Ianuario 2016)
- Birger Schmitz et al., "An extraterrestrial trigger for the mid-Ordovician ice age: Dust from the breakup of the L-chondrite parent body" in Science Advances vol. 5, no. 9, eaax4184 (18 Septembris 2019)
- Birger Schmitz et al., "Asteroid breakup linked to Great Ordovician Biodiversification Event" in Nature Geoscience vol. 1 (2008) pp. 49-53
- Thomas Servais et al., "The Ordovician Biodiversification: revolution in the oceanic trophic chain" in Lethaia (Iunio 2008)
- Thomas Servais, David A. T. Harper, "The Great Ordovician Biodiversification Event (GOBE) : definition, concept and duration" in Lethaia vol. 51 (2018) pp. 151-164
- Julie A. Trotter et al., "Did Cooling Oceans Trigger Ordovician Biodiversification? Evidence from Conodont Thermometry" in Science vol. 321 (2008) pp. 550-554
Nexus externi
recensere- "Great Ordovician Biodiversity Event"
- Tim Collart, A potential paleo-environmental signal in the calcareous rhythmites of the Frognerkilen Formation (uppermost Sandbian - lower Katian) in Norway (dissertatio magistralis Gandensis, 2013)