Glaciatio Ordovicia media
Glaciatio Ordovicia media,[1] Anglice mid Ordovician glaciation vel icehouse, est frigus globale quod media periodo Ordovicia accidisse constat, circa annorum 467 milies milium ante praesentem, post magnam pluviam meteoritarum L chondritae,[2] insequente diversificatione specierum.
Notae recensere
- ↑ Haec appellatio a Vicipaediano e lingua indigena in sermonem Latinum conversa est. Extra Vicipaediam huius locutionis testificatio vix inveniri potest.
- ↑ 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
- M. P. Dabard et al., "Sea-level curve for the Middle to early Late Ordovician in the Armorican Massif (western France): Icehouse third-order glacio-eustatic cycles" in Palaeogeography, Palaeoclimatology, Palaeoecology vol. 436 (2015) pp. 96-111
- 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)
- Julie A. Trotter et al., "Did Cooling Oceans Trigger Ordovician Biodiversification? Evidence from Conodont Thermometry" in Science vol. 321 (2008) pp. 550-554