Late Frasnian–Famennian climates based on palynomorph analyses and the question of the Late Devonian glaciations
M Streel, MV Caputo, S Loboziak, JHG Melo - Earth-Science Reviews, 2000 - Elsevier
Palynomorph distribution in Euramerica and western Gondwana, from the Latest Givetian to
the Latest Famennian, may be explained, to some extent, by climatic changes. Detailed …
the Latest Famennian, may be explained, to some extent, by climatic changes. Detailed …
Paleogeography and paleoenvironments of the Late Devonian Kellwasser event: A review of its sedimentological and geochemical expression
SK Carmichael, JA Waters, P Königshof… - Global and Planetary …, 2019 - Elsevier
Abstract The Late Devonian (383-359 Ma) was a time of prolonged climate instability with
catastrophic perturbation of global marine ecosystems at the Frasnian-Famennian (FF) and …
catastrophic perturbation of global marine ecosystems at the Frasnian-Famennian (FF) and …
Late Devonian sea-level changes, catastrophic events, and mass extinctions
C Sandberg, JR Morrow, W Ziegler - GSA Special Papers, 2002 - pubs.usgs.gov
Late Devonian history is explained through event stratigraphy comprising a sequence of 18
sea-level changes, catastrophic events, and mass extinctions. Generally rising sea level …
sea-level changes, catastrophic events, and mass extinctions. Generally rising sea level …
Extent and duration of marine anoxia during the Frasnian–Famennian (Late Devonian) mass extinction in Poland, Germany, Austria and France
The intensity and extent of anoxia during the two Kellwasser anoxic events has been
investigated in a range of European localities using a multidisciplinary approach (pyrite …
investigated in a range of European localities using a multidisciplinary approach (pyrite …
Reef development at the Frasnian/Famennian mass extinction boundary
P Copper - Palaeogeography, Palaeoclimatology, Palaeoecology, 2002 - Elsevier
A newly compiled global reef database indicates that the 5–6 Myr long Frasnian (Late
Devonian) metazoan reef episode had relatively low diversity compared to Middle Devonian …
Devonian) metazoan reef episode had relatively low diversity compared to Middle Devonian …
The Frasnian/Famennian boundary interval in the South Polish–Moravian shelf basins: integrated event-stratigraphical approach
The Late Devonian mass extinction event near the Frasnian/Famennian (F/F) boundary has
been analysed using conodont biostratigraphy and biofacies, sedimentology, magnetic …
been analysed using conodont biostratigraphy and biofacies, sedimentology, magnetic …
The role of sea-level change and marine anoxia in the Frasnian–Famennian (Late Devonian) mass extinction
DPG Bond, PB Wignall - Palaeogeography, Palaeoclimatology …, 2008 - Elsevier
Johnson et al.(Johnson, JG, Klapper, G., Sandberg, CA, 1985. Devonian eustatic
fluctuations in Euramerica. Geological Society of America Bulletin 96, 567–587) proposed …
fluctuations in Euramerica. Geological Society of America Bulletin 96, 567–587) proposed …
[HTML][HTML] 白垩纪世界与大洋红层
王成善， 胡修棉 - 地学前缘, 2005 - wenku.baidu.com
国际地球科学界视为研究地球系统科学的典型范看, 当时的海陆分布与现今最大的不同是在低
纬度[4 例, 被称为“白垩纪世界”]. 白垩纪时全球气温处地区存在一个东西向的特提斯洋(图1) …
纬度[4 例, 被称为“白垩纪世界”]. 白垩纪时全球气温处地区存在一个东西向的特提斯洋(图1) …
Global seawater redox trends during the Late Devonian mass extinction detected using U isotopes of marine limestones
Abstract The Late Devonian extinction ranks as one of the 'big five'Phanerozoic extinctions
affecting up to 80% of marine species and is characterized by two major extinction events …
affecting up to 80% of marine species and is characterized by two major extinction events …
Mountain building‐enhanced continental weathering and organic carbon burial as major causes for climatic cooling at the Frasnian–Famennian boundary (c. 376 …
O Averbuch, N Tribovillard, X Devleeschouwer… - Terra …, 2005 - Wiley Online Library
Abstract The Late Devonian was a period of drastic environmental changes, as exemplified
by a major biotic crisis at the Frasnian–Famennian boundary (FFB) and the onset in …
by a major biotic crisis at the Frasnian–Famennian boundary (FFB) and the onset in …