Environmental changes and growth history of a cold-water carbonate mound (Propeller Mound, Porcupine Seabight)

2005 ◽  
Vol 96 (1) ◽  
pp. 57-72 ◽  
Author(s):  
Andres Rüggeberg ◽  
Christian Dullo ◽  
Boris Dorschel ◽  
Dierk Hebbeln
Keyword(s):  
Environmental Changes ◽  
Cold Water ◽  
Carbonate Mound ◽  
Porcupine Seabight ◽  
Growth History ◽  
History Of ◽  
Water Carbonate

Growth history of a cold-water coral covered carbonate mound — Galway Mound, Porcupine Seabight, NE-Atlantic

2008 ◽  
Vol 253 (3-4) ◽  
pp. 160-169 ◽  
Author(s):  
Markus Eisele ◽  
Dierk Hebbeln ◽  
Claudia Wienberg
Keyword(s):  
Cold Water ◽  
Ne Atlantic ◽  
Carbonate Mound ◽  
Porcupine Seabight ◽  
Growth History ◽  
History Of ◽  
Water Coral

scholarly journals Subsurface microbiology and biogeochemistry of a deep, cold-water carbonate mound from the Porcupine Seabight (IODP Expedition 307)

2009 ◽  
Vol 11 (1) ◽  
pp. 239-257 ◽  
Author(s):  
Gordon Webster ◽  
Anna Blazejak ◽  
Barry A. Cragg ◽  
Axel Schippers ◽  
Henrik Sass ◽  
...  
Keyword(s):  
Cold Water ◽  
Carbonate Mound ◽  
Porcupine Seabight ◽  
Subsurface Microbiology ◽  
Water Carbonate

scholarly journals Microfossils, a Key to Unravel Cold-Water Carbonate Mound Evolution through Time: Evidence from the Eastern Alboran Sea

PLoS ONE ◽  
2015 ◽  
Vol 10 (10) ◽  
pp. e0140223 ◽  
Author(s):  
Claudio Stalder ◽  
Agostina Vertino ◽  
Antonietta Rosso ◽  
Andres Rüggeberg ◽  
Claudius Pirkenseer ◽  
...  
Keyword(s):  
Cold Water ◽  
Alboran Sea ◽  
Carbonate Mound ◽  
Alborán Sea ◽  
Water Carbonate

Carbonate budget of a cold-water coral carbonate mound: Propeller Mound, Porcupine Seabight

2005 ◽  
Vol 96 (1) ◽  
pp. 73-83 ◽  
Author(s):  
Boris Dorschel ◽  
Dierk Hebbeln ◽  
Andres Rüggeberg ◽  
Christian Dullo
Keyword(s):  
Cold Water ◽  
Carbonate Mound ◽  
Porcupine Seabight ◽  
Carbonate Budget ◽  
Coral Carbonate ◽  
Water Coral

Sediment accumulation on a cold-water carbonate mound at the Southwest Rockall Trough margin

2009 ◽  
Vol 265 (1-2) ◽  
pp. 40-50 ◽  
Author(s):  
F. Mienis ◽  
C. van der Land ◽  
H.C. de Stigter ◽  
M. van de Vorstenbosch ◽  
H. de Haas ◽  
...  
Keyword(s):  
Cold Water ◽  
Sediment Accumulation ◽  
Carbonate Mound ◽  
Rockall Trough ◽  
Water Carbonate

scholarly journals Scientific drilling of a cold-water carbonate mound: Shipboard biogeochemical results from IODP Expedition 307

2006 ◽  
Vol 70 (18) ◽  
pp. A170 ◽  
Author(s):  
T.G. Ferdelman ◽  
A. Kano ◽  
T. Williams ◽  
B.A. Cragg ◽  
T.D. Frank ◽  
...  
Keyword(s):  
Cold Water ◽  
Carbonate Mound ◽  
Scientific Drilling ◽  
Water Carbonate

scholarly journals Holocene growth history of a reef complex on a cool-water carbonate margin: Easter Group of the Houtman Abrolhos, Eastern Indian Ocean

1993 ◽  
Vol 115 (1-2) ◽  
pp. 29-46 ◽  
Author(s):  
L.B Collins ◽  
Z.R Zhu ◽  
K.-H Wyrwoll ◽  
B.G Hatcher ◽  
P.E Playford ◽  
...  
Keyword(s):  
Indian Ocean ◽  
Eastern Indian Ocean ◽  
Cool Water ◽  
Reef Complex ◽  
Growth History ◽  
History Of ◽  
Water Carbonate

scholarly journals Current understanding on the Cambrian Explosion: questions and answers

PalZ ◽  
2021 ◽  
Author(s):  
Xingliang Zhang ◽  
Degan Shu
Keyword(s):  
Environmental Changes ◽  
Size Variation ◽  
Progressive Increase ◽  
Cambrian Explosion ◽  
Time Interval ◽  
Early Cambrian ◽  
Ecological Processes ◽  
Questions And Answers ◽  
Evolutionary Event ◽  
History Of

AbstractThe Cambrian Explosion by nature is a three-phased explosion of animal body plans alongside episodic biomineralization, pulsed change of generic diversity, body size variation, and progressive increase of ecosystem complexity. The Cambrian was a time of crown groups nested by numbers of stem groups with a high-rank taxonomy of Linnaean system (classes and above). Some stem groups temporarily succeeded while others were ephemeral and underrepresented by few taxa. The high number of stem groups in the early history of animals is a major reason for morphological gaps across phyla that we see today. Most phylum-level clades achieved their maximal disparity (or morphological breadth) during the time interval close to their first appearance in the fossil record during the early Cambrian, whereas others, principally arthropods and chordates, exhibit a progressive exploration of morphospace in subsequent Phanerozoic. The overall envelope of metazoan morphospace occupation was already broad in the early Cambrian though it did not reach maximal disparity nor has diminished significantly as a consequence of extinction since the Cambrian. Intrinsic and extrinsic causes were extensively discussed but they are merely prerequisites for the Cambrian Explosion. Without the molecular evolution, there could be no Cambrian Explosion. However, the developmental system is alone insufficient to explain Cambrian Explosion. Time-equivalent environmental changes were often considered as extrinsic causes, but the time coincidence is also insufficient to establish causality. Like any other evolutionary event, it is the ecology that make the Cambrian Explosion possible though ecological processes failed to cause a burst of new body plans in the subsequent evolutionary radiations. The Cambrian Explosion is a polythetic event in natural history and manifested in many aspects. No simple, single cause can explain the entire phenomenon.

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