Paleoenvironmental changes and biotic response to Aptian−Albian episodes of accelerated global change: evidence from the western margin of the proto-North Atlantic (central-eastern Mexico)

2021 ◽  
pp. 104883
Author(s):  
Nicté A. Gutiérrez-Puente ◽  
Ricardo Barragán ◽  
Fernando Núñez-Useche
Keyword(s):  
Global Change ◽  
North Atlantic ◽  
Western Margin ◽  
Paleoenvironmental Changes ◽  
Biotic Response ◽  
Central Eastern

The biotic response to global change: a summary

2000 ◽  
pp. 391-398
Author(s):  
Stephen J. Culver ◽  
Peter F. Rawson
Keyword(s):  
Global Change ◽  
Biotic Response

scholarly journals Acoustic divergence between bottlenose dolphin whistles from the Central–Eastern North Atlantic and Mediterranean Sea

2013 ◽  
Vol 17 (3) ◽  
pp. 155-165 ◽  
Author(s):  
E. Papale ◽  
M. Azzolin ◽  
I. Cascão ◽  
A. Gannier ◽  
M. O. Lammers ◽  
...  
Keyword(s):  
Mediterranean Sea ◽  
North Atlantic ◽  
Bottlenose Dolphin ◽  
Central Eastern ◽  
Eastern North Atlantic

Modern Coral Reefs Under Global Change: New Opportunities to Understand Carbonate Depositional Hiatuses

2011 ◽  
Vol 17 ◽  
pp. 121-130 ◽  
Author(s):  
Pamela Hallock
Keyword(s):  
Global Change ◽  
Coral Reefs ◽  
Environmental Change ◽  
Mass Extinction ◽  
Paleoenvironmental Changes ◽  
Carbonate Sedimentation ◽  
Depositional Systems ◽  
Geologic Record ◽  
Extinction Events ◽  
Mass Extinction Events

As shallow-water reefs decline worldwide, opportunities abound for researchers to expand understanding of carbonate depositional systems. Recognizing the myriad of paradoxes associated with reefs and carbonate research hopefully can stimulate new questions that will assist researchers in understanding paleoenvironmental changes and mass extinction events. Two often counter-intuitive concepts are discussed, first that coral reefs thrive in clear, nutrient-poor waters, except when they don't; and second, that aragonite is energetically efficient for reef-builders to precipitate in tropical waters, except when it isn't. Coordinated studies of carbonate geochemistry with photozoan physiology and calcification will contribute to understanding carbonate sedimentation under environmental change, both in the future and in the geologic record.

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