about
The 2.1 Ga old Francevillian biota: biogenicity, taphonomy and biodiversityA molecular genetic timescale for the diversification of autotrophic stramenopiles (Ochrophyta): substantive underestimation of putative fossil agesSystematic analysis of compositional order of proteins reveals new characteristics of biological functions and a universal correlate of macroevolutionAnoxygenic photosynthesis modulated Proterozoic oxygen and sustained Earth's middle ageDeciphering deuterostome phylogeny: molecular, morphological and palaeontological perspectivesThe Ediacaran emergence of bilaterians: congruence between the genetic and the geological fossil recordsRegulation of cellular metabolism: programming and maintaining metabolic homeostasisOxygen, ecology, and the Cambrian radiation of animalsRise to modern levels of ocean oxygenation coincided with the Cambrian radiation of animalsMorphologically Conservative but Physiologically Diverse: The Mode of Stasis in Anostraca (Crustacea: Branchiopoda)Molecular paleontology and complexity in the last eukaryotic common ancestorNon-LTR R2 element evolutionary patterns: phylogenetic incongruences, rapid radiation and the maintenance of multiple lineagesThe origin of multicellularity in cyanobacteriaAn Early Cambrian radulaAre Asteraceae 1.5 billion years old? A reply to heads.Paleontology. Terminal developments in Ediacaran embryology.Giving the early fossil record of sponges a squeeze.Ediacaran matground ecology persisted into the earliest Cambrian.Morphological preservation of carbonaceous plant fossils in blueschist metamorphic rocks from New Zealand.The subject as cause and effect of evolution.The Anthropocene biosphereNeoproterozoic ‘snowball Earth’ glaciations and the evolution of altruismEarly evolution of the EukaryotaThe Precambrian emergence of animal life: a geobiological perspectiveEvolution of the life cycle in land plantsForbidden fruits in the Garden of EdiacaraSilicified microbiota from the Paleoproterozoic Dahongyu Formation, Tianjin, ChinaBioavailability of zinc in marine systems through timeOn the flux ratio method and the number of valid species namesMacroecology: more than the division of food and space among species on continentsMOLECULAR PALAEOBIOLOGYPlants and Animals as Geobiological AgentsA germ theory for glacial systems?
P2860
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P2860
description
2007 nî lūn-bûn
@nan
2007 թուականի Յունուարին հրատարակուած գիտական յօդուած
@hyw
2007 թվականի հունվարին հրատարակված գիտական հոդված
@hy
2007年の論文
@ja
2007年論文
@yue
2007年論文
@zh-hant
2007年論文
@zh-hk
2007年論文
@zh-mo
2007年論文
@zh-tw
2007年论文
@wuu
name
MACROEVOLUTION AND MACROECOLOGY THROUGH DEEP TIME
@ast
MACROEVOLUTION AND MACROECOLOGY THROUGH DEEP TIME
@en
type
label
MACROEVOLUTION AND MACROECOLOGY THROUGH DEEP TIME
@ast
MACROEVOLUTION AND MACROECOLOGY THROUGH DEEP TIME
@en
prefLabel
MACROEVOLUTION AND MACROECOLOGY THROUGH DEEP TIME
@ast
MACROEVOLUTION AND MACROECOLOGY THROUGH DEEP TIME
@en
P2860
P1433
P1476
MACROEVOLUTION AND MACROECOLOGY THROUGH DEEP TIME
@en
P2093
NICHOLAS J. BUTTERFIELD
P2860
P356
10.1111/J.1475-4983.2006.00613.X
P577
2007-01-01T00:00:00Z