• Publications
  • Influence
Questioning the evidence for Earth's oldest fossils
Structures resembling remarkably preserved bacterial and cyanobacterial microfossils from ∼3,465-million-year-old Apex cherts of the Warrawoona Group in Western Australia currently provide the oldestExpand
  • 757
  • 69
  • PDF
Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event
In the Jurassic period, the Early Toarcian oceanic anoxic event (about 183 million years ago) is associated with exceptionally high rates of organic-carbon burial, high palaeotemperatures andExpand
  • 744
  • 44
Cretaceous-Tertiary Carbonate Platform Evolution and the Age of the India-Asia Collision along the Ladakh Himalaya (Northwest India)
The India-Asia collision resulted in the formation and uplift of the Himalaya and the enhanced uplift of the Tibetan plateau. The transition from marine to continental facies within the Indus–YarlungExpand
  • 177
  • 20
A fresh look at the fossil evidence for early Archaean cellular life
The rock record provides us with unique evidence for testing models as to when and where cellular life first appeared on Earth. Its study, however, requires caution. The biogenicity of stromatolitesExpand
  • 211
  • 19
  • PDF
Critical testing of Earth's oldest putative fossil assemblage from the ∼3.5Ga Apex chert, Chinaman Creek, Western Australia
Abstract Structures resembling cyanobacterial microfossils from the ca. 3465 Ma old Apex chert of the Warrawoona Group in Western Australia have until recently been accepted as providing the oldestExpand
  • 195
  • 15
  • PDF
Ediacarian sponge spicule clusters from southwestern Mongolia and the origins of the Cambrian fauna
Carbon and strontium isotopic data are used to show that the earliest sponge spicule clusters and associated phosphatic sediments (with Anabarites ) from southwestern Mongolia are of Ediacarian age.Expand
  • 202
  • 10
On biogenicity criteria for endolithic microborings on early Earth and beyond.
Micron-sized cavities created by the actions of rock-etching microorganisms known as euendoliths are explored as a biosignature for life on early Earth and perhaps Mars. Rock-dwelling organisms canExpand
  • 104
  • 9
  • PDF
Earth's Oldest (∼ 3.5 Ga) Fossils and the `Early Eden Hypothesis': Questioning the Evidence
We question the biogenicity of putative bacterial andcyanobacterial `microfossils' from3465 Ma Apex cherts of the Warrawoona Group in WesternAustralia. They arechallenged on the basis of integratedExpand
  • 92
  • 9
  • PDF
Photang thrust sheet: an accretionary complex structurally below the Spontang ophiolite constraining timing and tectonic environment of ophiolite obduction, Ladakh Himalaya, NW India
The pre-collisional tectonic evolution of the north Indian continental margin is best recorded in the few ophiolite complexes preserved, the largest of which occurs in the Spontang area of theExpand
  • 54
  • 9
The problem of deep carbon—An Archean paradox
Black carbon-rich chert dikes are common features of early Archean terranes and are especially prominent on the Pilbara Craton of Western Australia. The dikes cut across the local stratigraphy beforeExpand
  • 92
  • 8