NASRRDDINE YOUBI

Prof. Dr. NASRRDDINE YOUBI

Department of Geology, Faculty of Sciences-Semlalia, Cadi Ayyad University, Marrakesh, Morocco.
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orcid

Research Focus & Metrics

Academic Career Length

32Years (1995-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 July 2017 in Palaeogeography, Palaeoclimatology, Palaeoecology
Verified
Journal Article
Closed access
RERichard Ernst
Richard Ernst
NASRRDDINE YOUBINASRRDDINE YOUBI
NASRRDDINE YOUBI

1 January 2004 in Geology
Verified
Journal Article
Closed access
AMAndrea Marzoli
Andrea Marzoli
HBHervé Bertrand
Hervé Bertrand
KKKim B. Knight
Kim B. Knight
SCSimonetta Cirilli
Simonetta Cirilli
NBNicoletta Buratti
Nicoletta Buratti
GBGiuliano Bellieni
Giuliano Bellieni
The evolution of life on Earth is marked by catastrophic extinction events, one of which occurred ca. 200 Ma at the transition from the Triassic Period to the Jurassic Period (Tr-J boundary), apparently contemporaneous with the eruption of the world's largest known continental igneous province, the Central Atlantic magmatic province. The temporal relationship of the Tr-J boundary and the province's volcanism is clarified by new multi-disciplinary (stratigraphic, palynologic, geochronologic, paleomagnetic, geochemical) data that demonstrate that development of the Central Atlantic magmatic province straddled the Tr-J boundary and thus may have had a causal relationship with the climatic crisis and biotic turnover demarcating the boundary

31 May 2017 in Nature Communications
Verified
Journal Article
Open access
PDF file
JDJoshua Davies
Joshua Davies
AMAndrea Marzoli
Andrea Marzoli
HBH. Bertrand
H. Bertrand
NASRRDDINE YOUBINASRRDDINE YOUBI
NASRRDDINE YOUBI
MEMarcia Ernesto
Marcia Ernesto
USU. Schaltegger
U. Schaltegger
The end-Triassic extinction is one of the Phanerozoic’s largest mass extinctions. This extinction is typically attributed to climate change associated with degassing of basalt flows from the central Atlantic magmatic province (CAMP). However, recent work suggests that the earliest known CAMP basalts occur above the extinction horizon and that climatic and biotic changes began before the earliest known CAMP eruptions. Here we present new high-precision U-Pb ages from CAMP mafic intrusive units, showing that magmatic activity was occurring ∼100 Kyr ago before the earliest known eruptions. We correlate the early magmatic activity with the onset of changes to the climatic and biotic records. We also report ages from sills in an organic rich sedimentary basin in Brazil that intrude synchronously with the extinction suggesting that degassing of these organics contributed to the climate change which drove the extinction. Our results indicate that the intrusive record from large igneous provinces may be more important for linking to mass extinctions than the eruptive record.

1 November 2004 in Earth and Planetary Science Letters
Verified
Journal Article
Closed access
KKK.B. Knight
K.B. Knight
SNS. Nomade
S. Nomade
PRP.R. Renne
P.R. Renne
AMAndrea Marzoli
Andrea Marzoli
HBH. Bertrand
H. Bertrand
NASRRDDINE YOUBINASRRDDINE YOUBI
NASRRDDINE YOUBI

1 February 2007 in Palaeogeography, Palaeoclimatology, Palaeoecology
Verified
Journal Article
Closed access
SNS. Nomade
S. Nomade
KKK.B. Knight
K.B. Knight
EBE. Beutel
E. Beutel
PRP.R. Renne
P.R. Renne
CVC. Verati
C. Verati
HBH. Bertrand
H. Bertrand

1 February 2007 in Palaeogeography, Palaeoclimatology, Palaeoecology
Verified
Journal Article
Closed access
CVChrystèle Verati
Chrystèle Verati
CRCédric Rapaille
Cédric Rapaille
GFGilbert Féraud
Gilbert Féraud
AMAndrea Marzoli
Andrea Marzoli
HBHervé Bertrand
Hervé Bertrand
NASRRDDINE YOUBINASRRDDINE YOUBI
NASRRDDINE YOUBI