about
Mediterranean megaturbidite triggered by the AD 365 Crete earthquake and tsunami.Ribosomal RNA gene fragments from fossilized cyanobacteria identified in primary gypsum from the late Miocene, Italy.Postglacial response of Arctic Ocean gas hydrates to climatic amelioration.Seepage from an arctic shallow marine gas hydrate reservoir is insensitive to momentary ocean warmingNovel biomineralization strategy in calcareous foraminiferaA thermogenic hydrocarbon seep in shallow Adriatic Sea (Italy): Gas origin, sediment contamination and benthic foraminiferaDeep-sourced gas seepage and methane-derived carbonates in the Northern Adriatic SeaAn integrated view of the methane system in the pockmarks at Vestnesa Ridge, 79°NLate Holocene foraminifera of Blake Ridge diapir: Assemblage variation and stable-isotope record in gas-hydrate bearing sedimentsRecord of methane emissions from the West Svalbard continental margin during the last 23.500yrs revealed by δ13C of benthic foraminiferaTracing seafloor methane emissions with benthic foraminifera: Results from the Ana submarine landslide (Eivissa Channel, Western Mediterranean Sea)Methane seepages recorded in benthic foraminifera from Miocene seep carbonates, Northern Apennines (Italy)Late Miocene seep-carbonates and fluid migration on top of the Montepetra intrabasinal high (Northern Apennines, Italy): Relations with synsedimentary foldingComplementary biomarker-based methods for characterising Arctic sea ice conditions: A case study comparison between multivariate analysis and the PIP25 indexMethane seepage at Vestnesa Ridge (NW Svalbard) since the Last Glacial MaximumPalaeoceanographic and environmental changes in the eastern Fram Strait during the last 14,000 years based on benthic and planktonic foraminiferaDiagenetic Mg-calcite overgrowths on foraminiferal tests in the vicinity of methane seepsDiagenetic alteration of benthic foraminifera from a methane seep site on Vestnesa Ridge (NW Svalbard)Foram-AMBI: A sensitivity index based on benthic foraminiferal faunas from North-East Atlantic and Arctic fjords, continental shelves and slopesPaleo-methane emissions recorded in foraminifera near the landward limit of the gas hydrate stability zone offshore western SvalbardRemoval of methane through hydrological, microbial, and geochemical processes in the shallow sediments of pockmarks along eastern Vestnesa Ridge (Svalbard)Are repetitive slumpings during sapropel S1 related to paleo-earthquakes?Bivalve shell horizons in seafloor pockmarks of the last glacial-interglacial transition: a thousand years of methane emissions in the Arctic OceanCarbon isotope (δ<sup>13</sup>C) excursions suggest times of major methane release during the last 14 kyr in Fram Strait, the deep-water gateway to the ArcticMud volcanoes along the inner deformation front of the Calabrian Arc accretionary wedge (Ionian Sea)Turbidite paleoseismology in the Calabrian Arc Subduction Complex (Ionian Sea)Benthic Foraminifera of the Blake Ridge hydrate mound, Western North Atlantic OceanForaminiferal response to an active methane seep environment: A case study from the Adriatic SeaTHE EFFECT OF SHALLOW MARINE HYDROTHERMAL VENT ACTIVITY ON BENTHIC FORAMINIFERA (AEOLIAN ARC, TYRRHENIAN SEA)Benthic foraminifera associated with a hydrocarbon seep in the Rockall Trough (NE Atlantic)Benthic foraminifera from a recent, shallow-water hydrothermal environment in the Aeolian Arc (Tyrrhenian Sea)How are benthic foraminiferal faunas influenced by cold seeps? Evidence from the Miocene of ItalyNordic Seas polynyas and their role in preconditioning marine productivity during the Last Glacial MaximumMethane-fuelled biofilms predominantly composed of methanotrophic ANME-1 in Arctic gas hydrate-related sedimentsThe benthic foraminiferal δ34S records flux and timing of paleo methane emissions
P50
Q30458228-109D4F68-75C8-46BB-AB64-BB1F15D708C1Q33522766-8CC897AA-3AF2-413D-B195-00D47994CE7BQ36393556-368D5F2F-15AE-4AF3-80B0-0942EC2C5717Q41089301-1744C43A-170D-4F38-AF1C-C66B8940417EQ57212261-AD538B85-18FB-434B-BC93-2A98CB9F711EQ57272043-1E422E4A-F263-4949-B906-3520A55DD322Q57691884-4D8342AA-4A73-4AF8-9038-FB25C2975748Q57851013-4C5C0183-DCDC-47DA-B137-395FD258F4BBQ57865799-D9BB7F63-F400-4A0F-9C0D-21090B8AA88DQ57865805-10F0984E-5970-4AF5-8A89-24414AFC7375Q57865865-1FED5F90-3B3A-4052-9AC3-1BDEFEFE52A3Q57865896-F26D2241-C1A6-4461-A9A1-2144BDC7B34BQ57872470-CB3CFE7A-F789-4752-8472-E80D69BAFAA0Q57885267-B4EA15B9-B397-4ECC-A160-483B2389ED9FQ57885271-E59FA5C4-ED69-4E39-AFF0-413EA3FFA666Q57885275-CC046999-E308-45F9-828B-EFD43F5C91A0Q57885279-7418795F-1425-4CB8-B093-FCC09DF5D39FQ57885282-D1208D37-3A33-4559-A0BA-3BCBADB2B2EFQ57885286-94726624-FB9F-4C66-83E9-2945B8CF71F3Q57885290-05B1D2CB-B8D9-4659-9C7C-3BEC3B6A6A7AQ57885293-DB302B53-6E71-4076-9B98-B34B04D2F9CCQ57885296-DF8A1737-5A64-4327-AEED-9F83876C356AQ57885305-8D1FE7D1-58F9-4F07-8985-55AEA2A68BF2Q57885311-C00D4D9B-F83E-44C9-8E05-F68F4E89B815Q57885325-864871CB-1142-4061-B02A-63102BBCEFCCQ57885331-F4CFB973-61AA-44F2-8C9D-4AAA89CDD267Q57885343-295AA0C0-C073-49B2-9124-7C1577338DC8Q57885348-49E9E474-D4C9-459B-8EBA-A8F6626DE275Q57885354-DEE9D025-470E-4DEC-8C5B-0DD5AF319B37Q57885362-1CBB60C4-9C2B-418E-8628-8ABE1B93A4A4Q57885367-E767AAEF-25AE-4B16-86F9-529D88236C0CQ57885374-6291BAB0-DB5A-4B55-9CF4-44A70BE8EFC1Q59128999-D944C2B3-0DBE-4E4E-852E-5586A100CDD8Q91666256-3FE80B94-BF35-4D56-9D11-DCE499079995Q93012677-86184B14-D7F5-4EE1-A20F-F0EBAEF2EB85
P50
description
onderzoeker
@nl
researcher ORCID ID = 0000-0001-9411-1729
@en
name
Giuliana Panieri
@ast
Giuliana Panieri
@en
Giuliana Panieri
@es
Giuliana Panieri
@nl
type
label
Giuliana Panieri
@ast
Giuliana Panieri
@en
Giuliana Panieri
@es
Giuliana Panieri
@nl
prefLabel
Giuliana Panieri
@ast
Giuliana Panieri
@en
Giuliana Panieri
@es
Giuliana Panieri
@nl
P106
P21
P31
P496
0000-0001-9411-1729