Philipp Böning
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View article: Hydrothermal mobilization and molecular transformations of dissolved organic matter from deep subsurface sediments
Hydrothermal mobilization and molecular transformations of dissolved organic matter from deep subsurface sediments Open
Carbon mobilization in hydrothermal sediments and advective transport of dissolved organic matter (DOM) to the ocean affect deep-sea ecosystems. However, the link between hydrothermal processes and DOM reactivity in organic-rich subsurface…
View article: Environmental DNA metabarcoding accelerates integral conservation assessments and species rediscoveries in tropical biodiversity hotspots
Environmental DNA metabarcoding accelerates integral conservation assessments and species rediscoveries in tropical biodiversity hotspots Open
Environmental DNA (eDNA) metabarcoding is an emerging and versatile tool in biodiversity research. With recent advances in field sampling techniques, this approach becomes increasingly suited for application in tropical ecosystems where bi…
View article: Stratigraphy and dating of Middle Pleistocene sediments from Rodderberg, Germany
Stratigraphy and dating of Middle Pleistocene sediments from Rodderberg, Germany Open
The stratigraphy and dating of lacustrine sediments and loess derivatives from Rodderberg, a crater of the East Eifel Volcanic Field in Germany, is based on luminescence dating and incorporates radiocarbon ages, fingerprinting of key tephr…
View article: Geochemical and depositional environment of an Upper Cretaceous greensand giant (Münsterland Cretaceous Basin, Germany)
Geochemical and depositional environment of an Upper Cretaceous greensand giant (Münsterland Cretaceous Basin, Germany) Open
Based on integrated geochemical, mineralogical and stratigraphic-sedimentological analyses of core section KB 4507/1001 Essen-Bedingrade from the Münsterland Cretaceous Basin (northern Germany), the geochemical and depositional environment…
View article: The erosional and weathering response to arc–continent collision in New Guinea
The erosional and weathering response to arc–continent collision in New Guinea Open
Arc–continent collision is a fundamental stage in the plate-tectonic cycle that allows the continental crust to grow and can influence global climate through chemical weathering. Collision between Australia and the oceanic North Coast Rang…
View article: Dissolved Organic Matter from Coastal Vegetated Ecosystems Through the Lens of Carbon Sequestration
Dissolved Organic Matter from Coastal Vegetated Ecosystems Through the Lens of Carbon Sequestration Open
Coastal vegetated ecosystems (CVEs) are highly productive habitats whose role in coastal biogeochemical cycles cannot be understated. The high productivity of salt marshes, seagrass meadows, and mangrove forests is channeled into the sedim…
View article: Sedimentary mercury cycling in recent upwelling systems
Sedimentary mercury cycling in recent upwelling systems Open
The sedimentary database of mercury (Hg) in modern upwelling sediments from the Humboldt and Benguela current systems is sparse, yet this element is a prime indicator of anthropogenic perturbations of the marine realm. Mercury has various …
View article: High enrichment of U, Cr, As and V in fish scales from the Namibian shelf of the Benguela Upwelling System.
High enrichment of U, Cr, As and V in fish scales from the Namibian shelf of the Benguela Upwelling System. Open
Enrichment patterns of redox- and biosensitive trace elements (TEs) are powerful tools to reconstruct depositional conditions during sedimentation in continental marine sediments. For several TEs (e.g., U, Cr, As and V), the mechanisms tha…
View article: Successful Drug-Mediated Host Clearance of <i>Batrachochytrium salamandrivorans</i>
Successful Drug-Mediated Host Clearance of <i>Batrachochytrium salamandrivorans</i> Open
Skin fungi are among the most dangerous drivers of global amphibian declines, and few mitigation strategies are known. For Batrachochytrium salamandrivorans (Chytridiomycota), available treatments rely on temperature, partially combined wi…
View article: Enhanced chemical weathering of the continents promoted fast Late Cretaceous nearshore glaucony formation: implications from the Danubian Cretaceous Group, Germany
Enhanced chemical weathering of the continents promoted fast Late Cretaceous nearshore glaucony formation: implications from the Danubian Cretaceous Group, Germany Open
Supplementary Table S1 provides contents of total carbon (TC), total inorganic carbon (TIC), total organic carbon (TOC), major elements and Zr as well as element/Al ratios, calculated excess K (Kxs), silicate K (Ksil or K2Osil), molar elem…
View article: Enhanced chemical weathering of the continents promoted fast Late Cretaceous nearshore glaucony formation: implications from the Danubian Cretaceous Group, Germany
Enhanced chemical weathering of the continents promoted fast Late Cretaceous nearshore glaucony formation: implications from the Danubian Cretaceous Group, Germany Open
Supplementary Table S1 provides contents of total carbon (TC), total inorganic carbon (TIC), total organic carbon (TOC), major elements and Zr as well as element/Al ratios, calculated excess K (Kxs), silicate K (Ksil or K2Osil), molar elem…
View article: Enhanced chemical weathering of the continents promoted fast Late Cretaceous nearshore glaucony formation: implications from the Danubian Cretaceous Group, Germany
Enhanced chemical weathering of the continents promoted fast Late Cretaceous nearshore glaucony formation: implications from the Danubian Cretaceous Group, Germany Open
Supplementary Table S1 provides contents of total carbon (TC), total inorganic carbon (TIC), total organic carbon (TOC), major elements and Zr as well as element/Al ratios, calculated excess K (Kxs), silicate K (Ksil or K2Osil), molar elem…
View article: Seawater‐Particle Interactions of Rare Earth Elements and Neodymium Isotopes in the Deep Central Arctic Ocean
Seawater‐Particle Interactions of Rare Earth Elements and Neodymium Isotopes in the Deep Central Arctic Ocean Open
In the central Arctic Ocean, dissolved rare earth element concentrations ([dREE]) and the neodymium (Nd) isotope compositions are constant throughout the deep water column (>1,000 m water depth), indicating unique conditions among the ocea…
View article: Uranium Isotope Fractionation in Non‐sulfidic Anoxic Settings and the Global Uranium Isotope Mass Balance
Uranium Isotope Fractionation in Non‐sulfidic Anoxic Settings and the Global Uranium Isotope Mass Balance Open
Uranium isotopes ( 238 U/ 235 U) have been used widely over the last decade as a global proxy for marine redox conditions. The largest isotopic fractionations in the system occur during U reduction, removal, and burial. Applying this basic…
View article: Late Pliocene and Early Pleistocene Variability of the REE and Nd Isotope Composition of Caribbean Bottom Water: A Record of Changes in Sea Level and Terrestrial Inputs During the Final Stages of Central American Seaway Closure
Late Pliocene and Early Pleistocene Variability of the REE and Nd Isotope Composition of Caribbean Bottom Water: A Record of Changes in Sea Level and Terrestrial Inputs During the Final Stages of Central American Seaway Closure Open
The isotopic composition of neodymium dissolved in seawater consists of a distal, advected component that reflects water mass mixing and circulation but near land can also contain a large local component originating from terrestrial source…
View article: Asian summer monsoon influence on chemical weathering and sediment provenance determined by clay mineral analysis from the Indus Submarine Canyon
Asian summer monsoon influence on chemical weathering and sediment provenance determined by clay mineral analysis from the Indus Submarine Canyon Open
Clay minerals from the Indus Canyon and eastern clinoform since ~12 ka are uniformly rich in smectite and illite, similar to those from the Holocene Indus flood plains. A systematic enrichment of smectite in the proximal delta compared to …
View article: Spatial and Temporal Patterns of Pore Water Chemistry in the Inter-Tidal Zone of a High Energy Beach
Spatial and Temporal Patterns of Pore Water Chemistry in the Inter-Tidal Zone of a High Energy Beach Open
Submarine groundwater discharge (SGD) is a ubiquitous source of meteoric fresh groundwater and recirculating seawater to the coastal ocean. Due to the hidden distribution of SGD, as well as the hydraulic- and stratigraphy-driven spatial an…
View article: ERRATUM: Climatic and glacial impact on erosion patterns and sediment provenance in the Himalayan rain shadow, Zanskar River, NW India
ERRATUM: Climatic and glacial impact on erosion patterns and sediment provenance in the Himalayan rain shadow, Zanskar River, NW India Open
ORIGINAL ARTICLE: 2017, v. 129, no. 7/8, p. 820-836, https://doi.org/10.1130/B31573.1. First published 28 April 2017. ERRATUM PUBLICATION: 2019, v. 131, no. 3/4, p. 704, https://doi.org/10.1130/B31573E.1. First published 31 January 2019. S…
View article: (Table S3b) YREE and U composition of weakly cleaned foraminifera for MIS 95-100 on ODP Site 165-999
(Table S3b) YREE and U composition of weakly cleaned foraminifera for MIS 95-100 on ODP Site 165-999 Open
Concentrations in ppm in solid CaCO3.\n(a) Age model Groeneveld et al. (2014)\n(b) 2σ SD reproducibility based on repeat measurements of the ECRM standard (Greaves et al., 2008) (n=8).\n(c) HREE/LREE = [YbN + LuN]/[PrN + NdN]\n(d) MREE/MRE…
View article: (Table S3a) YREE and U composition of weakly cleaned foraminifera for MIS M2 from ODP Site 165-999A
(Table S3a) YREE and U composition of weakly cleaned foraminifera for MIS M2 from ODP Site 165-999A Open
Concentrations in ppm in solid CaCO3.\n(a) Composite depth, De Schepper et al. (2013)\n(b) Age model De Schepper et al. (2013)\n(c) 2σ SD reproducibility based on repeat measurements of the ECRM standard (Greaves et al., 2008) (n=8).\n(d) …
View article: (Table S2a) Trace element composition of weakly cleaned foraminifera for MIS M2 from ODP Site 165-999A
(Table S2a) Trace element composition of weakly cleaned foraminifera for MIS M2 from ODP Site 165-999A Open
(a) Composite depth, De Schepper et al. (2013)\n(b) Age model De Schepper et al. (2013)\n(c) Using Nd concentration measured during trace element analysis\n(d) 2σ SD reproducibility based on repeat measurements of the ECRM standard (Greave…
View article: Neodymium isotope, trace- and rare-earth element concentrations in foraminifera from ODP Site 999
Neodymium isotope, trace- and rare-earth element concentrations in foraminifera from ODP Site 999 Open
Nd-isotope, trace- and rare-earth element concentrations measured in weakly cleaned foraminifera from ODP 999 for two time slices: MIS M2 (Late Pliocene) and MIS 95-100 (Early Pleistocene).