Major Element Composition of Sediments in Terms of Weathering and Provenance: Implications for Crustal Recycling

The elemental composition of a sediment is set by the composition of its protolithand modified by weathering, sorting, and diagenesis. An important problem is deconvolving these contributions to a sediment’s composition to arrive at information about processesthat operate on the Earth’s surface. We approach this problem by developing a predictive andinvertible model of sedimentary major-element composition. We compile a dataset of sedimentary rock, river sediment, soil, and igneous rock compositions. Principal componentanalysis of the dataset shows that most variation can be simplified to a small number of variables. We thus show that any sediment’s composition can be described with just two vectorsof igneous evolution and weathering. We hence define a model for sedimentary compositionas a combination of these processes. A 1:1 correspondence is observed between predictionsand independent data. The log-ratios ln(K 2 O/MgO) and ln(Al 2 O 3 /Na 2 O) are found to besimple proxies for respectively the model’s protolith and weathering indices. Significant deviations from the model can be explained by sodium-calcium exchange. Using this approach,we show that the major-element composition of the upper continental crust has been modified by weathering and we calculate the amount of each element that it must have lost tomodify it to its present composition. By extrapolating modern weathering rates over the ageof the crust we conclude that it has not retained a significant amount of the necessarily produced weathering restite. This restite has likely been subducted into the mantle, indicating acrust-to-mantle recycling rate of 1.33 ± 0.89 × 10 13 kg yr −1 .</p

Major‐element composition of sediments in terms of weathering and provenance: Implications for crustal recycling

The elemental composition of a sediment is set by the composition of its protolith and modified by weathering, sorting, and diagenesis. An important problem is deconvolving these contributions to a sediment's composition to arrive at information about processes that operate on the Earth's surface. We approach this problem by developing a predictive and invertible model of sedimentary major‐element composition. We compile a dataset of sedimentary rock, river sediment, soil, and igneous rock compositions. Principal component analysis of the dataset shows that most variation can be simplified to a small number of variables. We thus show that any sediment's composition can be described with just two vectors of igneous evolution and weathering. We hence define a model for sedimentary composition as a combination of these processes. A 1:1 correspondence is observed between predictions and independent data. The log‐ratios ln(K2O/MgO) and ln(Al2O3/Na2O) are found to be simple proxies for, respectively, the model's protolith and weathering indices. Significant deviations from the model can be explained by sodium‐calcium exchange. Using this approach, we show that the major‐element composition of the upper continental crust has been modified by weathering and we calculate the amount of each element that it must have lost to modify it to its present composition. By extrapolating modern weathering rates over the age of the crust we conclude that it has not retained a significant amount of the necessarily produced weathering restite. This restite has likely been subducted into the mantle, indicating a crust‐to‐mantle recycling rate of 1.33 ± 0.89×1013 kg yr‐1

Reciprocity and sensitivity kernels for sea level fingerprints

Reciprocity theorems are established for the elastic sea level fingerprint problem including rotational feedbacks. In their simplest form, these results show that the sea level change at a location x due to melting a unit point mass of ice at x' is equal to the sea level change at x' due to melting a unit point mass of ice at x. This identity holds irrespective of the shoreline geometry or of lateral variations in elastic Earth structure. Using the reciprocity theorems, sensitivity kernels for sea level and related observables with respect to the ice load can be readily derived. It is notable that calculation of the sensitivity kernels is possible using standard fingerprint codes, though for some types of observable a slight generalisation to the fingerprint problem must be considered. These results are of use within coastal hazard assessment and have a range of potential applications within studies of modern-day sea level change.Comment: Paper submitted to Geophysical Journal Internationa

European native oysters and associated species richness in the presence of non-native species in a southern North Sea estuary complex

There are growing calls to restore populations of European native oysters (Ostrea edulis), on the premise that restored populations will support a range of ecosystem services with an emphasis placed on restored oyster habitats promoting biological diversity, however benefits associated with naturally occurring O. edulis remain unclear. We undertook biannual surveys in the Blackwater, Crouch, Roach and Colne Estuaries Marine Conservation Zone (BCRC.MCZ), a highly sedimented estuary complex in the southern North Sea, to investigate links between natural densities of O. edulis (0-4.2 m-2), the prevalence of other dominant habitat features such as non-native slipper limpet (Crepidula fornicata), dead shell abundance and epibenthic macroinvertebrate species richness. Increased epibenthic species richness was associated with O. edulis, even at densities below the OSPAR Commission recognised definition of an oyster bed (5 oysters m-2). Our analysis predicts increased associated species richness with density of native oysters (e.g. +1.6 additional species at 1 oyster m-2 or + 2.8 species at 5 oysters m-2), but only in areas with lower density of C. fornicata. Where C. fornicata are at higher density, the potential benefits of oyster restoration for associated species were curtailed. This may explain the observed asymptotic relationship between oyster density and diversity at 1 oyster m-2. In these and other high Crepidula density areas we recommend extending native oyster habitat even at low density. This may be of particular interest to areas with the protozoan oyster parasite Bonamia ostreae, which spreads more easily in high density areas. These lower density thresholds should also be considered for future management decisions – closing harvests so they do not reduce density further and impair biodiversity services of the habitats. In conclusion, while C. fornicata may be a useful oyster settlement substrate, we find that it limits the potential increases in associated species gains of oyster restoration

Multi-uses in the Eastern Atlantic:Building bridges in maritime space

Promoting co-existence and synergies amongst maritime uses is a key issue in maritime spatial management. Maritime economies are developing globally, leading to competition for marine resources and increasing environmental pressures. Multi-use (MU) is the joint use of marine resources in close geographic proximity. Focusing on the Eastern Atlantic sea basin, this article provides an overview of the MU context, existing and potential MUs, and the main drivers and barriers thereof. Based on desk research, literature review and stakeholder engagement, this study highlights differences between countries, regarding the implementation and advancement of sea strategies, and sector-specific and other Maritime Spatial Planning (MSP)-related policies. The legal, administrative and operational processes required to realise MUs are highly diverse and are related to the maturity of national maritime policies including MSP. A total of 25 MUs were identified and the three most relevant (Fisheries &amp; Tourism &amp; Environmental protection; Underwater cultural heritage &amp; Tourism &amp; Environmental protection, and; Offshore wind &amp; Aquaculture) were analysed in-depth. The general conclusion refers to the need for multi-dimensional and multi-level policy actions overcoming technology constraints, and improving regulatory and policy frameworks. European strategies and actions might assist these efforts, however, the identified gaps are resolvable mainly at the national level within its specific context and through the engagement of innovative stakeholders. Recommendations for promoting MUs are presented. In summary, MUs are recognised as joint ventures, enabling synergy of interests and minimising conflicts. Findings suggest that early stakeholder engagement in the process of planning and implementing MU is necessary to achieve synergies, while respecting national planning cultures and existing MU experience leads to conflict solving solutions.</p

Invasion genetics of Pacific oyster Crassostrea gigas shaped by aquaculture stocking practices

As a result of aquaculture activities Pacific oysters Crassostrea gigas (Thunberg, 1793) have invaded the European Wadden Sea. Using a variable noncoding mitochondrial marker, we show that the invaded range is the result of two independent invasions. Haplotype frequencies point towards two separate groups, one in the southern and the other in the northern Wadden Sea. We found virtually no genetic differentiation throughout the southern range and the putative source from British Columbia, Canada, suggesting that the Southern region can be consid- ered as a closed population. In the North, mismatch distributions, haplotype ordination and isolation-by-distance analysis suggest a stronger, persistent impact of aquaculture on invasive populations. Due to the ongoing supply of new genetic material from hatchery production the northern invasive populations can therefore be considered as an open population highlighting the importance of aquaculture practice on the genetics of this keystone invader in the Wadden Sea