Oceanography 443, Winter 2009
Design of Oceanographic Field Experiments

Preliminary reference list

Preliminary reading list for Ocean 443, Winter 2009.  These papers will all be accessible on e-reserve. 

 

A.  You have received two papers that provide overviews:

 (A1) de Ronde, et al. (2007).  Submarine hydrothermal activity along the mid-Kermadec Arc, New Zealand:  large-scale effects on venting.  Geochemistry, Geophysics, Geosystems 8: doi 10.1029/2006GC001495.

(A2)  Bradford-Grieve et al. (2005).  New Zealand Shelf Region. The Sea, vol. 14.

 

B.  Leaning towards Physical Oceanography

 Articles on regional physical oceanography and the Kermadec hydrothermal plumes

An example study of a regional current system, with implications for the distribution of marine larvae:

(B1) Chiswell and Roemmich (1998).  The East Cape Current and two eddies:  A mechanism for larval retention?  NZ Journal of Marine and Freshwater Research 32: 385-397.

An overview of the water column signatures of hydrothermal venting from the Kermadec arc volcanoes (Note:  The book that contains this article will also be on physical reserve in the fish-ocean library, as the article contains a number of figures that have not scanned very well into black and white):

(B2) Baker, et al. (2003).  Submarine hydrothermal venting on the southern Kermadec volcanic arc front (offshore New Zealand):  Location and extent of particle plume signatures.  In Intra-Oceanic Subduction Systems:  Tectonic and Magmatic Processes (R. D. Larter and P. T. Leat, Eds.).  Geological Soc. London Special Pub 219, pp. 141-161.

Techniques for physical plume measurements in hydrothermal systems

Plumes from high-temperature (aka “discrete” or “black smoker”) sources:

 (B3) Bemis, et al. (1993).  Geothermal heat flux from hydrothermal plumes on the Juan de Fuca Ridge.  J. Geophys. Res. 98 (B4): 6351-6365.

Plumes from low-temperature (aka “diffuse”) sources:

 (B4) Rona and Trivett (1992).  Discrete and diffuse heat transfer at ASHES vent field, Axial Volcano, Juan de Fuca Ridge.  Earth and Planet. Sci. Lett. 109: 57-71. (Note: a newer version of the model referred to here is available and was used by a student in 443/444 two years ago.)

 Plume measurement on the scale of entire vent fields:

(B5) Baker and Massoth (1986).  Hydrothermal plume measurements: a regional perspective.  Science 234: 980-982.

Other…

A study of ocean bottom currents deduced from images of sediment ripples:

(B6) Wright (2001). In situ modification of modern submarine hyaloclastic/pyroclastic deposits by oceanic currents: an example from the Southern Kermadec arc (SW Pacific).  Marine Geology 172 (2001) 287–307 

Finally, here is a very broad, but older, overview of the regional physical oceanography … skim and use as a reference, not everything will be relevant:

(B7)  Heath (1985).  A review of the physical oceanography of the seas around New Zealand - 1982.  NZ Journal of Marine and Freshwater Research 19: 79-124.

 
 

C.  Leaning towards Marine Geology and Geophysics

(C1) Smith and Price (2006).  The Tonga-Kermadec arc and Havre-lau back-arc system:  their role in the development of tectonic and magmatic models for the western Pacific.

A good overview of the geology of the Brothers Volcano and some water column work

(C2) de Ronde et al. (2003).  Evolution of a submarine magmatic-hydrothermal system:  Brothers Volcano, southern Kermadec Arc, New Zealand.  Economic Geology 100: 1097-1133.

Microbiology of solid phases

(C3)  Jones et al. (2008).  Mineralized microbes from Giggenbach submarine volcano.  Journal of Geophysical Research 113: doi: 10.1029/2007JB005482

Paper on the Tonga Arc hydrothermal system

(C4) Stoffers et al. (2006).  Submarine volcanoes and high-temperature hydrothermal venting on the Tonga arc, southwest Pacific

Not many places you can see mercury rolling around on the deck of the ship when you bring up a dredge…

(C5)  Stoffers et al. (1999).  Elemental mercury at submarine hydrothermal vents in the Bay of Plenty, Taupo volcanic zone, New Zealand.  Geology 27: 931-934.

Anomalous chemistry in a plume after an eruption

 (C6)  Kelley, et al. (1998).  Enriched H2, CH4, and 3He concentrations in hydrothermal plumes associated with the 1996 Gorda Ridge eruptive event.  Deep-Sea Research II 45: 2665-2682.

D.  Leaning towards Biology 

Pelagic populations: distributions and mechanisms

Overview information on regional plankton distributions:

 (D1) Chang et al. (2003). Seasonal and spatial variation of phytoplankton assemblages, biomass and cell size from spring to summer across the north-eastern New Zealand continental shelf. Journal of Plankton Research 25(7):737-758.

 (D2) Chang et al. (1998) Phytoplankton assemblages and photosynthetic pigments during winter and spring in the Subtropical Convergence region near New Zealand. New Zealand Journal of Marine and Freshwater Research 32:515-530.

 

Plankton distributions in and near hydrothermal vent plumes:

(D3) Vereshchaka and Vinogradov (1999) Visual observations of the vertical distribution of plankton throughout the water column above Broken Spur vent field, Mid-Atlantic Ridge. Deep Sea Research I 46(9):1615-1632.

 

Consumers of plankton (look: charismatic megafauna! but why are they there…?):

(D4) Richards, R. (2002) Southern right whales: a reassessment of their former distribution and migration routes in New Zealand waters, including on the Kermadec grounds. Journal of the Royal Society of New Zealand 32(3):355-377.

If any of you are interested in applied ecosystem analysis, the gray literature has a lot of interesting information. A couple of examples for the Orange Roughly, a commercially important deep-water fish in our area of study (see http://fpcs.fish.govt.nz/Science/Plenary.aspx for a broad range of other species):

(D5) Ministry of Fisheries (2008) Report from the fishery assessment plenary, 2008: stock assessments and yield estimates. Ministry of Fisheries, Wellington, New Zealand.

http://fpcs.fish.govt.nz/science/documents/Plenary/ORHINTRO_FINAL%2008.pdf

http://fpcs.fish.govt.nz/science/documents/Plenary/ORH%202A2B3A_FINAL%2008.pdf

Linking pelagic and benthic communities

Distributions of benthic marine invertebrate larval, and the roles of transport by horizontal currents and hydrothermal plumes:

(D6) Kim and Mullineaux (1998) Distribution and near-bottom transport of larvae and other plankton at hydrothermal vents. Deep-Sea Research II 45:423-440.

 

One of many papers on species endemic to the region:

(D7) Glover et al. (2004) Bathyaustriella thionipta, a new lucinid bivalve from a hydrothermal vent on the Kermadec Ridge, New Zealand and its relationship to shallow-water taxa (Bivalvia : Lucinidae).

 

An example of using percent cover data (i.e., what you could do from photographs) to compare benthic communities…

(D8) Gardner et al. (2006) Benthic community structure and water column characteristics at two sites in the Kermadec Islands Marine Reserve, New Zealand

 

An evolutionary modeling perspective on population structure of vent fauna (an interesting consideration of moving adult habitat patches, in addition to dispersing larvae):

(D9) Jollivet et al. (1999) Hydrothermal-Vent Alvinellid Polychaete Dispersal in the Eastern Pacific. 2. A Metapopulation Model Based on Habitat Shifts. Evolution 53(4):1128-1142.

 

E.  Leaning towards Chemical Oceanography

Techniques available in Keil Lab (pollutants, sinking particles, carbon fluxes)

(E1) Arditsoglou, A. and Voutsa, D., 2008. Determination of phenolic and steroid endocrine disrupting compounds in environmental matrices. Environ. Sci. Pollut. Res. 15, 228-236.

(E2) Dittmar, T., 2008. The molecular level determination of black carbon in marine dissolved organic matter. Org. Geochem. 39, 396-407.

(E3) Dittmar, T., Koch, B., Hertkorn, N., and Kattner, G., 2008. A simple and efficient method for the solid-phase extraction of dissolved organic matter (SPE-DOM) from seawater. Limnol. Oceanogr. Meth. 6, 230-235.

(E4) Peterson, M. L., Wakeham, S. G., Lee, C., Askea, M. A., and Miquel, J. C., 2005. Novel techniques for collection of sinking particles in the ocean and determining their settling rates. Limnol. Oceanogr. Meth. 3, 520-532.

(E5) Vidal, J. L. M., Vega, A. B., Frenich, A. G., Gonzalez, F. J. E., and Liebanas, F. J. A., 2004. Determination of fifteen priority phenolic compounds in environmental samples from Andalusia (Spain) by liquid chromatography-mass spectrometry. Springer-Verlag Heidelberg.

 

Vent Chemistry:

(E6) Kawagucci, S., Okamura, K., Kiyota, K., Tsunogai, U., Sano, Y., Tamaki, K., and Gamo, T., 2008. Methane, manganese, and helium-3 in newly discovered hydrothermal plumes over the Central Indian Ridge, 18 degrees-20 degrees S. Geochem. Geophys. Geosyst. 9, 14.

(E7) Love, B. A., Resing, J. A., Cowen, J. P., Lupton, J. E., Fornari, D. J., Shank, T. M., and Biller, D., 2008. Methane, manganese, and helium in hydrothermal plumes following volcanic eruptions on the East Pacific Rise near 9 degrees 50 ' N. Geochem. Geophys. Geosyst. 9, 15.

(E8) Lupton, J., Lilley, M., Butterfield, D., Evans, L., Embley, R., Massoth, G., Christenson, B., Nakamura, K., and Schmidt, M., 2008. Venting of a separate CO2-rich gas phase from submarine arc volcanoes: Examples from the Mariana and Tonga-Kermadec arcs. J. Geophys. Res.-Solid Earth 113, 21.

(E9) Proskurowski, G., Lilley, M. D., Seewald, J. S., Fruh-Green, G. L., Olson, E. J., Lupton, J. E., Sylva, S. P., and Kelley, D. S., 2008. Abiogenic hydrocarbon production at Lost City hydrothermal field. Science 319, 604-607.