Mesopelagic crustacea in and around a warm-core eddy in the Tasman Sea off eastern Australia

1983 ◽  
Vol 34 (4) ◽  
pp. 609 ◽  
Author(s):  
FB Griffiths ◽  
SB Brandt

Decapod Crustacea were collected during five cruises (in August, September, and October 1979, February and May 1980) at sites inside, at the edge, and outside of warm-core eddy J. These sampling sites were considered to have come from different domains of the Tasman Sea water mass. All 146 samples in this time series were taken in the upper 500 m at night using horizontal tows with an RMT 8. A total of 21 494 individuals belonging to 41 species and five larval categories was found. Nine of the 18 abundant species were cosmopolitan species: typical of samples from outside, at the edge of, and inside eddy J. Oplophorus spinosus was typical only at the eddy edge. Four species were typical of the outside and edge domains, and another four were typical of the inside and edge domains. Species abundances outside the eddy were dominated by Sergia prehensilis, Gennadas gilchristi, and Acanthephyra quadrispinosa. The first two species, plus Systellaspis debilis, were dominant at the eddy edge. Six species (Systellaspis debilis, Sergia prehensilis, Sergia scintillans, Sergia splendens, Sergestes atlanticus, and Parapandalas cf. richardi) were dominant at various times inside the eddy. There were no significant differences in the abundance of Sergia prehensilis in the three domains. Systellaspis debilis was significantly more abundant inside and at the eddy edge than outside the eddy, and Gennadas gilchristi was significantly more abundant outside and at the eddy edge than inside the eddy. An analysis of the community changes with time showed that the outside communities remained very similar in spite of the 5°30' change in latitude of eddy J between August 1979 and May 1980. In contrast, the inside communities were quite dissimilar between months, and there was no trend in this pattern. The edge communities were very similar except in May, when a large increase in the abundance of Gennadas gilchristi was found. Comparisons of communities between domains within each month showed the outside and edge communities were very similar over the entire period. In contrast, the outside and inside communities became increasingly different in time, mainly caused by changes in the abundances of species inside the eddy. The inside and edge communities were also quite different, but no consistent pattern in their dissimilarity with time was seen. Differences in the size-frequency distributions of Sergla prehensilis and Systellaspis debilis between domains through time suggest that breeding and recruitment were occumng at different times inside and outside the eddy. There was little evidence for colonization of the eddy by Tasman Sea species. We conclude that a secondary succession has been initiated, probably in response to the different physical and biological environments present inside eddy J as compared with the surrounding Tasman Sea.

1988 ◽  
Vol 39 (1) ◽  
pp. 71 ◽  
Author(s):  
S Andrijanic

Major water masses found off eastern Australia can be identified by their planktonic foraminiferal faunas. A total of 83 surface and oblique plankton samples from two cruises, in spring (October) and summer (January), between Hobart at 44� S. and Townsville at 18� S. yielded 27 species belonging to four distinct faunas: 'tropical', 'warm subtropical', 'cool subtropical' and 'transitional'. The tropical fauna is characterized by Globigerinoides sacculifer at an abundance greater than 42% and the co- dominance of Globigerinoides conglobatus, and is associated with Coral Sea water of equatorial origin. The subtropical fauna can be subdivided into warm and cool elements. The warm-subtropical fauna, with G. sacculifer more abundant than Globigerinoides ruber, inhabits Coral and Tasman Sea waters. The cool-subtropical fauna is a mixture of the warm subtropical and the transitional faunas. The transitional fauna is dominated by Globorotalia inflata and Globigerina bulloides in the south Tasman Sea subantarctic waters. It characterizes the South West Tasman water as defined by Rochford (1957). These water masses can be clearly separated, and the extent of mixing determined by their foraminiferal fauna. The shifts in the boundaries between the faunal zones was evident between spring and summer. The boundary between the tropical and subtropical water corresponds to the tropical convergence and the subtropical/transitional boundary is the Tasman Front. During the spring cruise, a warm core eddy was identified by its warm subtropical foraminiferal fauna surrounded by a transitional fauna to the south and cool subtropical fauna to the north. This water body was near 32� S., which is consistent with the reported positions of eddies shed by the East Australian Current. The distribution patterns of individual species are discussed.


1987 ◽  
Vol 38 (6) ◽  
pp. 711 ◽  
Author(s):  
JW Young

Hyperiid amphipods were sampled from a warm-core eddy in the Tasman Sea in August, September and October 1979. Samples were taken at night to a depth of 400 m using a midwater trawl (RMT-8). In all, 22 798 hyperiids representing 38 species and 10 families were identified, adding 13 new records for eastern Australian waters. For each species, synoptic information is given on taxonomy, life history, vertical distribution, geographic range and associations with gelatinous zooplankton. Hyperiids were confined mainly to the upper 100 m of water at night. Evidence for a summer breeding season was found in three abundant species (Scina crassicornis, Primno johnsoni and Brachyscelus crusculum). Tropical hyperiid species may be transported into the Tasman Sea by the southward movement of eddies from their origin in the Coral Sea.


Author(s):  
Keizo Negi ◽  
Keizo Negi ◽  
Takuya Ishikawa ◽  
Takuya Ishikawa ◽  
Kenichiro Iba ◽  
...  

Japan experienced serious water pollution during the period of high economic growth in 1960s. It was also the period that we had such damages to human health, fishery and living conditions due to red tide as much of chemicals, organic materials and the like flowing into the seas along the growing population and industries in the coastal areas. Notable in those days was the issues of environment conservation in the enclosed coastal seas where pollutants were prone to accumulate inside due to low level of water circulation, resulting in the issues including red tide and oxygen-deficient water mass. In responding to these issues, we implemented countermeasures like effluent control with the Water Pollution Control Law and improvement/expansion of sewage facilities. In the extensive enclosed coastal seas of Tokyo Bay, Ise Bay and the Seto Inland Sea, the three areas of high concentration of population, we implemented water quality total reduction in seven terms from 1979, reducing the total quantities of pollutant load of COD, TN and TP. Sea water quality hence has been on an improvement trend as a whole along the steady reduction of pollutants from the land. We however recognize that there are differences in improvement by sea area such as red tide and oxygen-deficient water mass continue to occur in some areas. Meanwhile, it has been pointed out that bio-diversity and bio-productivity should be secured through conservation/creation of tidal flats and seaweed beds in the view point of “Bountiful Sea” To work at these challenges, through the studies depending on the circumstances of the water environment in the enclosed coastal seas, we composed “The Policy of Desirable State of 8th TPLCS” in 2015. We have also added the sediment DO into the water quality standard related to the life-environmental items in view of the preservation of aquatic creatures in the enclosed water areas. Important from now on, along the Policy, is to proceed with necessary measures to improve water quality with good considerations of differences by area in the view point of “Beautiful and bountiful Sea”.


Coral Reefs ◽  
2021 ◽  
Author(s):  
Liam Lachs ◽  
Brigitte Sommer ◽  
James Cant ◽  
Jessica M. Hodge ◽  
Hamish A. Malcolm ◽  
...  

AbstractAnthropocene coral reefs are faced with increasingly severe marine heatwaves and mass coral bleaching mortality events. The ensuing demographic changes to coral assemblages can have long-term impacts on reef community organisation. Thus, understanding the dynamics of subtropical scleractinian coral populations is essential to predict their recovery or extinction post-disturbance. Here we present a 10-yr demographic assessment of a subtropical endemic coral, Pocillopora aliciae (Schmidt-Roach et al. in Zootaxa 3626:576–582, 2013) from the Solitary Islands Marine Park, eastern Australia, paired with long-term temperature records. These coral populations are regularly affected by storms, undergo seasonal thermal variability, and are increasingly impacted by severe marine heatwaves. We examined the demographic processes governing the persistence of these populations using inference from size-frequency distributions based on log-transformed planar area measurements of 7196 coral colonies. Specifically, the size-frequency distribution mean, coefficient of variation, skewness, kurtosis, and coral density were applied to describe population dynamics. Generalised Linear Mixed Effects Models were used to determine temporal trends and test demographic responses to heat stress. Temporal variation in size-frequency distributions revealed various population processes, from recruitment pulses and cohort growth, to bleaching impacts and temperature dependencies. Sporadic recruitment pulses likely support population persistence, illustrated in 2010 by strong positively skewed size-frequency distributions and the highest density of juvenile corals measured during the study. Increasing mean colony size over the following 6 yr indicates further cohort growth of these recruits. Severe heat stress in 2016 resulted in mass bleaching mortality and a 51% decline in coral density. Moderate heat stress in the following years was associated with suppressed P. aliciae recruitment and a lack of early recovery, marked by an exponential decrease of juvenile density (i.e. recruitment) with increasing heat stress. Here, population reliance on sporadic recruitment and susceptibility to heat stress underpin the vulnerability of subtropical coral assemblages to climate change.


2007 ◽  
Vol 67 (1) ◽  
pp. 100-114 ◽  
Author(s):  
Tine L. Rasmussen ◽  
Erik Thomsen ◽  
Marta A. Ślubowska ◽  
Simon Jessen ◽  
Anders Solheim ◽  
...  

AbstractTwo cores from the southwestern shelf and slope of Storfjorden, Svalbard, taken at 389 m and 1485 m water depth have been analyzed for benthic and planktic foraminifera, oxygen isotopes, and ice-rafted debris. The results show that over the last 20,000 yr, Atlantic water has been continuously present on the southwestern Svalbard shelf. However, from 15,000 to 10,000 14C yr BP, comprising the Heinrich event H1 interval, the Bølling–Allerød interstades and the Younger Dryas stade, it flowed as a subsurface water mass below a layer of polar surface water. In the benthic environment, the shift to interglacial conditions occurred at 10,000 14C yr BP. Due to the presence of a thin upper layer of polar water, surface conditions remained cold until ca. 9000 14C yr BP, when the warm Atlantic water finally appeared at the surface. Neither extensive sea ice cover nor large inputs of meltwater stopped the inflow of Atlantic water. Its warm core was merely submerged below the cold polar surface water.


2005 ◽  
Vol 2 (4) ◽  
pp. 417-435 ◽  
Author(s):  
A. Henry-Edwards ◽  
M. Tomczak

Abstract. A new water mass analysis technique is used to analyse the BATS oceanographic data set in the Sargasso Sea of 1988-1998 for changes in Labrador Sea Water (LSW) properties. The technique is based on a sequential quadratic programming method and requires careful definition of constraints to produce reliable results. Variations in LSW temperature and salinity observed in the Labrador Sea are used to define the constraints. It is shown that to minimize the residuals while matching the observed temperature and salinity changes in the source region the nitrate concentration in the Labrador Sea has to be allowed to vary as well. It is concluded that during the period of investigation nitrate underwent significant variations in the Labrador Sea.


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