GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    ISSN: 1432-2072
    Keywords: Morphine ; Physical Dependence ; Secondary Reinforcement ; Etonitazene ; Addiction ; Anise-Flavor ; Relapse
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract 1. On 9 nights (2000-0800) over a 25-day period, an anise-flavored aqueous solution of etonitazene, 5 mcg/ml, was provided as the sole drinking fluid for one group of physically dependent rats (MFETZ) maintained on morphine, 200 mg/kg i.p. once daily at 0800 (hence acutely abstinent each night) and for one group of saline-injected rats (SFETZ), while only anise-flavored water was available to comparable physically dependent (MFH2O) and saline-injected (SFH2O) groups. 2. Beginning 3 days after abrupt and permanent termination of morphine or saline injections, all rats were tested at intervals over a period of 287 days on nocturnal (2000-0800) choice drinking from 2 tubes (positions alternated), one contained anise-flavored water and the other, plain water. 3. Analyses of variance on the mean volumes of each of the two fluids consumed by each rat over blocks of choice-drinking tests revealed that through the VIIth test (137th post-injection day), MFETZ drank more anise-flavored water than any other group while there were no significant differences among the groups as regards consumption of plain water. 4. The evidence indicates that the potency of secondary reinforcers so generated can persist long after morphine withdrawal. Some implications for problems of relapse and treatment of opioid addicts are discussed.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Psychopharmacology 16 (1970), S. 375-384 
    ISSN: 1432-2072
    Keywords: Morphine ; Etonitazene ; Addiction ; Physical Dependence ; Relapse
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Summary 1. Measurements of 24 hr tap water consumption, body weight, “wet dog” shake frequency and free choice drinking (etonitazene, 5 mcg/ml versus distilled water) were made at intervals up to 434 days following abrupt withdrawal of morphine (from a daily maintenance dose level of 200 mg/kg i.p.) in one group of rats (“postaddicts”) and following termination of i.p. injections of saline in a control group of rats (“normals”). 2. During the first five days after termination of injections, signs of primary morphine abstinence were observed in the “postaddict” rats: transient decrease in 24 hr tap water consumption and in body weight, and increase in “wet dog” shake frequency. 3. Secondary morphine-abstinence phenomena, consisting of signicantly greater 24 hr tap water consumption and slightly higher “wet dog” shake frequency (compared with normal rats) were observed in “postaddict” rats over the 7th–23rd post-injection days. Thereafter, these differences persisted, but not at significant levels. 4. In a no-choice test (etonitazene, 5 mcg/ml or water on different occasions) conducted between the 28th and 37th days after termination of injections, “post-addict” rats drank significantly more etonitazene than water, whereas normal rats drank slightly less etonitazene than water. 5. In free-choice drinking tests (etonitazene, 5 mcg/ml versus water) conducted at intervals over a period of 434 days following termination of injections (morphine or saline), no significant differences in mean water consumption between “post-addict” and normal rats were observed. In contrast, “postaddict” rats drank significantly larger mean volumes of the etonitazene solution on every “relapse” test through the 336th and again on the 406th post-withdrawal day (but not on the 372nd or 434th day). 6. It is concluded that in the “postaddict” rat a “need” for an opioid persists for about one year after abrupt withdrawal of morphine, and that this “need” is based on long-term derangement of homeostasis. although the physiological characteristics of such homeostatic derangement differ in the relatively short primary and more protracted secondary abstinence periods. 7. The long persistence of “relapse-tendency” in rats previously made physically dependent on morphine may be based on such long-term derangement of homeostasis coupled, perhaps, with “interoceptive” conditioning generated during daily cycles of primary abstinence from and relief by morphine in the “addiction” period, through which the internal sensorial effects of opioids (morphine while receiving injections; etonitazene imbibed in “relapse” tests) may acquire secondary reinforcing properties.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2021-06-25
    Description: The compositional record of the AND-2A drillcore is examined using petrological, sedimentological, volcanological and geochemical analysis of clasts, sediments and pore waters. Preliminary investigations of basement clasts (granitoids and metasediments) indicate both local and distal sources corresponding to variable ice-volume and ice-flow directions. Low abundance of sedimentary clasts (e.g., arkose, litharenite) suggests reduced contributions from sedimentary covers while intraclasts (e.g., diamictite, conglomerate) attest to intrabasinal reworking. Volcanic material includes pyroclasts (e.g., pumice, scoria), sediments and lava. Primary and reworked tephra layers occur within the Early Miocene interval (1093 to 640 metres below sea floor). The compositions of volcanic clasts reveal a diversity of alkaline types derived from the McMurdo Volcanic Group. Finer-grained sediments (e.g., sandstone, siltstone) show increases in biogenic silica and volcanic glass from 230 to 780 mbsf and higher proportions of terrigenous material ca. 350 to 750 mbsf and below 970 mbsf. Basement clast assemblages suggest a dominant provenance from the Skelton Glacier - Darwin Glacier area and from the Ferrar Glacier - Koettlitz Glacier area. Provenance of sand grains is consistent with clast sources. Thirteen Geochemical Units are established based on compositional trends derived from continuous XRF scanning. High values of Fe and Ti indicate terrigenous and volcanic sources, whereas high Ca values signify either biogenic or diagenic sources. Highly alkaline and saline pore waters were produced by chemical exchange with glass at moderately elevated temperatures.
    Description: Published
    Description: 147-192
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: N/A or not JCR
    Description: open
    Keywords: Antartica ; ANDRILL ; Sea Ross ; Volcanic Rocks ; 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology ; 04. Solid Earth::04.04. Geology::04.04.07. Rock geochemistry ; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2021-06-25
    Description: The compositional record of the AND-2A drillcore is examined using petrological, sedimentological, volcanological and geochemical analysis of clasts, sediments and pore waters. Preliminary investigations of basement clasts (granitoids and metasediments) indicate both local and distal sources corresponding to variable ice-volume and ice-flow directions. Low abundance of sedimentary clasts (e.g., arkose, litharenite) suggests reduced contributions from sedimentary covers while intraclasts (e.g., diamictite, conglomerate) attest to intrabasinal reworking. Volcanic material includes pyroclasts (e.g., pumice, scoria), sediments and lava. Primary and reworked tephra layers occur within the Early Miocene interval (1093 to 640 metres below sea floor). The compositions of volcanic clasts reveal a diversity of alkaline types derived from the McMurdo Volcanic Group. Finer-grained sediments (e.g., sandstone, siltstone) show increases in biogenic silica and volcanic glass from 230 to 780 mbsf and higher proportions of terrigenous material ca. 350 to 750 mbsf and below 970 mbsf. Basement clast assemblages suggest a dominant provenance from the Skelton Glacier -Darwin Glacier area and from the Ferrar Glacier -Koettlitz Glacier area. Provenance of sand grains is consistent with clast sources. Thirteen Geochemical Units are established based on compositional trends derived from continuous XRF scanning. High values of Fe and Ti indicate terrigenous and volcanic sources, whereas high Ca values signify either biogenic or diagenic sources. Highly alkaline and saline pore waters were produced by chemical exchange with glass at moderately elevated temperatures.
    Description: Published
    Description: 147-192
    Description: 2.3. TTC - Laboratori di chimica e fisica delle rocce
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: N/A or not JCR
    Description: reserved
    Keywords: Andrill ; Antarctica ; Geochemestry ; Volcanology ; 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology ; 04. Solid Earth::04.04. Geology::04.04.07. Rock geochemistry ; 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport ; 04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...